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+ Pyotr Ilyich Tchaikovsky (Russian: Пётр Ильич Чайкoвский, Pëtr Il’ič Čajkovskij; listen (help·info)) (born Kamsko-Votkinsk, 7 May 1840; died St Petersburg, 6 November 1893; pronounced chai-KOV-skee) was a Russian composer who lived in the Romantic period. He is one of the most popular of all Russian composers. He wrote melodies which were usually dramatic and emotional. He learned a lot from studying the music of Western Europe, but his music also sounds very Russian. His compositions include 11 operas, 3 ballets, orchestral music, chamber music and over 100 songs. His famous ballets (Swan Lake, The Nutcracker and Sleeping Beauty) have some of the best known tunes in all of romantic music. He is widely regarded as the greatest composer of ballets.
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+ Tchaikovsky’s father was a Ukrainian who worked as a mining engineer. His mother’s grandfather was a Frenchman who had moved to Russia. She was a nervous woman and Tchaikovsky may have gotten his nervous character from her. Tchaikovsky was only five when he started taking piano lessons. He was soon better than his teacher. The family had an orchestrion (a kind of musical box) which played some tunes from classical music by Mozart, Bellini, Donizetti and Rossini.
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+ In 1848 the family moved to St. Petersburg. Tchaikovsky was unhappy and unsettled as he was often separated from his family who moved several times. In 1854 his mother died. He tried to comfort himself by playing music. He spent nine years at the School of Jurisprudence. When he left school, he had to get a job. For four years he worked as a clerk in the Ministry of Justice. Then the composer and pianist Anton Rubinstein helped him to become a music student at the newly opened conservatory in St. Petersburg. He learned to play the flute and the organ as well as the piano and learning all about composition. In 1866 he moved to Moscow where Nikolai Rubinstein, the brother of Anton, encouraged him to write music with a Russian character. He worked very hard, and was often exhausted, but he managed to finish his First Symphony, which was performed in 1868.
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+ Tchaikovsky met some famous musicians including the French composer Berlioz who was visiting Moscow. He also became friendly with the Russian composer Mily Balakirev who was very helpful and persuaded him to rewrite one of his works several times until it was very good. he result was a piece for orchestra called Romeo and Juliet which soon became internationally known. Balakirev had four friends who were composers. This circle of friends is often called “The Five” or “The Mighty Handful”. They were interested in using Russian folktunes in their music. Tchaikovsky was never a member of the group, although he liked their ideas. Tchaikovsky was different to them: he had learned music at the Conservatoire where he had studied Western music. The harmonies that he used in his works were often not suitable for Russian folktunes. He wrote many songs which are romantic in character. One of them, None But the Lonely Heart, is especially well known in English.
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+ By now, Tchaikovsky was writing works which were to make him very famous. He wrote two more symphonies, and his First Piano Concerto, one of the most popular of all piano concertos, was given its first performance in Boston. He was also writing operas and chamber music.
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+ In 1875, Tchaikovsky began making a long tour of Europe. He liked Bizet’s opera Carmen, but Wagner’s operas from the Ring cycle bored him. In 1877 he finished Swan Lake, the first of his three ballets. The audience did not like it at first because the dancers were not very good.
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+ Tchaikovsky was a closeted homosexual.[1] In the summer of 1877 Tchaikovsky decided to marry. His wife was called Antonina Milyukova. The marriage was a disaster. A few weeks after the marriage, he ran away and never lived with her again.
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+ Another woman was to become important in his life, but in a very different way. It was to be a very unusual relationship. Her name was Nadezhda von Meck. She was the wife of a rich man. She loved Tchaikovsky’s music and promised him that she would pay him a lot of money every month so long as he promised her that he would never try to meet her. Tchaikovsky no longer needed to work. He was able to give up his teaching job at the Conservatory. For several years he spent the winters in Europe and the summers in Russia. Nadezhda and Tchaikovsky wrote long letters to one another, often quite passionate and dreamy they talked about love, life and how they wanted it to change, but they never saw one another. He had plenty of time to write music: he wrote several operas including Eugene Onegin and his Fourth and Fifth Symphonies, the Violin Concerto, the Serenade for Strings, Capriccio Italienne and the 1812 Overture. Tchaikovsky loved Nadezhda very much but never actually told her his true feelings.
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+ By 1885, Tchaikovsky had tired of travelling around. He rented a country house in Klin, just outside Moscow. He lived a regular life, reading, walking in the forest, composing during the day and playing music with his friends in the evenings. He started to have more confidence as a conductor and toured Europe twice, conducting in Leipzig, Berlin, Prague, Hamburg, Paris and London. In 1889 he finished his second ballet, The Sleeping Beauty and the next year, while staying in Florence, he wrote his famous opera The Queen of Spades based on a story by Pushkin. Later that year Nadezhda von Meck wrote to him that she had lost nearly all her money and could not continue to support him.
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+ In the spring of 1891 he was invited to conduct in New York where the Carnegie Hall was being opened. He also conducted concerts in Baltimore and Philadelphia. When he returned to Russia he wrote his last ballet The Nutcracker and his Sixth Symphony, known as the “Pathétique” which was dedicated to his nephew with whom he was passionately in love. This work is often considered his best. It was performed in St Petersburg on October 16 1893. Five days later he suddenly became ill with cholera, a disease many people were catching in the city. Tchaikovsky died four days later. Many people think that he committed suicide by deliberately drinking contaminated water. He may have wanted to (or even been forced to) commit suicide in order to avoid a scandal because he was having a relationship with a nephew of an important aristocratic man. Exactly what happened is still a mystery.
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+ The sunflower (Helianthus annuus) is a living annual plant in the family Asteraceae, with a large flower head (capitulum). The stem of the flower can grow up to 3 metres tall, with a flower head that can be 30 cm wide. Other types of sunflowers include the California Royal Sunflower, which has a burgundy (red + purple) flower head.
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+ The flower head is actually an inflorescence made of hundreds or thousands of tiny flowers called florets. The central florets look like the centre of a normal flower, apseudanthium. The benefit to the plant is that it is very easily seen by the insects and birds which pollinate it, and it produces thousands of seeds.
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+ The sunflower is the state flower of Kansas. That is why Kansas is sometimes called the Sunflower State.
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+ To grow well, sunflowers need full sun. They grow best in fertile, wet, well-drained soil with a lot of mulch. In commercial planting, seeds are planted 45 cm (1.5 ft) apart and 2.5 cm (1 in) deep.
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+ The outer petal-bearing florets are the sterile florets and can be yellow, red, orange, or other colors. The florets inside the circular head are called disc florets, which mature into seeds.
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+ The flower petals within the sunflower's cluster are always in a spiral pattern. Generally, each floret is oriented toward the next by approximately the golden angle, 137.5°, producing a pattern of interconnecting spirals, where the number of left spirals and the number of right spirals are successive Fibonacci numbers. Typically, there are 34 spirals in one direction and 55 in the other; on a very large sunflower there could be 89 in one direction and 144 in the other.[1][2]
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+ Sunflowers commonly grow to heights between 1.5 and 3.5 m (5–12 ft.). The tallest sunflower confirmed by Guinness World Records is 9.17 m (2014, Germany). In 16th century Europe the record was already 7.3 m (24 ft., Spain).[3] Most cultivars are variants of H. annuus, but four other species (all perennials) are also domesticated. This includes H. tuberosus, the Jerusalem Artichoke, which produces edible tubers.
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+ Sunflower "whole seed" (fruit) are sold as a snack food, after roasting in ovens, with or without salt added. Sunflowers can be processed into a peanut butter alternative, Sunbutter. In Germany, it is mixed together with rye flour to make Sonnenblumenkernbrot (literally: sunflower whole seed bread), which is quite popular in German-speaking Europe. It is also sold as food for birds and can be used directly in cooking and salads.
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+ Sunflower oil, extracted from the seeds, is used for cooking, as a carrier oil and to produce margarine and biodiesel, as it is cheaper than olive oil. A range of sunflower varieties exist with differing fatty acid compositions; some 'high oleic' types contain a higher level of healthy monounsaturated fats in their oil than Olive oil.
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+ The cake remaining after the seeds have been processed for oil is used as a livestock feed. Some recently developed cultivars have drooping heads. These cultivars are less attractive to gardeners growing the flowers as ornamental plants, but appeal to farmers, because they reduce bird damage and losses from some plant diseases. Sunflowers also produce latex and are the subject of experiments to improve their suitability as an alternative crop for producing hypoallergenic rubber.
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+ Traditionally, several Native American groups planted sunflowers on the north edges of their gardens as a "fourth sister" to the better known three sisters combination of corn, beans, and squash.[9] Annual species are often planted for their allelopathic properties.[source?] However, for commercial farmers growing commodity crops, the sunflower, like any other unwanted plant, is often considered a weed. Especially in the midwestern USA, wild (perennial) species are often found in corn and soybean fields and can have a negative impact on yields.
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+ Sunflowers may also be used to extract toxic ingredients from soil, such as lead, arsenic and uranium. They were used to remove uranium, cesium-137, and strontium-90 from soil after the Chernobyl disaster (see phytoremediation).
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+ Pisa is a city in Tuscany, Italy. About 90,000 people live in the city. The city has a very long and turbulent history. The "Leaning Tower of Pisa" is a famous landmark of Pisa.
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+ The Pitcairn Islands are a group of islands in the southern Pacific. People only live on the second-largest of the four islands. That island is named Pitcairn. It is governed by the United Kingdom. It has the smallest number of people of any country. In 2019, 50 people lived there.
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+ The islands are best known as home of the descendants of the Bounty mutineers and the Tahitians (or Polynesians) who accompanied them, an event retold in numerous books and films. This history still shows in the surnames of many of the islanders. There are only four family names (as of 2010): Christian, Warren, Young and Brown.
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+ Originally people from Polynesia lived on the Pitcairn Islands, but there was no one living on the islands when they were discovered (found) by Captain Philip Carteret of H.M.S. Swallow on 2 July 1767. The island was named after Robert Pitcairn, a 15 year old midshipman who was the first person on the Swallow to see it. Robert is believed to have been lost at sea in early 1770 when the ship he was on, HMS Aurora, went missing in the Indian Ocean.[1]
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+ In 2004 charges were laid against seven men living on Pitcairn and six living abroad with sex-related offences dating back a number of years. On 25 October 2004, six men were convicted, including the island's mayor at the time. After the six men lost their final appeal, the British government set up a prison on the island at Bob's Valley. The men began serving their sentences in late 2006, as of 2010 all men have served their sentences or been granted home detention status (Pitcairn News, 2010).
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+ In 2010 the island received a new and updated constitution.[2]
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+ Durcie atoll
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+ Oeno atoll
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+ Satellite image of Pitcairn island
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+ Henderson Island
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+ Adamstown on Pitcairn Island.
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+ Pizza is a type of food that was created in Italy. It is made by putting "toppings" (such as cheese, sausages, pepperoni, vegetables, tomatoes, spices and herbs and basil and fries) over a piece of bread covered with sauce. The sauce is most often tomato-based, but sometimes butter-based sauces are used. The piece of bread is usually called a "pizza crust". Almost any kind of topping can be put over a pizza. The toppings used are different in different parts of the world. Pizza comes from Italy, from Neapolitan cuisine, but has become popular in many parts of the world.[1]
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+ The origin of the word Pizza is uncertain. The food was invented in Naples about 200 years ago. It is the name for a special type of flatbread, made with special dough.[2] The pizza enjoyed a second birth as it was taken to the United States in the later 19th century.
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+ Flatbreads like the focaccia from Liguria have been known for a very long time. Pizzas need to be baked at temperatures of 200–250 °C. Hardly any household oven could reach such temperatures at the time. Because of this, the pizza was made at home, and then given to the town bakery to bake. In June 1889, the Neapolitan chef Raffaele Esposito created the "Margherita" in honour of Queen Margherita, and was the first pizza to include cheese.[3]
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+ Pizza was brought to the United States with Italian immigrants in the late nineteenth century;[4] and first appeared in areas where Italian immigrants concentrated. The country's first pizzeria, Lombardi's, opened in 1905.[5] Veterans returning from World War II's Italian Campaign were a ready market for pizza.[6] Since then pizza consumption has exploded in the U.S.[7] Pizza chains such as Domino's, Pizza Hut, and Papa John's, have outlets all over the nation. Thirteen percent of the U.S. population eats pizza on any given day.[8]
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+ In the 20th century, pizza has become an international food and the toppings may be quite different in accordance with local tastes. These pizzas consist of the same basic design but include many choice of ingredients, such as anchovies, egg, pineapple, banana, coconut, sauerkraut, eggplant, kimchi, lamb, couscous, chicken, fish, and shellfish, meats prepared in styles such as Turkish lamb, Doner or chicken tikka masala, and non-traditional spices such as curry and Thai sweet chili. Pizzas can also be made without meat for vegetarians, and without cheese for vegans.
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+ Neapolitan pizza (pizza Napoletana). Authentic Neapolitan pizzas are made with local ingredients like San Marzano tomatoes, which grow on the volcanic plains to the south of Mount Vesuvius and Mozzarella di Bufala Campana, made with the milk from water buffalo raised in the marshlands of Campania and Lazio in a semi-wild state (this mozzarella is protected by its own European law). The genuine Neapolitan pizza dough consists of Italian flour, natural Neapolitan yeast or brewer's yeast, salt and water.The dough must be kneaded by hand or with a low-speed mixer. After the rising process, the dough must be formed by hand without the help of a rolling pin or other mechanical device, and may be no more than 3 mm (1/8 in) thick.Pizza is cooked in a oven.When cooked, it should be crispy, tender and fragrant. Neapolitan pizza has gained the status of "guaranteed traditional specialty" in Italy. This admits only three official variants: Pizza marinara, which is made with tomato, garlic, oregano and extra virgin olive oil (although most Neapolitan pizzerias also add basil to the marinara), Pizza Margherita, made with tomato,mozzarella, basil and extra virgin olive oil, and Pizza Margherita DOC made with tomato, buffalo mozzarella from Campania in fillets, basil and extra virgin olive oil.
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+ Lazio style: Pizza in Lazio (Rome), as well as in many other parts of Italy is available in 2 different "flavors": 1) In take-away shops so-called "Pizza Rustica" or "Pizza a Taglio". Pizza is cooked in long, rectangular baking pans and relatively thick (1–2 cm). The crust similar to that of an English muffin and mostly cooked in an electric oven. When purchased, it is usually cut with scissors or knife and priced by weight. 2) In Pizza Restaurants (Pizzerias) it is served in a dish in its traditional round shape.
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+ Other types of Lazio-style pizza include:
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+ Sicilian-style pizza has its toppings baked directly into the crust.
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+ Pizza Hut's Sicilian Pizza, introduced in 1994, is not an authentic example of the style as only garlic, basil, and oregano are mixed into the crust,it's sold in the restaurant chain Pizza Hut.
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+ White pizza (pizza bianca) uses no tomato sauce, often substituting pesto or dairy products such as sour cream. Most commonly, especially on the East Coast of the United States, the toppings consist only of mozzarella and ricotta cheese drizzled with olive oil and basil and garlic. In Rome, the term pizza bianca refers to a type of bread topped only with olive oil.
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+ Antica Pizzeria Port'Alba, the first pizzeria in Italy, started making pizzas in 1738 and still serves pizza today.[9]
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+ Some global pizza franchises are Pizza Hut, Domino's Pizza, Cici's Pizza, Papa John's and Little Caesars.
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+ Frozen pizza is pizza that has been prepared beforehand, and is then deep-frozen, to be distributed in supermarkets. It is among the most successful and popular types of convenience food. One main frozen pizza brand is Digiorno.
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+ A beach is a landform along the coast of an ocean, sea, lake, or river. It usually consists of loose particles, such as sand, gravel, shingle, or pebbles. The particles of a beach are sometimes biological in origin, such as mollusc shells or bits of coral and sometimes bits of igneous rock, but the most common mineral in beaches is quartz.
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+ Beaches are natural landing and launching places for boats, and landing craft are specially made for beaches.
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+ People often use beaches for recreation. They swim, bask in the sun, or just relax. The most popular beaches have fine white or light-colored sand and warm water to swim in. Beaches are also used for diving or for seeing marine life.
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+ Among the world's most popular and well-known beaches are Aruba (Dutch Caribbean), Long Beach (Canada), Copacabana Beach (Brazil), Hot Water Beach (New Zealand), Megan Bay (St. Thomas), Kailua Beach (Hawaii), Zandvoort Beach (Netherlands), Jeffreys Bay (South Africa) and Bondi Beach (Australia).
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+ Taking holidays on the beach is something of a British cultural export. Early railways in the 19th century took people to places they had never seen before. This tourism was made possible by the industrial revolution. Whole seaside resort towns grew to support visitors, where before there were just villages. Vacations at the sea became common all over the world.[1]
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+ Beaches are never static. They are always being built up or eroded, more quickly than other landforms. Over time the boundary between the land and the sea changes. New Romney, a small town in Kent, is one of the Cinque Ports, a mile from the sea. In Henry VIII's time it was a port on the south coast of England. The growth of Dungeness has cut it off from the sea. Dungeness is a huge shingle beach.
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+ Football (soccer)
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+ Basketball
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+ Rugby
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+ Gymnastics
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+ Baseball
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+ American football
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+ Cycling·Auto racing
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+ Cricket·Golf
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+ Field hockey·Handball
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+ Archery·Shooting
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+ Fencing·Weightlifting
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+ Pentathlon·Triathlon
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+ Horseback riding
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+ Swimming· Diving
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+ Water polo·Sailing
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+ Canoeing·Rowing
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+ Boxing·Wrestling
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+ Karate·Taekwondo
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+ Tennis· Volleyball
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+ Table tennis· Badminton
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+ Winter sports
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+ Skiing·Curling
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+ Bobsled·Luge
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+ Snowboarding·Biathlon
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+ Ice sledge hockey
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+ Snowboarding is a sport that is much like skiing. A person stands on a snowboard and rides down a mountain covered with snow. A snowboard is a flat board with bindings that hold your feet in place while gliding down the mountain. It is different from skiing because both feet are on one board - like surfing.
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+ Some snowboarders like to ride over jumps and do tricks.
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+ The snowboard was born in the seventy's through the imagination of several different Americans.
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+ The original idea was born in 1965 through Sherman Poppen. He invented the ‘’snurfer ‘’, which was made of two skis fixed together, as a gift to his daughter. It soon became very popular, so he licensed it to the Brunswick Corporation who sold about a million over the next 10 years.
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+ In the mid 1970s Dimitrije Milovich created a snowboard inspired by the surfing board called the 'Winterstick'. Finally, in 1977 Jake Burton Carpenter helped by Tom Sims and Chuck Barfoot created the first snowboard model, which made them very rich.
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+ During the eighty's, the sport became very popular. In 1982 the first National Snowboard race was held in Vermont at Suicide Six. The number of windsurfering and snowboarding stations grew very fast everywhere there was snow and mountains.
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+ Snowboarding was first recommended to join the Olympic program in 1996 by the Olympic council in Atlanta. Two years later, some competitions like the Big slalom and the Half-pipe took place in The Olympic Nagano games.[1]
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+ Snowboarders must wear hot and good quality clothes against the cold temperature. They wear also some ski goggles to protect their eyes from reflection of the sun on the snow, against the snow and the wind that can be very hurtful. It is essential to have a good view during the ride. The board that they used has to be fitted by squares on all its length that allow snowboarders to practice this sport even if there is not a lot of snow. Also, the snowboard is equipped with binding to provide snowboarders solidity and stability. The security attach have to be firmly tied on the binding and clip on one of your boots adapted to this sport. Wearing a helmet is strongly recommended.[2]
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+ There are two possible positions on the board. First of all, there is the regular one. With this position, your right foot is placed in the back. The second one is called goofy where you have to put your left foot in the back. The choice between those two positions is personal to everyone. Contrary to what everybody can thinks, goofys are not necessary left-handed or regulars right-handed. In fact, seventy-five percent of the people are regulars. Because the board make a curve in the front and in the back, it can glide on the two sides. In addition, the board called twin-tips is perfectly symmetric, so it allows windsurfers to glide in switch (when the favorite foot is in the back) or in normal-foot (when the favorite foot is in the front).
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+ A gas giant is a large planet that has a solid core, but a very thick atmosphere. This means that most of the planet is made up of gas. These planets are very large.
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+ In our outer Solar System, there are 4 gas giants: Jupiter, Saturn, Uranus, and Neptune.
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+ Jupiter and Saturn are similar because they are made up of mostly hydrogen and helium. They both contain massive rocky cores that are bigger than Earth. Neptune and Uranus are similar because they are mainly made up of water and rock (a mixture of one or several minerals).
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+ Gas giants have also been found around other stars than the sun. Most of those giant extrasolar planets are "hot giants" orbiting close to their star.
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+ Wikipedia does not yet have an article with this name.
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+ Wikipedia does not yet have an article with this name.
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+ Australia, formally the Commonwealth of Australia, is a country and sovereign state in the southern hemisphere, located in Oceania. Its capital city is Canberra, and its largest city is Sydney.
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+ Australia is the sixth biggest country in the world by land area, and is part of the Oceanic and Australasian regions. Australia, New Zealand, New Guinea and other islands on the Australian tectonic plate are together called Australasia, which is one of the world's great ecozones. When other Pacific islands are included with Australasia, it is called Oceania.
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+ 25 million[10] people live in Australia, and about 85% of them live near the east coast. [11] The country is divided up into six states and two territories, and more than half of Australia's population lives in and around the cities of Sydney, Melbourne, Brisbane, Perth and Adelaide.
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+ Australia is known for its mining (coal, iron, gold, diamonds and crystals), its production of wool, and as the world's largest producer of bauxite.[12] Its emblem is a flower called the Golden Wattle.
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+
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+ Australia's landmass of 7,617,930 square kilometers is on the Indo-Australian plate.[13] The continent of Australia, including the island of Tasmania, was separated from the other continents of the world many millions of years ago. Because of this, many animals and plants live in Australia that do not live anywhere else. These include animals like the kangaroo, the koala, the emu, the kookaburra, and the platypus.
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+
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+ People first arrived in Australia more than 50,000 years ago. These native Australians are called the Australian Aborigines. For the history of Australia, see History of Australia.
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+
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+ Most of the Australian colonies, having been settled from Britain, became mostly independent democratic states in the 1850s and all six combined as a federation on 1 January 1901. The first Prime Minister of Australia was Edmund Barton in 1901. Australia is a member of the United Nations and the Commonwealth of Nations. It is a parliamentary democracy and a constitutional monarchy with Elizabeth II as Queen of Australia and Head of State and a Governor-General who is chosen by the Prime Minister to carry out all the duties of the Queen in Australia.
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+ Australia has six states, two major mainland territories, and other minor territories. The states are New South Wales, Queensland, South Australia, Tasmania, Victoria, and Western Australia.[14] The two major mainland territories are the Northern Territory and the Australian Capital Territory (ACT).
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+
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+ In 2013 according to world bank Australia had just over 23.13 million people. Most Australians live in cities along the coast, such as Sydney, Melbourne, Brisbane, Perth, Darwin, Hobart and Adelaide. The largest inland city is Canberra, which is also the nation's capital. The largest city is Sydney.[15]
18
+
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+ Australia is a very big country, but much of the land is very dry, and the middle of the continent is mostly desert. Only the areas around the east, west and south coast have enough rain and a suitable climate (not too hot) for many farms and cities.
20
+
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+ The Australian Aboriginal people arrived in Australia about 50,000 years ago or even earlier.[16][17][18] Until the arrival of British settlers in 1788, the Aboriginal people lived by hunting and gathering food from the land. They lived in all sorts of climates and managed the land in different ways. An example of Aboriginal land management was the Cumberland Plain where Sydney is now. Every few years the Aboriginal people would burn the grass and small trees.[19] This meant that a lot of grass grew back, but not many big trees. Kangaroos like to live on grassy plains, but not in forests. The kangaroos that lived on the plain were a good food supply for the Aboriginal people. Sometimes, Aborigines would name a person after an animal, and they could not eat that animal to help level out the food population.
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+
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+ Aboriginal people did not usually build houses, except huts of grass, leaves and bark. They did not usually build walls or fences, and there were no horses, cows or sheep in Australia that needed to be kept in pens. The only Aboriginal buildings that are known are fish-traps made from stones piled up in the river, and the remains of a few stone huts in Victoria and Tasmania.[20][21][22] The Aboriginal people did not use metal or make pottery or use bows and arrows or weave cloth. In some parts of Australia the people used sharp flaked-stone spearheads, but most Aboriginal spears were made of sharply pointed wood. Australia has a lot of trees that have very hard wood that was good for spear making. The boomerang was used in some areas for sport and for hunting.
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+
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+ The Aboriginal people did not think that the land belonged to them. They believed that they had grown from the land, so it was like their mother, and they belonged to the land.
26
+
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+ In the 1600s, Dutch merchants traded with the islands of Batavia (now Indonesia), to the north of Australia and several different Dutch ships touched on the coast of Australia. The Dutch governor, van Diemen, sent Abel Tasman on a voyage of discovery and he found Tasmania, which he named Van Diemen's Land. Its name was later changed to honour the man who discovered it.
28
+
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+ The British Government was sure that there must be a very large land in the south, that had not been explored. They sent Captain James Cook to the Pacific Ocean. His ship, HMS Endeavour, carried the famous scientists, Sir Joseph Banks and Dr Solander who were going to Tahiti where they would watch the planet Venus pass in front of the Sun. Captain Cook's secret mission was to find "Terra Australis" (the Land of the South).
30
+
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+ The voyage of discovery was very successful, because they found New Zealand and sailed right around it. Then they sailed westward. At last, a boy, William Hicks, who was up the mast spotted land on the horizon. Captain Cook named that bit of land Point Hicks. They sailed up the coast and Captain Cook named the land that he saw "New South Wales". At last they sailed into a large open bay which was full of fish and stingrays which the sailors speared for food. Joseph Banks and Dr. Solander went ashore and were astonished to find that they did not know what any of the plants or birds or animals that they saw were. They collected hundreds of plants to take back to England.
32
+
33
+ Captain Cook saw the Aboriginal people with their simple way of life. He saw them fishing and hunting and collecting grass seeds and fruit. But there were no houses and no fences. In most parts of the world, people put up a house and a fence or some marker to show that they own the land. But the Aboriginal people did not own the land in that way. They belonged to the land, like a baby belongs to its mother. Captain Cook went home to England and told the government that no-one owned the land. This would later cause a terrible problem for the Aboriginal people.
34
+
35
+ In the 1700s, in England, laws were tough, many people were poor and gaols (jails) were full. A person could be sentenced to death for stealing a loaf of bread. Many people were hung for small crimes. But usually they were just thrown in gaol. Often they were sent away to the British colonies in America. But by the 1770s, the colonies in America became the United States. They were free from British rule and would not take England's convicts any more, so England needed to find a new and less populated place.
36
+
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+ By the 1780s the gaols of England were so full that convicts were often chained up in rotting old ships. The government decided to make a settlement in New South Wales and send some of the convicts there. In 1788 the First Fleet of eleven ships set sail from Portsmouth carrying convicts, sailors, marines, a few free settlers and enough food to last for two years. Their leader was Captain Arthur Phillip. They were to make a new colony at the place that Captain Cook had discovered, named Botany Bay because of all the unknown plants found there by the two scientists.
38
+
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+ Captain Phillip found that Botany Bay was flat and windy. There was not much fresh water. He went with two ships up the coast and sailed into a great harbor which he said was "the finest harbor in the world!" There were many small bays on the harbor so he decided on one which had a good stream of fresh water and some flat shore to land on. On 26 January 1788, the flag was raised and New South Wales was claimed in the name of King George III of England, and the new settlement was called Sydney.
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+ For the first few years of the settlement, things were very difficult. No-one in the British Government had thought very hard about what sort of convicts should be sent to make a new colony. Nobody had chosen them carefully. There was only one man who was a farmer. There was no-one among the convicts who was a builder, a brick-maker or a blacksmith. No-one knew how to fix the tools when they broke. All of the cattle escaped. There were no cooking pots. All the plants were different so no-one knew which ones could be eaten. It was probable that everyone in the new colony would die of starvation.
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+
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+ Somehow, the little group of tents with a hut for the Governor, Arthur Phillip, and another hut for the supply of food, grew into a small town with streets, a bridge over the stream, a windmill for grinding grain and wharves for ships. By the 1820s there was a fine brick house for the Governor. There was also a hospital and a convict barracks and a beautiful church which are still standing today. Settlements had spread out from Sydney, firstly to Norfolk Island and to Van Diemen's Land (Tasmania), and also up the coast to Newcastle, where coal was discovered, and inland where the missing cattle were found to have grown to a large herd. Spanish Merino sheep had been brought to Sydney, and by 1820, farmers were raising fat lambs for meat and also sending fine wool back to the factories of England.
44
+
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+ While the settlement was growing in New South Wales, it was also growing in Tasmania. The climate in Tasmania was more like that in England, and farmers found it easy to grow crops there.
46
+
47
+ Because Australia is such a very large land, it was easy to think that it might be able to hold a very large number of people. In the early days of the colony, a great number of explorers went out, searching for good land to settle on.
48
+ When the settlers looked west from Sydney, they saw a range of mountains which they called the Blue Mountains. They were not very high and did not look very rugged but for many years no-one could find their way through them. In 1813 Gregory Blaxland, William Lawson and a 17-year-old called William Charles Wentworth crossed the Blue Mountains and found land on the other side which was good for farming. A road was built and the governor, Lachlan Macquarie founded the town of Bathurst on the other side, 100 miles from Sydney.
49
+
50
+ Some people, like Captain Charles Sturt were sure that there must be a sea in the middle of Australia and set out to find it. Many of the explorers did not prepare very well, or else they went out to explore at the hottest time of year. Some died like Burke and Wills. Ludwig Leichhardt got lost twice. The second time, he was never seen again. Major Thomas Mitchell was one of the most successful explorers. He mapped the country as he went, and his maps remained in use for more than 100 years. He travelled all the way to what is now western Victoria, and to his surprise and annoyance found that he was not the first white person there. The Henty brothers had come from Tasmania, had built themselves a house, had a successful farm and fed the Major and his men on roast lamb and wine.
51
+
52
+ The gold rushes of New South Wales and Victoria started in 1851 leading to large numbers of people arriving to search for gold. The population grew across south east Australia and made great wealth and industry. By 1853 the gold rushes had made some poor people, very rich.
53
+
54
+ The transportation of convicts to Australia ended in the 1840s and 1850s and more changes came. The people in Australia wanted to run their own country, and not be told what to do from London. The first governments in the colonies were run by governors chosen by London. Soon the settlers wanted local government and more democracy. William Wentworth started the Australian Patriotic Association (Australia's first political party) in 1835 to demand democratic government. In 1840, the city councils started and some people could vote. New South Wales Legislative Council had its first elections in 1843, again with some limits on who could vote. In 1855, limited self-government was given by London to New South Wales, Victoria, South Australia and Tasmania. In 1855, the right to vote was given to all men over 21 in South Australia. The other colonies soon followed. Women were given the vote in the Parliament of South Australia in 1895 and they became the first women in the world allowed to stand in elections.[23][24]
55
+
56
+ Australians had started parliamentary democracies all across the continent. But voices were getting louder for all of them to come together as one country with a national parliament.
57
+
58
+ Until 1901, Australia was not a nation, it was six separate colonies governed by Britain. They voted to join together to form one new country, called the Commonwealth of Australia, in 1901. Australia was still part of the British Empire, and at first wanted only British or Europeans to come to Australia. But soon it had its own money, and its own Army and Navy.
59
+
60
+ In Australia at this time, the trade unions were very strong, and they started a political party, the Australian Labor Party. Australia passed many laws to help the workers.[26]
61
+
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+ In 1914, the First World War started in Europe. Australia joined in on the side of Britain against Germany, Austria-Hungary and the Ottoman Empire. Australian soldiers were sent to Gallipoli, in the Ottoman Empire. They fought bravely, but were beaten by the Turks. Today Australia remembers this battle every year on ANZAC Day. They also fought on the Western Front. More than 60,000 Australians were killed.
63
+
64
+ Australia had a really hard time in the Great Depression of the 1930s and joined Britain in a war against Nazi Germany when Hitler invaded Poland in 1939. But in 1941 lots of Australian soldiers were captured in the Fall of Singapore by Japan. Then Japan started attacking Australia and people worried about invasion. But with help from the United States Navy, the Japanese were stopped. After the war, Australia became a close friend of the United States.
65
+
66
+ When the war ended, Australia felt that it needed many more people to fill the country up and to work. So the government said it would take in people from Europe who had lost their homes in the war. It did things like building the Snowy Mountains Scheme. Over the next 25 years, millions of people came to Australia. They came especially from Italy and Greece, other countries in Europe. Later they also came from countries like Turkey and Lebanon. An important new party, the Liberal Party of Australia was made by Robert Menzies in 1944 and it won lots of elections from 1949 until in 1972, then Gough Whitlam won for the Labor Party. Whitlam made changes, but he made the Senate unhappy and the Governor-General sacked him and forced an election in 1975. Then Malcolm Fraser won a few elections for the Liberal Party.
67
+
68
+ In the 1960s many people began coming to Australia from China, Vietnam, Malaysia and other countries in Asia. Australia became more multicultural. In the 1950s and 1960s Australia became one of the richest countries in the world, helped by mining and wool. Australia started trading more with America, than Japan. Australia supported the United States in wars against dictatorships in Korea and Vietnam and later Iraq. Australian soldiers also helped the United Nations in countries like East Timor in 1999.
69
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+ In 1973, the famous Sydney Opera House opened. In the 1970s, 80s and 90s lots of Australian movies, actors and singers became famous around the world. In the year 2000, Sydney had the Summer Olympics.
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+ In the 1980s and 90s, the Labor Party under Bob Hawke and Paul Keating, then the Liberal Party under John Howard made lots of changes to the economy. Australia had a bad recession in 1991, but when other Western countries had trouble with their economies in 2008, Australia stayed strong.
73
+
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+ Today Australia is a rich, peaceful and democratic country. But it still has problems. Around 4-5% of Australians could not get a job in 2010. A lot of land in Australia (like Uluru) has been returned to Aboriginal people, but lots of Aborigines are still poorer than everybody else. Every year the government chooses a big number of new people from all around the world to come as immigrants to live in Australia. These people may come because they want to do business, or to live in a democracy, to join their family, or because they are refugees. Australia took 6.5 million immigrants in the 60 years after World War Two, including around 660,000 refugees.[27]
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+ Julia Gillard became the first woman Prime Minister of Australia in 2010 when she replaced her colleague Kevin Rudd of the Labor Party.
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+ Australia is made up of six states, and two mainland territories. Each state and territory has its own Parliament and makes its own local laws. The Parliament of Australia sits in Canberra and makes laws for the whole country, also known as the Commonwealth or Federation.
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+ The Federal government is led by the Prime Minister of Australia, who is the member of Parliament chosen as leader. The current Prime Minister is Scott Morrison.
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+ The leader of Australia is the Prime Minister, although the Governor-General represents the Queen of Australia, who is also the Queen of Great Britain, as head of state. The Governor-General, currently His Excellency David Hurley, is chosen by the Prime Minister.
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+
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+ Australia was colonised by people from Britain,[28] but today people from all over the world live there. English is the main spoken language, and Christianity is the main religion, though all religions are accepted and not everybody has a religion. Australia is multicultural, which means that all its people are encouraged to keep their different languages, religions and ways of life, while also learning English and joining in with other Australians.
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+ Famous Australian writers include the bush balladeers Banjo Paterson and Henry Lawson who wrote about life in the Australian bush. More modern famous writers include Peter Carey, Thomas Keneally and Colleen McCullough. In 1973, Patrick White won the Nobel Prize in Literature, the only Australian to have achieved this; he is seen as one of the great English-language writers of the twentieth century.
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+
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+ Australian music has had lots of world-wide stars, for example the opera singers Nellie Melba and Joan Sutherland, the rock and roll bands Bee Gees, AC/DC and INXS, the folk-rocker Paul Kelly (musician), the pop singer Kylie Minogue and Australian country music stars Slim Dusty and John Williamson. Australian Aboriginal music is very special and very ancient: it has the famous digeridoo woodwind instrument.
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+ Australian TV has produced many successful programs for home and overseas - including Skippy the Bush Kangaroo, Home and Away and Neighbours - and produced such well known TV stars as Barry Humphries (Dame Edna Everage), Steve Irwin (The Crocodile Hunter) and The Wiggles. Major Australian subgroups such as the Bogan have been shown on Australian TV in shows such as Bogan Hunters and Kath & Kim.[29]
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+ Australia has two public broadcasters (the ABC and the multi-cultural SBS), three commercial television networks, three pay-TV services, and numerous public, non-profit television and radio stations. Each major city has its daily newspapers, and there are two national daily newspapers, The Australian and The Australian Financial Review.
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+ Australian movies have a very long history. The world's first feature movie was the Australian movie The Story of the Kelly Gang of 1906.[30] In 1933, In the Wake of the Bounty, directed by Charles Chauvel, had Errol Flynn as the main actor.[31] Flynn went on to a celebrated career in Hollywood. The first Australian Oscar was won by 1942's Kokoda Front Line!, directed by Ken G. Hall.[32] In the 1970s and 1980s lots of big Australian movies and movie stars became world famous with movies like Picnic at Hanging Rock, Gallipoli (with Mel Gibson), The Man From Snowy River and Crocodile Dundee.[33] Russell Crowe, Cate Blanchett and Heath Ledger became global stars during the 1990s and Australia starring Nicole Kidman and Hugh Jackman made a lot of money in 2008.
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+ Australia is also a popular destination for business conferences and research, with Sydney named as one of the top 20 meeting destinations in the world.[34]
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+ Sport is an important part of Australian culture because the climate is good for outdoor activities. 23.5% Australians over the age of 15 regularly take part in organised sporting activities.[35] In international sports, Australia has very strong teams in cricket, hockey, netball, rugby league and rugby union, and performs well in cycling, rowing and swimming. Local popular sports include Australian Rules Football, horse racing, soccer and motor racing. Australia has participated in every summer Olympic Games since 1896, and every Commonwealth Games. Australia has hosted the 1956 and 2000 Summer Olympics, and has ranked in the top five medal-winners since 2000. Australia has also hosted the 1938, 1962, 1982 and 2006 Commonwealth Games and are to host the 2018 Commonwealth Games. Other major international events held regularly in Australia include the Australian Open, one of the four Grand Slam tennis tournaments, annual international cricket matches and the Formula One Australian Grand Prix. Corporate and government sponsorship of many sports and elite athletes is common in Australia. Televised sport is popular; some of the highest-rated television programs include the Summer Olympic Games and the grand finals of local and international football competitions.
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+ The main sporting leagues for males are the Australian Football League, National Rugby League, A-League and NBL.
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+ For women, they are ANZ Netball Championships, W-League and WNBL.
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+ Famous Australian sports players include the cricketer Sir Donald Bradman, the swimmer Ian Thorpe and the athlete Cathy Freeman.
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+ Just 60 years ago, Australia had only one big art festival. Now Australia has hundreds of smaller community-based festivals, and national and regional festivals that focus on specific art forms.[36]
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+ Australia is home to many animals that can be found nowhere else on Earth, which include: the Koalas,the Kangaroos, the Wombat, the Numbat, the Emu, among many others. Most of the marsupials in the world are found only on the continent.
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+ Africa
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+ Antarctica
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+ Asia
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+ Australia
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+ Europe
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+ North America
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+ South America
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+ Afro-Eurasia
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+ Americas
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+ Eurasia
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+ Oceania
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+ Wikipedia does not yet have an article with this name.
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+ A gas giant is a large planet that has a solid core, but a very thick atmosphere. This means that most of the planet is made up of gas. These planets are very large.
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+ In our outer Solar System, there are 4 gas giants: Jupiter, Saturn, Uranus, and Neptune.
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+ Jupiter and Saturn are similar because they are made up of mostly hydrogen and helium. They both contain massive rocky cores that are bigger than Earth. Neptune and Uranus are similar because they are mainly made up of water and rock (a mixture of one or several minerals).
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+ Gas giants have also been found around other stars than the sun. Most of those giant extrasolar planets are "hot giants" orbiting close to their star.
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+ Ices:
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+ Jupiter is the largest planet in the Solar System.[10] It is the fifth planet from the Sun.[11] Jupiter is a gas giant, both because it is so large and made up of gas. The other gas giants are Saturn, Uranus, and Neptune.
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+
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+ Jupiter has a mass of 1.8986×1027 kg, or about 318 Earths. This is twice the mass of all the other planets in the Solar System put together.[12]
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+ Jupiter can be seen even without the use of telescope. It was known to the ancient Romans, who named it after their god Jupiter (Latin: Iuppiter).[13][14] Jupiter is the third brightest object in the night sky. Only the Earth's moon and Venus are brighter.[15][16]
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+ Jupiter has at least 79 moons. Of these, around 50 are very small and less than five kilometres wide. The four largest moons of Jupiter are Io, Europa, Ganymede, and Callisto. They are called the Galilean moons, because Galileo Galilei discovered them. Ganymede is the largest moon in the Solar System. It is larger in diameter than Mercury. In 2018 another ten very small moons were discovered [17]
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+ Jupiter is the biggest planet in the Solar System with a diameter of 142,984 km. This is eleven times bigger than the diameter of Earth.[18]
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+ The atmosphere near the surface of Jupiter is made of about 88 to 92% hydrogen, 8 to 12% helium, and 1% other gases.
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+ The lower atmosphere is so heated and the pressure so high that helium changes to liquid. It rains down onto the planet.[19] Based on spectroscopy, Jupiter seems to be made of the same gases as Saturn. It is different from Neptune or Uranus. These two planets have much less hydrogen and helium gas.[20]
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+ The very high temperatures and pressures in Jupiter's core mean scientists cannot tell what materials would be there. This cannot be found out, because it is not possible to create the same amount of pressure on Earth.
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+ Above the unknown inner core is an outer core. The outer core of Jupiter is thick, liquid hydrogen.[21] The pressure is high enough to make the hydrogen solid, but then it melts because of the heat.
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+ Jupiter is twice as massive as all the other planets in the Solar System put together.[12] It gives off more heat than it gets from the sun.[22]
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+ Jupiter is 11 times the width of Earth and 318 times as massive. The volume of Jupiter is 1,317 times the volume of Earth. In other words, 1,317 Earth-sized objects could fit inside it.[23]
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+ Jupiter has many bands of clouds going horizontally across its surface. The light parts are zones and the darker are belts. The zones and belts often interact with each other. This causes huge storms. Wind speeds of 360 kilometres per hour (km/h) are common on Jupiter.[24] To show the difference the strongest tropical storms on Earth are about 100 km/h.[25]
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+ Most of the clouds on Jupiter are made of ammonia.[26] There may also be clouds of water vapour like clouds on Earth. Spacecrafts such as Voyager 1 have seen lightning on the surface of the planet. Scientists think it was water vapour because lightning needs water vapour.[27] These lightning bolts have been measured as up 1,000 times as powerful as those on Earth.[27]
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+ The brown and orange colours are caused when sunlight passes through or refracts with the many gases in the atmosphere.
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+ One of the biggest features in Jupiter's atmosphere is the Great Red Spot. It is a huge storm which is bigger than the entire Earth. It is on record since at least 1831,[28] and as early as 1665.[29][30] Images by the Hubble Space Telescope have shown as many as two smaller "red spots" right next to the Great Red Spot.[31][32] Storms can last for hours or as long as hundreds of years in the case of the Great Red Spot.[33][34]
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+ Jupiter has a magnetic field like Earth's but 11 times stronger.[35] It also has a magnetosphere much bigger and stronger than Earth's. The field traps radiation belts much stronger than Earth's Van Allen radiation belts, strong enough to endanger any spacecraft travelling past or to Jupiter. The magnetic field is probably caused by the large amounts of liquid metallic hydrogen in the core of Jupiter.[36] The four largest moons of Jupiter and many of the smaller ones orbit or go around the planet within the magnetic field. This protects them from the solar wind. Jupiter's magnetic field is so large, it reaches the orbit of Saturn 7.7 million miles (12 million km) away.[37] The Earth's magnetosphere does not even cover its moon, less than a quarter of a million miles (400,000 km) away.
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+ Jupiter also has a thin planetary ring system.[38] These rings are difficult to see and were not discovered until 1979 by NASA's Voyager 1 probe.[39] There are four parts to Jupiter's rings. The closest ring to Jupiter is called the Halo Ring.[40] The next ring is called the Main Ring. It is about 6,440 km (4,002 mi) wide and only 30 km (19 mi) thick.[40] The Main and Halo rings of Jupiter are made of small, dark particles.[39] The third and fourth rings, called the Gossamer Rings, are transparent (see through) and are made from microscopic debris and dust.[39] This dust probably comes from small meteors striking the surface of Jupiter's moons. The third ring is called the Amalthea Gossamer Ring, named after moon Amalthea. The outer ring, the Thebe Gossamer Ring, is named after the moon Thebe. The outer edge of this ring is about 220,000 km (136,702 mi) from Jupiter.[40]
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+ The orbit of a planet is the time and path it takes to go around the Sun. In the amount of time it takes for Jupiter to orbit the Sun one time, the Earth orbits the Sun 11.86 times.[41] One year on Jupiter is equal to 11.86 years on Earth. The average distance between Jupiter and the Sun is 778 million kilometres. This is five times the distance between Earth and the Sun. Jupiter is not tilted on its axis as much as Earth or Mars. This causes it to have no seasons, for example summer or winter. Jupiter rotates, or spins around very quickly.[42] This causes the planet to bulge in the middle. Jupiter is the fastest spinning planet in the Solar System.[42] It completes one rotation or spin in 10 hours.[11] Because of the bulge, the length of the equator of Jupiter is much longer than the length from pole to pole.[43]
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+ Jupiter is the third brightest object in the night sky, after the Moon and Venus.[15] Because of that, people have always been able to see it from Earth. The first person known to really study the planet was Galileo Galilei in 1610.[44] He was the first person to see Jupiter's moons Io, Europa, Ganymede and Callisto.[44] This was because he used a telescope, unlike anyone before him.
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+ No new moons were discovered for more than two hundred years. In 1892, astronomer E.E Barnard found a new moon using his observatory in California. He called the moon Amalthea.[45] It was the last of Jupiter's 67 moons to be discovered by human observation through a telescope.[44]
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+ In 1994, bits of the comet Shoemaker Levy-9 hit Jupiter. It was the first time people saw a collision between two Solar System objects.[46]
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+
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+ Seven spacecraft have flown past Jupiter since 1973.[11] These were Pioneer 10 (1973), Pioneer 11 (1974), Voyagers 1 and 2 (1979), Ulysses (1992 and 2004), Cassini (2000) and New Horizons (2007).
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+
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+ The Pioneer missions were the first spacecraft to take close up pictures of Jupiter and its moons. Five years later, the two Voyager spacecraft discovered over 20 new moons. They captured photo evidence of lightning on the night side of Jupiter.[47]
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+ The Ulysses probe was sent to study the Sun. It only went to Jupiter after it had finished its main mission. Ulysses had no cameras so it took no photographs.
47
+ In 2006, the Cassini spacecraft, on its way to Saturn, took some very good, very clear pictures of the planet. Cassini also found a moon and took a picture of it but it was too far away to show the details.[48]
48
+
49
+ The Galileo mission in 1995 was the first spacecraft to go into orbit around Jupiter. It flew around the planet for seven years and studied the four biggest moons. It launched a probe into the planet to get information about Jupiter's atmosphere. The probe travelled to a depth of about 150 km before it was crushed by the weight of all the gas above it.[49] This is called pressure. The Galileo spacecraft was also crushed in 2003 when NASA steered the craft into the planet. They did this so that the craft could not crash into Europa, a moon which scientists think might have life.[49]
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+ NASA have sent another spacecraft to Jupiter called Juno. It was launched on August 5, 2011[50] and arrived at Jupiter on July 4, 2016.[51] NASA published some results from the Juno mission in March 2018.[52] Several other missions have been planned to send spacecraft to Jupiter's moons Europa and Callisto. One called JIMO (Jupiter Icy Moons Orbiter) was cancelled in 2006 because it cost too much money.[53]
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+
53
+ Jupiter has 79 known moons. The four largest were seen by Galileo with his primitive telescope, and nine more can be seen from Earth with modern telescopes. The rest of the moons have been identified by spacecraft.[54] The smallest moon (S/2003 J 12) is only one kilometre across. The largest, Ganymede, has a diameter of 5,262 kilometres. It is bigger than the planet Mercury.[55] The other three Galilean moons are Io, Europa and Callisto. Because of the way they orbit Jupiter, gravity affects three of these moons greatly. The friction caused by the gravity of Europa and Ganymede pulling on Io makes it the most volcanic object in the Solar System. It has over 400 volcanoes, more than three times as many as Earth.[56]
54
+
55
+ Jupiter's large gravity has had an effect on the Solar System. Jupiter protects the inner planets from comets by pulling them towards itself. Because of this, Jupiter has the most comet impacts in the Solar System.[46]
56
+
57
+ Two groups of asteroids, called Trojan asteroids, have settled into Jupiter's orbit round the Sun. One group is called the Trojans and the other group is called the Greeks. They go around the Sun at the same time as Jupiter.[57][58]
58
+
59
+ Notes
60
+
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1
+ Mars may mean:
ensimple/4644.html.txt ADDED
@@ -0,0 +1,11 @@
 
 
 
 
 
 
 
 
 
 
 
 
1
+ Mercury is the smallest planet in the Solar System.[8][9][10] It is the closest planet to the sun.[11] It makes one trip around the Sun once every 87.969 days.[2][12] Mercury is bright when it is visible from Earth, ranging from −2.0 to 5.5 in apparent magnitude. It cannot be easily seen as it is usually too close to the Sun. Because Mercury is normally lost in the glare of the Sun, Mercury can only be seen in the morning or evening twilight[13] or during a solar eclipse.
2
+
3
+ Less is known about Mercury than about other planets of our Solar System. Telescopes on the Earth show only a small, bright crescent, and putting a satellite in orbit around it is difficult. The first of two spacecraft to visit the planet was Mariner 10,[14] which mapped only about 45% of the planet’s surface from 1974 to 1975. The second is the MESSENGER spacecraft, which finished mapping the planet in March 2013.
4
+
5
+ Mercury looks like Earth's Moon. It has many craters and areas of smooth plains, no moons around it and no atmosphere as we know it. However, Mercury does have an extremely thin atmosphere, known as an exosphere.[11] Unlike Earth's Moon, Mercury has a large iron core, which gives off a magnetic field about 1% as strong as that of the Earth.[15] It is a very dense planet due to the large size of its core. Surface temperatures can be anywhere from about 90 to 700 K (−183 °C to 427 °C, −297 °F to 801 °F),[16] with the subsolar point being the hottest and the bottoms of craters near the poles being the coldest.
6
+
7
+ Known sightings of Mercury date back to at least the first millennium BC. Before the 4th century BC, Greek astronomers thought that Mercury was two different objects: one able to be seen only at sunrise, which they called Apollo; the other that was only able to be seen at sunset, which they called Hermes.[17] The English name for the planet is from the Romans, who named it after the Roman god Mercury, which they thought to be the same as the Greek god Hermes. The symbol for Mercury is based on Hermes' staff.[18]
8
+
9
+ Even though Mercury is the closest planet to the Sun, it is not the warmest. This is because it has no greenhouse effect, so any heat that the Sun gives to it quickly escapes into space. The hottest planet is Venus.[19]
10
+
11
+ Mercury is one of four inner planets in the Solar System, and has a rocky body like the Earth. It is the smallest planet in the Solar System, with a radius of 2,439.7 km (1,516.0 mi).[2] Mercury is even smaller than some of the largest moons in the solar system, such as Ganymede and Titan. However, it has a greater mass than the largest moons in the solar system. Mercury is made of about 70% metallic and 30% silicate material.[20] Mercury's density is the second highest in the Solar System at 5.427 g/cm³, only a little bit less than Earth’s.[2]
ensimple/4645.html.txt ADDED
@@ -0,0 +1,11 @@
 
 
 
 
 
 
 
 
 
 
 
 
1
+ Mercury is the smallest planet in the Solar System.[8][9][10] It is the closest planet to the sun.[11] It makes one trip around the Sun once every 87.969 days.[2][12] Mercury is bright when it is visible from Earth, ranging from −2.0 to 5.5 in apparent magnitude. It cannot be easily seen as it is usually too close to the Sun. Because Mercury is normally lost in the glare of the Sun, Mercury can only be seen in the morning or evening twilight[13] or during a solar eclipse.
2
+
3
+ Less is known about Mercury than about other planets of our Solar System. Telescopes on the Earth show only a small, bright crescent, and putting a satellite in orbit around it is difficult. The first of two spacecraft to visit the planet was Mariner 10,[14] which mapped only about 45% of the planet’s surface from 1974 to 1975. The second is the MESSENGER spacecraft, which finished mapping the planet in March 2013.
4
+
5
+ Mercury looks like Earth's Moon. It has many craters and areas of smooth plains, no moons around it and no atmosphere as we know it. However, Mercury does have an extremely thin atmosphere, known as an exosphere.[11] Unlike Earth's Moon, Mercury has a large iron core, which gives off a magnetic field about 1% as strong as that of the Earth.[15] It is a very dense planet due to the large size of its core. Surface temperatures can be anywhere from about 90 to 700 K (−183 °C to 427 °C, −297 °F to 801 °F),[16] with the subsolar point being the hottest and the bottoms of craters near the poles being the coldest.
6
+
7
+ Known sightings of Mercury date back to at least the first millennium BC. Before the 4th century BC, Greek astronomers thought that Mercury was two different objects: one able to be seen only at sunrise, which they called Apollo; the other that was only able to be seen at sunset, which they called Hermes.[17] The English name for the planet is from the Romans, who named it after the Roman god Mercury, which they thought to be the same as the Greek god Hermes. The symbol for Mercury is based on Hermes' staff.[18]
8
+
9
+ Even though Mercury is the closest planet to the Sun, it is not the warmest. This is because it has no greenhouse effect, so any heat that the Sun gives to it quickly escapes into space. The hottest planet is Venus.[19]
10
+
11
+ Mercury is one of four inner planets in the Solar System, and has a rocky body like the Earth. It is the smallest planet in the Solar System, with a radius of 2,439.7 km (1,516.0 mi).[2] Mercury is even smaller than some of the largest moons in the solar system, such as Ganymede and Titan. However, it has a greater mass than the largest moons in the solar system. Mercury is made of about 70% metallic and 30% silicate material.[20] Mercury's density is the second highest in the Solar System at 5.427 g/cm³, only a little bit less than Earth’s.[2]
ensimple/4646.html.txt ADDED
@@ -0,0 +1,9 @@
 
 
 
 
 
 
 
 
 
 
1
+ Dwarf planet is the name used to classify some objects in the solar system. This definition was made on August 24, 2006 by the International Astronomical Union (IAU), and can be described as; a dwarf planet is a body orbiting the Sun that is big enough to round itself by its own gravity, but has not cleared its orbital path of other rival bodies. At the same meeting the IAU also defined the term planet for the first time. Some astronomers think that the term "dwarf planet" is too confusing and needs to be changed.
2
+
3
+ The seven dwarf planets, in order from their distance from the Sun are:
4
+
5
+ The dwarf planets, unlike the terrestrial and gas giant planets, are in more than one region of the solar system. Ceres is in the asteroid belt. The high orbital eccentricity of Pluto puts it mostly outside Neptune's orbit, but partly inside. The others are in the trans-Neptune region.
6
+
7
+ NASA's Dawn and New Horizons missions reached Ceres and Pluto, respectively, in 2015. Dawn had already orbited and observed Vesta in 2011.
8
+
9
+ There are many other dwarf planets in the solar system. Most of them are also Kuiper belt objects.
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@@ -0,0 +1,66 @@
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
1
+
2
+
3
+ Saturn is the sixth planet from the Sun in the Solar System. It is the second largest planet in the Solar System, after Jupiter. Saturn is one of the four gas giant planets, along with Jupiter, Uranus, and Neptune.
4
+
5
+ Inside Saturn is probably a core of iron, nickel, silicon and oxygen compounds, surrounded by a deep layer of metallic hydrogen, then a layer of liquid hydrogen and liquid helium and finally, an outer gaseous layer.[4]
6
+
7
+ Saturn has 67 known moons orbiting the planet. 38 are officially named and 29 are waiting to be named.[5] The largest moon is Titan, which is larger in volume than the planet Mercury. Titan is the second-largest moon in the Solar System. The largest moon is Jupiter's moon, Ganymede. There is also a very large system of rings around Saturn. These rings are made of ice with smaller amounts of rocks and dust. Some people believe that the rings were caused from a moon impact or other event. Saturn is about 1,433,000,000 km (869,000,000 mi) on average from the Sun. Saturn takes 29.6 Earth years to revolve around the Sun.
8
+
9
+ Saturn was named after the Roman god Saturnus (called Kronos in Greek mythology).[6] Saturn's symbol is ♄ which is the symbol of Saturnus' sickle.[7]
10
+
11
+ Saturn is an oblate spheroid, meaning that it is flattened at the poles, and it swells out around its equator.[8] The planet's equatorial diameter is 120,536 km (74,898 mi), while its polar diameter (the distance from the north pole to the south pole) is 108,728 km (67,560 mi); a 9% difference.[9] Saturn has a flattened shape due to its very fast rotation, once every 10.8 hours.
12
+
13
+ Saturn is the only planet in the Solar System that is less dense than water. Even though the planet's core is very dense, it has a gaseous atmosphere, so the average specific density of the planet is 0.69 g/cm3. This means if Saturn could be placed in a large pool of water, it would float.[10]
14
+
15
+ The outer part of Saturn's atmosphere is made up of about 96% hydrogen, 3% helium, 0.4% methane and 0.01% ammonia. There are also very small amounts of acetylene, ethane and phosphine.[11]
16
+
17
+ Saturn's clouds show a banded pattern, like the cloud bands seen on Jupiter. Saturn's clouds are much fainter and the bands are wider at the equator. Saturn's lowest cloud layer is made up of water ice, and is about 10 km (6 mi) thick.[11] The temperature here is quite low, at 250 K (-10°F, -23°C). However scientists do not agree about this. The layer above, about 77 km (48 mi) thick, is made up of ammonium hydrosulfide ice, and above that is a layer of ammonia ice clouds 80 km (50 mi) thick.[11] The highest layer is made up of hydrogen and helium gases, which extends between 200 km (124 mi) and 270 km (168 mi) above the water cloud tops. Auroras are also known to form in Saturn in the mesosphere.[11] The temperature at Saturn's cloud tops is extremely low, at 98 K (-283 °F, -175 °C). The temperatures in the inner layers are much higher than the outside layers because of the heat produced by Saturn's interior.[12]
18
+ Saturn's winds are some of the fastest in the Solar System, reaching 1,800 km/h (1,118 mph),[13] ten times faster than winds on Earth.[14]
19
+
20
+ Saturn's atmosphere is also known to form oval shaped clouds, similar to the clearer spots seen in Jupiter. These oval spots are cyclonic storms, the same as cyclones seen on Earth. In 1990, the Hubble Space Telescope found a very large white cloud near Saturn's equator. Storms like the one in 1990 were known as Great White Spots. These unique storms only exist for a short time and only happen about every 30 Earth years, at the time of the summer solstice in the Northern Hemisphere.[15]
21
+ Great White Spots were also found in 1876, 1903, 1933, and 1960. If this cycle continues, another storm will form in about 2020.[16]
22
+
23
+ The Voyager 1 spacecraft found a hexagonal cloud pattern near Saturn's north pole at about 78°N. The Cassini−Huygens probe later confirmed it in 2006. Unlike the north pole, the south pole does not show any hexagonal cloud feature. The probe also discovered a hurricane-like storm locked to the south pole that clearly showed an eyewall. Until this discovery, eyewalls had only been seen on Earth.[17]
24
+
25
+ Saturn's interior is similar to Jupiter's interior. It has a small rocky core about the size of the Earth at its center.[8] It is very hot; its temperature reaches 15,000 K (26,540 °F (14,727 °C)). Saturn is so hot that it gives out more heat energy into space than it receives from the Sun.[12] Above it is a thicker layer of metallic hydrogen, about 30,000 km (18,641 mi) deep. Above that layer is a region of liquid hydrogen and helium.[18] The core is heavy, with about 9 to 22 times more mass than the Earth's core.[19]
26
+
27
+ Saturn has a natural magnetic field that is weaker than Jupiter's. Like the Earth's, Saturn's field is a magnetic dipole. Saturn's field is unique in that it is perfectly symmetrical, unlike any other known planet.[20] This means the field is exactly in line with the planet's axis.[20] Saturn generates radio waves, but they are too weak to be detected from Earth.[21] The moon Titan orbits in the outer part of Saturn's magnetic field and gives out plasma to the field from the ionised particles in Titan's atmosphere.[22]
28
+
29
+ Saturn's average distance from the Sun is over 1,400,000,000 km (869,000,000 mi), about nine times the distance from the Earth to the Sun. It takes 10,759 days, or about 29.8 years, for Saturn to orbit around the Sun.[23] This is known as Saturn's orbital period.
30
+
31
+ Voyager 1 measured Saturn's rotation as being 10 hours 14 minutes at the equator, 10 hours 40 minutes closer to the poles, and 10 hours 39 minutes 24 seconds for the planet's interior.[24] This is known as its rotational period.
32
+
33
+ Cassini measured the rotation of Saturn as being 10 hours 45 minutes 45 seconds ± 36 seconds.[25] That is about six minutes, or one percent, longer than the radio rotational period measured by the Voyager 1 and Voyager 2 spacecraft, which flew by Saturn in 1980 and 1981.
34
+
35
+ Saturn's rotational period is calculated by the rotation speed of radio waves released by the planet. The Cassini−Huygens spacecraft discovered that the radio waves slowed down, suggesting that the rotational period increased.[25] Since the scientists do not think Saturn's rotation is actually slowing down, the explanation may lie in the magnetic field that causes the radio waves.[25]
36
+
37
+ Saturn is best known for its planetary rings which are easy to see with a telescope. There are seven named rings; A, B, C, D, E, F, and G rings.[26] They were named in the order they were discovered, which is different to their order from the planet. From the planet the rings are: D, C, B, A, F, G and E.[26]:57
38
+
39
+ Scientists believe that the rings are material left after a moon broke apart.[26]:60 A new idea says that it was a very large moon, most of which crashed into the planet. This left a large amount of ice to form the rings, and also some of the moons, like Enceladus, which are thought to be made of ice.[26]:61
40
+
41
+ The rings were first discovered by Galileo Galilei in 1610, using his telescope. They did not look like rings to Galileo, so he called them "handles". He thought that Saturn was three separate planets that almost touched one another. In 1612, when the rings were facing edge on with the Earth, the rings disappeared, then reappeared again in 1613, further confusing Galileo.[27] In 1655, Christiaan Huygens was the first person to recognise Saturn was surrounded by rings. Using a much more powerful telescope than Galilei's, he noted Saturn "is surrounded by a thin, flat, ring, nowhere touching...".[27] In 1675, Giovanni Domenico Cassini discovered that the planet's rings were in fact made of smaller ringlets with gaps. The largest ring gap was later named the Cassini Division. In 1859, James Clerk Maxwell showed that the rings cannot be solid, but are made of small particles, each orbiting Saturn on their own, otherwise, it would become unstable or break apart.[28] James Keeler studied the rings using a spectroscope in 1895 which proved Maxwell's theory.[29]
42
+
43
+ The rings range from 6,630 km (4,120 mi) to 120,700 km (75,000 mi) above the planet's equator. As proved by Maxwell, even though the rings appear to be solid and unbroken when viewed from above, the rings are made of small particles of rock and ice. They are only about 10 m (33 ft) thick; made of silica rock, iron oxide and ice particles.[26]:55 The smallest particles are only specks of dust while the largest are the size of a house. The C and D rings also seem to have a "wave" in them, like waves in water.[26]:58 These large waves are 500 m (1,640 ft) high, but only moving slowly at about 250 m (820 ft) each day.[26]:58 Some scientists believe that the wave is caused by Saturn's moons.[30] Another idea is the waves were made by a comet hitting Saturn in 1983 or 1984.[26]:60
44
+
45
+ The largest gaps in the rings are the Cassini Division and the Encke Division, both visible from the Earth. The Cassini Division is the largest, measuring 4,800 km (2,983 mi) wide.[31] However, when the Voyager spacecrafts visited Saturn in 1980, they discovered that the rings are a complex structure, made out of thousands of thin gaps and ringlets. Scientists believe this is caused by the gravitational force of some of Saturn's moons. The tiny moon Pan orbits inside Saturn's rings, creating a gap within the rings. Other ringlets keep their structure due to the gravitational force of shepherd satellites, such as Prometheus and Pandora. Other gaps form due to the gravitational force of a large moon farther away. The moon Mimas is responsible for clearing away the Cassini gap.[31]
46
+
47
+ Recent data from the Cassini spacecraft has shown that the rings have their own atmosphere, free from the planet's atmosphere. The rings' atmosphere is made of oxygen gas, and it is produced when the Sun's ultraviolet light breaks up the water ice in the rings. Chemical reaction also occurs between the ultraviolet light and the water molecules, creating hydrogen gas. The oxygen and hydrogen atmospheres around the rings are very widely spaced.[32] As well as oxygen and hydrogen gas, the rings have a thin atmosphere made of hydroxide. This anion was discovered by the Hubble Space Telescope.[33]
48
+
49
+ The Voyager space probe discovered features shaped like rays, called spokes.[34] These were also seen later by the Hubble telescope. The Cassini probe photographed the spokes in 2005.[34] They are seen as dark when under sunlight, and appear light when against the unlit side. At first it was thought the spokes were made of microscopic dust particles but new evidence shows that they are made of ice.[35]
50
+ They rotate at the same time with the planet's magnetosphere, therefore, it is believed that they have a connection with electromagnetism. However, what causes the spokes to form is still unknown. They appear to be seasonal, disappearing during solstice and appearing again during equinox.[36]
51
+
52
+ Saturn has 53 named moons, and another nine which are still being studied.[37] Many of the moons are very small: 33 are less than 10 km (6 mi) in diameter and 13 moons are less than 50 km (31 mi).[38] Seven moons are large enough to be a near perfect sphere caused by their own gravitation. These moons are Titan, Rhea, Iapetus, Dione, Tethys, Enceladus and Mimas.[39] Titan is the largest moon, larger than the planet Mercury, and it is the only moon in the Solar System to have a thick, dense atmosphere.[40][41] Hyperion and Phoebe are the next largest moons, larger than 200 km (124 mi) in diameter.
53
+
54
+ In December 2004 and January 2005 a man-made satellite called the Cassini−Huygens probe took lots of close photos of Titan. One part of this satellite, known as the Huygens probe, then landed on Titan. Named after the Dutch astronomer Christiaan Huygens, it was the first spacecraft to land in the outer Solar System.[42] The probe was designed to float in case it landed in liquid.[42]
55
+ Enceladus, the sixth largest moon, is about 500 km (311 mi) in diameter. It is one of the few outer solar system objects that shows volcanic activity.[43] In 2011, scientists discovered an electric link between Saturn and Enceladus. This is caused by ionised particles from volcanos on the small moon interacting with Saturn's magnetic fields.[43] Similar interactions cause the northern lights on Earth.[44]
56
+
57
+ Saturn was first explored by the Pioneer 11 spacecraft in September 1979. It flew as close as 20,000 km (12,427 mi) above the planet's cloud tops. It took photographs of the planet and a few of its moons, but were low in resolution. It discovered a new, thin ring called the F ring. It also discovered that the dark ring gaps appear bright when viewed towards the Sun, which shows the gaps are not empty of material. The spacecraft measured the temperature of the moon Titan.[45]
58
+
59
+ In November 1980, Voyager 1 visited Saturn, and took higher resolution photographs of the planet, rings and moons. These photos were able to show the surface features of the moons. Voyager 1 went close to Titan, and gained much information about its atmosphere. In August, 1981, Voyager 2 continued to study the planet. Photos taken by the space probe showed that changes were happening to the rings and atmosphere. The Voyager spacecrafts discovered a number of moons orbiting close to Saturn's rings, as well as discovering new ring gaps.
60
+
61
+ On July 1, 2004, the Cassini−Huygens probe entered into orbit around Saturn. Before then, it flew close to Phoebe, taking very high resolution photos of its surface and collecting data. On December 25, 2004, the Huygens probe separated from the Cassini probe before moving down towards Titan's surface and landed there on January 14, 2005. It landed on a dry surface, but it found that large bodies of liquid exist on the moon. The Cassini probe continued to collect data from Titan and a number of the icy moons. It found evidence that the moon Enceladus had water erupting from its geysers.[46] Cassini also proved, in July 2006, that Titan had hydrocarbon lakes, located near its north pole. In March 2007, it discovered a large hydrocarbon lake the size of the Caspian Sea near its north pole.[47]
62
+
63
+ Cassini observed lightning occurring in Saturn since early 2005. The power of the lightning was measured to be 1,000 times more powerful than lightning on Earth. Astronomers believe that the lightning observed in Saturn is the strongest ever seen.[48]
64
+
65
+ Notes
66
+
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1
+
2
+
3
+ Saturn is the sixth planet from the Sun in the Solar System. It is the second largest planet in the Solar System, after Jupiter. Saturn is one of the four gas giant planets, along with Jupiter, Uranus, and Neptune.
4
+
5
+ Inside Saturn is probably a core of iron, nickel, silicon and oxygen compounds, surrounded by a deep layer of metallic hydrogen, then a layer of liquid hydrogen and liquid helium and finally, an outer gaseous layer.[4]
6
+
7
+ Saturn has 67 known moons orbiting the planet. 38 are officially named and 29 are waiting to be named.[5] The largest moon is Titan, which is larger in volume than the planet Mercury. Titan is the second-largest moon in the Solar System. The largest moon is Jupiter's moon, Ganymede. There is also a very large system of rings around Saturn. These rings are made of ice with smaller amounts of rocks and dust. Some people believe that the rings were caused from a moon impact or other event. Saturn is about 1,433,000,000 km (869,000,000 mi) on average from the Sun. Saturn takes 29.6 Earth years to revolve around the Sun.
8
+
9
+ Saturn was named after the Roman god Saturnus (called Kronos in Greek mythology).[6] Saturn's symbol is ♄ which is the symbol of Saturnus' sickle.[7]
10
+
11
+ Saturn is an oblate spheroid, meaning that it is flattened at the poles, and it swells out around its equator.[8] The planet's equatorial diameter is 120,536 km (74,898 mi), while its polar diameter (the distance from the north pole to the south pole) is 108,728 km (67,560 mi); a 9% difference.[9] Saturn has a flattened shape due to its very fast rotation, once every 10.8 hours.
12
+
13
+ Saturn is the only planet in the Solar System that is less dense than water. Even though the planet's core is very dense, it has a gaseous atmosphere, so the average specific density of the planet is 0.69 g/cm3. This means if Saturn could be placed in a large pool of water, it would float.[10]
14
+
15
+ The outer part of Saturn's atmosphere is made up of about 96% hydrogen, 3% helium, 0.4% methane and 0.01% ammonia. There are also very small amounts of acetylene, ethane and phosphine.[11]
16
+
17
+ Saturn's clouds show a banded pattern, like the cloud bands seen on Jupiter. Saturn's clouds are much fainter and the bands are wider at the equator. Saturn's lowest cloud layer is made up of water ice, and is about 10 km (6 mi) thick.[11] The temperature here is quite low, at 250 K (-10°F, -23°C). However scientists do not agree about this. The layer above, about 77 km (48 mi) thick, is made up of ammonium hydrosulfide ice, and above that is a layer of ammonia ice clouds 80 km (50 mi) thick.[11] The highest layer is made up of hydrogen and helium gases, which extends between 200 km (124 mi) and 270 km (168 mi) above the water cloud tops. Auroras are also known to form in Saturn in the mesosphere.[11] The temperature at Saturn's cloud tops is extremely low, at 98 K (-283 °F, -175 °C). The temperatures in the inner layers are much higher than the outside layers because of the heat produced by Saturn's interior.[12]
18
+ Saturn's winds are some of the fastest in the Solar System, reaching 1,800 km/h (1,118 mph),[13] ten times faster than winds on Earth.[14]
19
+
20
+ Saturn's atmosphere is also known to form oval shaped clouds, similar to the clearer spots seen in Jupiter. These oval spots are cyclonic storms, the same as cyclones seen on Earth. In 1990, the Hubble Space Telescope found a very large white cloud near Saturn's equator. Storms like the one in 1990 were known as Great White Spots. These unique storms only exist for a short time and only happen about every 30 Earth years, at the time of the summer solstice in the Northern Hemisphere.[15]
21
+ Great White Spots were also found in 1876, 1903, 1933, and 1960. If this cycle continues, another storm will form in about 2020.[16]
22
+
23
+ The Voyager 1 spacecraft found a hexagonal cloud pattern near Saturn's north pole at about 78°N. The Cassini−Huygens probe later confirmed it in 2006. Unlike the north pole, the south pole does not show any hexagonal cloud feature. The probe also discovered a hurricane-like storm locked to the south pole that clearly showed an eyewall. Until this discovery, eyewalls had only been seen on Earth.[17]
24
+
25
+ Saturn's interior is similar to Jupiter's interior. It has a small rocky core about the size of the Earth at its center.[8] It is very hot; its temperature reaches 15,000 K (26,540 °F (14,727 °C)). Saturn is so hot that it gives out more heat energy into space than it receives from the Sun.[12] Above it is a thicker layer of metallic hydrogen, about 30,000 km (18,641 mi) deep. Above that layer is a region of liquid hydrogen and helium.[18] The core is heavy, with about 9 to 22 times more mass than the Earth's core.[19]
26
+
27
+ Saturn has a natural magnetic field that is weaker than Jupiter's. Like the Earth's, Saturn's field is a magnetic dipole. Saturn's field is unique in that it is perfectly symmetrical, unlike any other known planet.[20] This means the field is exactly in line with the planet's axis.[20] Saturn generates radio waves, but they are too weak to be detected from Earth.[21] The moon Titan orbits in the outer part of Saturn's magnetic field and gives out plasma to the field from the ionised particles in Titan's atmosphere.[22]
28
+
29
+ Saturn's average distance from the Sun is over 1,400,000,000 km (869,000,000 mi), about nine times the distance from the Earth to the Sun. It takes 10,759 days, or about 29.8 years, for Saturn to orbit around the Sun.[23] This is known as Saturn's orbital period.
30
+
31
+ Voyager 1 measured Saturn's rotation as being 10 hours 14 minutes at the equator, 10 hours 40 minutes closer to the poles, and 10 hours 39 minutes 24 seconds for the planet's interior.[24] This is known as its rotational period.
32
+
33
+ Cassini measured the rotation of Saturn as being 10 hours 45 minutes 45 seconds ± 36 seconds.[25] That is about six minutes, or one percent, longer than the radio rotational period measured by the Voyager 1 and Voyager 2 spacecraft, which flew by Saturn in 1980 and 1981.
34
+
35
+ Saturn's rotational period is calculated by the rotation speed of radio waves released by the planet. The Cassini−Huygens spacecraft discovered that the radio waves slowed down, suggesting that the rotational period increased.[25] Since the scientists do not think Saturn's rotation is actually slowing down, the explanation may lie in the magnetic field that causes the radio waves.[25]
36
+
37
+ Saturn is best known for its planetary rings which are easy to see with a telescope. There are seven named rings; A, B, C, D, E, F, and G rings.[26] They were named in the order they were discovered, which is different to their order from the planet. From the planet the rings are: D, C, B, A, F, G and E.[26]:57
38
+
39
+ Scientists believe that the rings are material left after a moon broke apart.[26]:60 A new idea says that it was a very large moon, most of which crashed into the planet. This left a large amount of ice to form the rings, and also some of the moons, like Enceladus, which are thought to be made of ice.[26]:61
40
+
41
+ The rings were first discovered by Galileo Galilei in 1610, using his telescope. They did not look like rings to Galileo, so he called them "handles". He thought that Saturn was three separate planets that almost touched one another. In 1612, when the rings were facing edge on with the Earth, the rings disappeared, then reappeared again in 1613, further confusing Galileo.[27] In 1655, Christiaan Huygens was the first person to recognise Saturn was surrounded by rings. Using a much more powerful telescope than Galilei's, he noted Saturn "is surrounded by a thin, flat, ring, nowhere touching...".[27] In 1675, Giovanni Domenico Cassini discovered that the planet's rings were in fact made of smaller ringlets with gaps. The largest ring gap was later named the Cassini Division. In 1859, James Clerk Maxwell showed that the rings cannot be solid, but are made of small particles, each orbiting Saturn on their own, otherwise, it would become unstable or break apart.[28] James Keeler studied the rings using a spectroscope in 1895 which proved Maxwell's theory.[29]
42
+
43
+ The rings range from 6,630 km (4,120 mi) to 120,700 km (75,000 mi) above the planet's equator. As proved by Maxwell, even though the rings appear to be solid and unbroken when viewed from above, the rings are made of small particles of rock and ice. They are only about 10 m (33 ft) thick; made of silica rock, iron oxide and ice particles.[26]:55 The smallest particles are only specks of dust while the largest are the size of a house. The C and D rings also seem to have a "wave" in them, like waves in water.[26]:58 These large waves are 500 m (1,640 ft) high, but only moving slowly at about 250 m (820 ft) each day.[26]:58 Some scientists believe that the wave is caused by Saturn's moons.[30] Another idea is the waves were made by a comet hitting Saturn in 1983 or 1984.[26]:60
44
+
45
+ The largest gaps in the rings are the Cassini Division and the Encke Division, both visible from the Earth. The Cassini Division is the largest, measuring 4,800 km (2,983 mi) wide.[31] However, when the Voyager spacecrafts visited Saturn in 1980, they discovered that the rings are a complex structure, made out of thousands of thin gaps and ringlets. Scientists believe this is caused by the gravitational force of some of Saturn's moons. The tiny moon Pan orbits inside Saturn's rings, creating a gap within the rings. Other ringlets keep their structure due to the gravitational force of shepherd satellites, such as Prometheus and Pandora. Other gaps form due to the gravitational force of a large moon farther away. The moon Mimas is responsible for clearing away the Cassini gap.[31]
46
+
47
+ Recent data from the Cassini spacecraft has shown that the rings have their own atmosphere, free from the planet's atmosphere. The rings' atmosphere is made of oxygen gas, and it is produced when the Sun's ultraviolet light breaks up the water ice in the rings. Chemical reaction also occurs between the ultraviolet light and the water molecules, creating hydrogen gas. The oxygen and hydrogen atmospheres around the rings are very widely spaced.[32] As well as oxygen and hydrogen gas, the rings have a thin atmosphere made of hydroxide. This anion was discovered by the Hubble Space Telescope.[33]
48
+
49
+ The Voyager space probe discovered features shaped like rays, called spokes.[34] These were also seen later by the Hubble telescope. The Cassini probe photographed the spokes in 2005.[34] They are seen as dark when under sunlight, and appear light when against the unlit side. At first it was thought the spokes were made of microscopic dust particles but new evidence shows that they are made of ice.[35]
50
+ They rotate at the same time with the planet's magnetosphere, therefore, it is believed that they have a connection with electromagnetism. However, what causes the spokes to form is still unknown. They appear to be seasonal, disappearing during solstice and appearing again during equinox.[36]
51
+
52
+ Saturn has 53 named moons, and another nine which are still being studied.[37] Many of the moons are very small: 33 are less than 10 km (6 mi) in diameter and 13 moons are less than 50 km (31 mi).[38] Seven moons are large enough to be a near perfect sphere caused by their own gravitation. These moons are Titan, Rhea, Iapetus, Dione, Tethys, Enceladus and Mimas.[39] Titan is the largest moon, larger than the planet Mercury, and it is the only moon in the Solar System to have a thick, dense atmosphere.[40][41] Hyperion and Phoebe are the next largest moons, larger than 200 km (124 mi) in diameter.
53
+
54
+ In December 2004 and January 2005 a man-made satellite called the Cassini−Huygens probe took lots of close photos of Titan. One part of this satellite, known as the Huygens probe, then landed on Titan. Named after the Dutch astronomer Christiaan Huygens, it was the first spacecraft to land in the outer Solar System.[42] The probe was designed to float in case it landed in liquid.[42]
55
+ Enceladus, the sixth largest moon, is about 500 km (311 mi) in diameter. It is one of the few outer solar system objects that shows volcanic activity.[43] In 2011, scientists discovered an electric link between Saturn and Enceladus. This is caused by ionised particles from volcanos on the small moon interacting with Saturn's magnetic fields.[43] Similar interactions cause the northern lights on Earth.[44]
56
+
57
+ Saturn was first explored by the Pioneer 11 spacecraft in September 1979. It flew as close as 20,000 km (12,427 mi) above the planet's cloud tops. It took photographs of the planet and a few of its moons, but were low in resolution. It discovered a new, thin ring called the F ring. It also discovered that the dark ring gaps appear bright when viewed towards the Sun, which shows the gaps are not empty of material. The spacecraft measured the temperature of the moon Titan.[45]
58
+
59
+ In November 1980, Voyager 1 visited Saturn, and took higher resolution photographs of the planet, rings and moons. These photos were able to show the surface features of the moons. Voyager 1 went close to Titan, and gained much information about its atmosphere. In August, 1981, Voyager 2 continued to study the planet. Photos taken by the space probe showed that changes were happening to the rings and atmosphere. The Voyager spacecrafts discovered a number of moons orbiting close to Saturn's rings, as well as discovering new ring gaps.
60
+
61
+ On July 1, 2004, the Cassini−Huygens probe entered into orbit around Saturn. Before then, it flew close to Phoebe, taking very high resolution photos of its surface and collecting data. On December 25, 2004, the Huygens probe separated from the Cassini probe before moving down towards Titan's surface and landed there on January 14, 2005. It landed on a dry surface, but it found that large bodies of liquid exist on the moon. The Cassini probe continued to collect data from Titan and a number of the icy moons. It found evidence that the moon Enceladus had water erupting from its geysers.[46] Cassini also proved, in July 2006, that Titan had hydrocarbon lakes, located near its north pole. In March 2007, it discovered a large hydrocarbon lake the size of the Caspian Sea near its north pole.[47]
62
+
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+ Cassini observed lightning occurring in Saturn since early 2005. The power of the lightning was measured to be 1,000 times more powerful than lightning on Earth. Astronomers believe that the lightning observed in Saturn is the strongest ever seen.[48]
64
+
65
+ Notes
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+
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+ A gas giant is a large planet that has a solid core, but a very thick atmosphere. This means that most of the planet is made up of gas. These planets are very large.
2
+
3
+ In our outer Solar System, there are 4 gas giants: Jupiter, Saturn, Uranus, and Neptune.
4
+
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+ Jupiter and Saturn are similar because they are made up of mostly hydrogen and helium. They both contain massive rocky cores that are bigger than Earth. Neptune and Uranus are similar because they are mainly made up of water and rock (a mixture of one or several minerals).
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+ Gas giants have also been found around other stars than the sun. Most of those giant extrasolar planets are "hot giants" orbiting close to their star.
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1
+ Australia, formally the Commonwealth of Australia, is a country and sovereign state in the southern hemisphere, located in Oceania. Its capital city is Canberra, and its largest city is Sydney.
2
+
3
+ Australia is the sixth biggest country in the world by land area, and is part of the Oceanic and Australasian regions. Australia, New Zealand, New Guinea and other islands on the Australian tectonic plate are together called Australasia, which is one of the world's great ecozones. When other Pacific islands are included with Australasia, it is called Oceania.
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+
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+ 25 million[10] people live in Australia, and about 85% of them live near the east coast. [11] The country is divided up into six states and two territories, and more than half of Australia's population lives in and around the cities of Sydney, Melbourne, Brisbane, Perth and Adelaide.
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+ Australia is known for its mining (coal, iron, gold, diamonds and crystals), its production of wool, and as the world's largest producer of bauxite.[12] Its emblem is a flower called the Golden Wattle.
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+ Australia's landmass of 7,617,930 square kilometers is on the Indo-Australian plate.[13] The continent of Australia, including the island of Tasmania, was separated from the other continents of the world many millions of years ago. Because of this, many animals and plants live in Australia that do not live anywhere else. These include animals like the kangaroo, the koala, the emu, the kookaburra, and the platypus.
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+
11
+ People first arrived in Australia more than 50,000 years ago. These native Australians are called the Australian Aborigines. For the history of Australia, see History of Australia.
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+
13
+ Most of the Australian colonies, having been settled from Britain, became mostly independent democratic states in the 1850s and all six combined as a federation on 1 January 1901. The first Prime Minister of Australia was Edmund Barton in 1901. Australia is a member of the United Nations and the Commonwealth of Nations. It is a parliamentary democracy and a constitutional monarchy with Elizabeth II as Queen of Australia and Head of State and a Governor-General who is chosen by the Prime Minister to carry out all the duties of the Queen in Australia.
14
+
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+ Australia has six states, two major mainland territories, and other minor territories. The states are New South Wales, Queensland, South Australia, Tasmania, Victoria, and Western Australia.[14] The two major mainland territories are the Northern Territory and the Australian Capital Territory (ACT).
16
+
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+ In 2013 according to world bank Australia had just over 23.13 million people. Most Australians live in cities along the coast, such as Sydney, Melbourne, Brisbane, Perth, Darwin, Hobart and Adelaide. The largest inland city is Canberra, which is also the nation's capital. The largest city is Sydney.[15]
18
+
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+ Australia is a very big country, but much of the land is very dry, and the middle of the continent is mostly desert. Only the areas around the east, west and south coast have enough rain and a suitable climate (not too hot) for many farms and cities.
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+
21
+ The Australian Aboriginal people arrived in Australia about 50,000 years ago or even earlier.[16][17][18] Until the arrival of British settlers in 1788, the Aboriginal people lived by hunting and gathering food from the land. They lived in all sorts of climates and managed the land in different ways. An example of Aboriginal land management was the Cumberland Plain where Sydney is now. Every few years the Aboriginal people would burn the grass and small trees.[19] This meant that a lot of grass grew back, but not many big trees. Kangaroos like to live on grassy plains, but not in forests. The kangaroos that lived on the plain were a good food supply for the Aboriginal people. Sometimes, Aborigines would name a person after an animal, and they could not eat that animal to help level out the food population.
22
+
23
+ Aboriginal people did not usually build houses, except huts of grass, leaves and bark. They did not usually build walls or fences, and there were no horses, cows or sheep in Australia that needed to be kept in pens. The only Aboriginal buildings that are known are fish-traps made from stones piled up in the river, and the remains of a few stone huts in Victoria and Tasmania.[20][21][22] The Aboriginal people did not use metal or make pottery or use bows and arrows or weave cloth. In some parts of Australia the people used sharp flaked-stone spearheads, but most Aboriginal spears were made of sharply pointed wood. Australia has a lot of trees that have very hard wood that was good for spear making. The boomerang was used in some areas for sport and for hunting.
24
+
25
+ The Aboriginal people did not think that the land belonged to them. They believed that they had grown from the land, so it was like their mother, and they belonged to the land.
26
+
27
+ In the 1600s, Dutch merchants traded with the islands of Batavia (now Indonesia), to the north of Australia and several different Dutch ships touched on the coast of Australia. The Dutch governor, van Diemen, sent Abel Tasman on a voyage of discovery and he found Tasmania, which he named Van Diemen's Land. Its name was later changed to honour the man who discovered it.
28
+
29
+ The British Government was sure that there must be a very large land in the south, that had not been explored. They sent Captain James Cook to the Pacific Ocean. His ship, HMS Endeavour, carried the famous scientists, Sir Joseph Banks and Dr Solander who were going to Tahiti where they would watch the planet Venus pass in front of the Sun. Captain Cook's secret mission was to find "Terra Australis" (the Land of the South).
30
+
31
+ The voyage of discovery was very successful, because they found New Zealand and sailed right around it. Then they sailed westward. At last, a boy, William Hicks, who was up the mast spotted land on the horizon. Captain Cook named that bit of land Point Hicks. They sailed up the coast and Captain Cook named the land that he saw "New South Wales". At last they sailed into a large open bay which was full of fish and stingrays which the sailors speared for food. Joseph Banks and Dr. Solander went ashore and were astonished to find that they did not know what any of the plants or birds or animals that they saw were. They collected hundreds of plants to take back to England.
32
+
33
+ Captain Cook saw the Aboriginal people with their simple way of life. He saw them fishing and hunting and collecting grass seeds and fruit. But there were no houses and no fences. In most parts of the world, people put up a house and a fence or some marker to show that they own the land. But the Aboriginal people did not own the land in that way. They belonged to the land, like a baby belongs to its mother. Captain Cook went home to England and told the government that no-one owned the land. This would later cause a terrible problem for the Aboriginal people.
34
+
35
+ In the 1700s, in England, laws were tough, many people were poor and gaols (jails) were full. A person could be sentenced to death for stealing a loaf of bread. Many people were hung for small crimes. But usually they were just thrown in gaol. Often they were sent away to the British colonies in America. But by the 1770s, the colonies in America became the United States. They were free from British rule and would not take England's convicts any more, so England needed to find a new and less populated place.
36
+
37
+ By the 1780s the gaols of England were so full that convicts were often chained up in rotting old ships. The government decided to make a settlement in New South Wales and send some of the convicts there. In 1788 the First Fleet of eleven ships set sail from Portsmouth carrying convicts, sailors, marines, a few free settlers and enough food to last for two years. Their leader was Captain Arthur Phillip. They were to make a new colony at the place that Captain Cook had discovered, named Botany Bay because of all the unknown plants found there by the two scientists.
38
+
39
+ Captain Phillip found that Botany Bay was flat and windy. There was not much fresh water. He went with two ships up the coast and sailed into a great harbor which he said was "the finest harbor in the world!" There were many small bays on the harbor so he decided on one which had a good stream of fresh water and some flat shore to land on. On 26 January 1788, the flag was raised and New South Wales was claimed in the name of King George III of England, and the new settlement was called Sydney.
40
+
41
+ For the first few years of the settlement, things were very difficult. No-one in the British Government had thought very hard about what sort of convicts should be sent to make a new colony. Nobody had chosen them carefully. There was only one man who was a farmer. There was no-one among the convicts who was a builder, a brick-maker or a blacksmith. No-one knew how to fix the tools when they broke. All of the cattle escaped. There were no cooking pots. All the plants were different so no-one knew which ones could be eaten. It was probable that everyone in the new colony would die of starvation.
42
+
43
+ Somehow, the little group of tents with a hut for the Governor, Arthur Phillip, and another hut for the supply of food, grew into a small town with streets, a bridge over the stream, a windmill for grinding grain and wharves for ships. By the 1820s there was a fine brick house for the Governor. There was also a hospital and a convict barracks and a beautiful church which are still standing today. Settlements had spread out from Sydney, firstly to Norfolk Island and to Van Diemen's Land (Tasmania), and also up the coast to Newcastle, where coal was discovered, and inland where the missing cattle were found to have grown to a large herd. Spanish Merino sheep had been brought to Sydney, and by 1820, farmers were raising fat lambs for meat and also sending fine wool back to the factories of England.
44
+
45
+ While the settlement was growing in New South Wales, it was also growing in Tasmania. The climate in Tasmania was more like that in England, and farmers found it easy to grow crops there.
46
+
47
+ Because Australia is such a very large land, it was easy to think that it might be able to hold a very large number of people. In the early days of the colony, a great number of explorers went out, searching for good land to settle on.
48
+ When the settlers looked west from Sydney, they saw a range of mountains which they called the Blue Mountains. They were not very high and did not look very rugged but for many years no-one could find their way through them. In 1813 Gregory Blaxland, William Lawson and a 17-year-old called William Charles Wentworth crossed the Blue Mountains and found land on the other side which was good for farming. A road was built and the governor, Lachlan Macquarie founded the town of Bathurst on the other side, 100 miles from Sydney.
49
+
50
+ Some people, like Captain Charles Sturt were sure that there must be a sea in the middle of Australia and set out to find it. Many of the explorers did not prepare very well, or else they went out to explore at the hottest time of year. Some died like Burke and Wills. Ludwig Leichhardt got lost twice. The second time, he was never seen again. Major Thomas Mitchell was one of the most successful explorers. He mapped the country as he went, and his maps remained in use for more than 100 years. He travelled all the way to what is now western Victoria, and to his surprise and annoyance found that he was not the first white person there. The Henty brothers had come from Tasmania, had built themselves a house, had a successful farm and fed the Major and his men on roast lamb and wine.
51
+
52
+ The gold rushes of New South Wales and Victoria started in 1851 leading to large numbers of people arriving to search for gold. The population grew across south east Australia and made great wealth and industry. By 1853 the gold rushes had made some poor people, very rich.
53
+
54
+ The transportation of convicts to Australia ended in the 1840s and 1850s and more changes came. The people in Australia wanted to run their own country, and not be told what to do from London. The first governments in the colonies were run by governors chosen by London. Soon the settlers wanted local government and more democracy. William Wentworth started the Australian Patriotic Association (Australia's first political party) in 1835 to demand democratic government. In 1840, the city councils started and some people could vote. New South Wales Legislative Council had its first elections in 1843, again with some limits on who could vote. In 1855, limited self-government was given by London to New South Wales, Victoria, South Australia and Tasmania. In 1855, the right to vote was given to all men over 21 in South Australia. The other colonies soon followed. Women were given the vote in the Parliament of South Australia in 1895 and they became the first women in the world allowed to stand in elections.[23][24]
55
+
56
+ Australians had started parliamentary democracies all across the continent. But voices were getting louder for all of them to come together as one country with a national parliament.
57
+
58
+ Until 1901, Australia was not a nation, it was six separate colonies governed by Britain. They voted to join together to form one new country, called the Commonwealth of Australia, in 1901. Australia was still part of the British Empire, and at first wanted only British or Europeans to come to Australia. But soon it had its own money, and its own Army and Navy.
59
+
60
+ In Australia at this time, the trade unions were very strong, and they started a political party, the Australian Labor Party. Australia passed many laws to help the workers.[26]
61
+
62
+ In 1914, the First World War started in Europe. Australia joined in on the side of Britain against Germany, Austria-Hungary and the Ottoman Empire. Australian soldiers were sent to Gallipoli, in the Ottoman Empire. They fought bravely, but were beaten by the Turks. Today Australia remembers this battle every year on ANZAC Day. They also fought on the Western Front. More than 60,000 Australians were killed.
63
+
64
+ Australia had a really hard time in the Great Depression of the 1930s and joined Britain in a war against Nazi Germany when Hitler invaded Poland in 1939. But in 1941 lots of Australian soldiers were captured in the Fall of Singapore by Japan. Then Japan started attacking Australia and people worried about invasion. But with help from the United States Navy, the Japanese were stopped. After the war, Australia became a close friend of the United States.
65
+
66
+ When the war ended, Australia felt that it needed many more people to fill the country up and to work. So the government said it would take in people from Europe who had lost their homes in the war. It did things like building the Snowy Mountains Scheme. Over the next 25 years, millions of people came to Australia. They came especially from Italy and Greece, other countries in Europe. Later they also came from countries like Turkey and Lebanon. An important new party, the Liberal Party of Australia was made by Robert Menzies in 1944 and it won lots of elections from 1949 until in 1972, then Gough Whitlam won for the Labor Party. Whitlam made changes, but he made the Senate unhappy and the Governor-General sacked him and forced an election in 1975. Then Malcolm Fraser won a few elections for the Liberal Party.
67
+
68
+ In the 1960s many people began coming to Australia from China, Vietnam, Malaysia and other countries in Asia. Australia became more multicultural. In the 1950s and 1960s Australia became one of the richest countries in the world, helped by mining and wool. Australia started trading more with America, than Japan. Australia supported the United States in wars against dictatorships in Korea and Vietnam and later Iraq. Australian soldiers also helped the United Nations in countries like East Timor in 1999.
69
+
70
+ In 1973, the famous Sydney Opera House opened. In the 1970s, 80s and 90s lots of Australian movies, actors and singers became famous around the world. In the year 2000, Sydney had the Summer Olympics.
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+
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+ In the 1980s and 90s, the Labor Party under Bob Hawke and Paul Keating, then the Liberal Party under John Howard made lots of changes to the economy. Australia had a bad recession in 1991, but when other Western countries had trouble with their economies in 2008, Australia stayed strong.
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+
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+ Today Australia is a rich, peaceful and democratic country. But it still has problems. Around 4-5% of Australians could not get a job in 2010. A lot of land in Australia (like Uluru) has been returned to Aboriginal people, but lots of Aborigines are still poorer than everybody else. Every year the government chooses a big number of new people from all around the world to come as immigrants to live in Australia. These people may come because they want to do business, or to live in a democracy, to join their family, or because they are refugees. Australia took 6.5 million immigrants in the 60 years after World War Two, including around 660,000 refugees.[27]
75
+
76
+ Julia Gillard became the first woman Prime Minister of Australia in 2010 when she replaced her colleague Kevin Rudd of the Labor Party.
77
+
78
+ Australia is made up of six states, and two mainland territories. Each state and territory has its own Parliament and makes its own local laws. The Parliament of Australia sits in Canberra and makes laws for the whole country, also known as the Commonwealth or Federation.
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+
80
+ The Federal government is led by the Prime Minister of Australia, who is the member of Parliament chosen as leader. The current Prime Minister is Scott Morrison.
81
+
82
+ The leader of Australia is the Prime Minister, although the Governor-General represents the Queen of Australia, who is also the Queen of Great Britain, as head of state. The Governor-General, currently His Excellency David Hurley, is chosen by the Prime Minister.
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+
84
+ Australia was colonised by people from Britain,[28] but today people from all over the world live there. English is the main spoken language, and Christianity is the main religion, though all religions are accepted and not everybody has a religion. Australia is multicultural, which means that all its people are encouraged to keep their different languages, religions and ways of life, while also learning English and joining in with other Australians.
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+
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+ Famous Australian writers include the bush balladeers Banjo Paterson and Henry Lawson who wrote about life in the Australian bush. More modern famous writers include Peter Carey, Thomas Keneally and Colleen McCullough. In 1973, Patrick White won the Nobel Prize in Literature, the only Australian to have achieved this; he is seen as one of the great English-language writers of the twentieth century.
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+ Australian music has had lots of world-wide stars, for example the opera singers Nellie Melba and Joan Sutherland, the rock and roll bands Bee Gees, AC/DC and INXS, the folk-rocker Paul Kelly (musician), the pop singer Kylie Minogue and Australian country music stars Slim Dusty and John Williamson. Australian Aboriginal music is very special and very ancient: it has the famous digeridoo woodwind instrument.
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+ Australian TV has produced many successful programs for home and overseas - including Skippy the Bush Kangaroo, Home and Away and Neighbours - and produced such well known TV stars as Barry Humphries (Dame Edna Everage), Steve Irwin (The Crocodile Hunter) and The Wiggles. Major Australian subgroups such as the Bogan have been shown on Australian TV in shows such as Bogan Hunters and Kath & Kim.[29]
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+ Australia has two public broadcasters (the ABC and the multi-cultural SBS), three commercial television networks, three pay-TV services, and numerous public, non-profit television and radio stations. Each major city has its daily newspapers, and there are two national daily newspapers, The Australian and The Australian Financial Review.
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+ Australian movies have a very long history. The world's first feature movie was the Australian movie The Story of the Kelly Gang of 1906.[30] In 1933, In the Wake of the Bounty, directed by Charles Chauvel, had Errol Flynn as the main actor.[31] Flynn went on to a celebrated career in Hollywood. The first Australian Oscar was won by 1942's Kokoda Front Line!, directed by Ken G. Hall.[32] In the 1970s and 1980s lots of big Australian movies and movie stars became world famous with movies like Picnic at Hanging Rock, Gallipoli (with Mel Gibson), The Man From Snowy River and Crocodile Dundee.[33] Russell Crowe, Cate Blanchett and Heath Ledger became global stars during the 1990s and Australia starring Nicole Kidman and Hugh Jackman made a lot of money in 2008.
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+ Australia is also a popular destination for business conferences and research, with Sydney named as one of the top 20 meeting destinations in the world.[34]
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+ Sport is an important part of Australian culture because the climate is good for outdoor activities. 23.5% Australians over the age of 15 regularly take part in organised sporting activities.[35] In international sports, Australia has very strong teams in cricket, hockey, netball, rugby league and rugby union, and performs well in cycling, rowing and swimming. Local popular sports include Australian Rules Football, horse racing, soccer and motor racing. Australia has participated in every summer Olympic Games since 1896, and every Commonwealth Games. Australia has hosted the 1956 and 2000 Summer Olympics, and has ranked in the top five medal-winners since 2000. Australia has also hosted the 1938, 1962, 1982 and 2006 Commonwealth Games and are to host the 2018 Commonwealth Games. Other major international events held regularly in Australia include the Australian Open, one of the four Grand Slam tennis tournaments, annual international cricket matches and the Formula One Australian Grand Prix. Corporate and government sponsorship of many sports and elite athletes is common in Australia. Televised sport is popular; some of the highest-rated television programs include the Summer Olympic Games and the grand finals of local and international football competitions.
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+ The main sporting leagues for males are the Australian Football League, National Rugby League, A-League and NBL.
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+ For women, they are ANZ Netball Championships, W-League and WNBL.
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+ Famous Australian sports players include the cricketer Sir Donald Bradman, the swimmer Ian Thorpe and the athlete Cathy Freeman.
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+ Just 60 years ago, Australia had only one big art festival. Now Australia has hundreds of smaller community-based festivals, and national and regional festivals that focus on specific art forms.[36]
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+ Australia is home to many animals that can be found nowhere else on Earth, which include: the Koalas,the Kangaroos, the Wombat, the Numbat, the Emu, among many others. Most of the marsupials in the world are found only on the continent.
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+ Africa
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+ Antarctica
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+ Asia
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+ Australia
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+
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+ Europe
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+ North America
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+ South America
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+ Afro-Eurasia
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+ Americas
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+ Eurasia
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+ Oceania
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+ Wikipedia does not yet have an article with this name.
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+ Wikipedia does not yet have an article with this name.
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+ Dwarf planet is the name used to classify some objects in the solar system. This definition was made on August 24, 2006 by the International Astronomical Union (IAU), and can be described as; a dwarf planet is a body orbiting the Sun that is big enough to round itself by its own gravity, but has not cleared its orbital path of other rival bodies. At the same meeting the IAU also defined the term planet for the first time. Some astronomers think that the term "dwarf planet" is too confusing and needs to be changed.
2
+
3
+ The seven dwarf planets, in order from their distance from the Sun are:
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+
5
+ The dwarf planets, unlike the terrestrial and gas giant planets, are in more than one region of the solar system. Ceres is in the asteroid belt. The high orbital eccentricity of Pluto puts it mostly outside Neptune's orbit, but partly inside. The others are in the trans-Neptune region.
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+
7
+ NASA's Dawn and New Horizons missions reached Ceres and Pluto, respectively, in 2015. Dawn had already orbited and observed Vesta in 2011.
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+ There are many other dwarf planets in the solar system. Most of them are also Kuiper belt objects.
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+ Earth is the planet we live on. It is the third planet from the Sun. It is the only planet known to have life on it. The Earth formed around 4.5 billion years ago.[28][29] It is one of four rocky planets on the inside of the Solar System. The other three are Mercury, Venus, and Mars.
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+ The large mass of the Sun makes Earth move around it, just as the mass of Earth makes the moon move around it. Earth also turns around in space, so that different parts face the Sun at different times. Earth goes around the Sun once (one year) for every 365​1⁄4 times it turns around (one day).
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+ Earth is the only planet in our solar system that has a large amount of liquid water.[30] About 74% of the surface of Earth is covered by liquid or frozen water. Because of this, people sometimes call it the blue planet.[31]
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+ Because of its water, Earth is home to millions of species of plants and animals.[32][33] The things that live on Earth have changed its surface greatly. For example, early cyanobacteria changed the air and gave it oxygen. The living part of Earth's surface is called the "biosphere".[34]
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+ Earth is part of the eight planets and many thousands of small bodies that move around the Sun as its solar system. The Solar System is moving through the Orion Arm of the Milky Way galaxy now, and will be for about the next 10,000 years.[35][36]
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+ Earth is about 150,000,000 kilometres or 93,000,000 miles away from the Sun (this distance is called an "Astronomical Unit"). It moves on its orbit at an average speed of about 30 km/s (19 mi/s).[37] Earth turns all the way around about 365​1⁄4 times in the time it takes for Earth to go all the way around the Sun.[4] To make up this extra bit of a day every year, an additional day is used every four years. This is named a "leap year".
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+ The Moon goes around Earth at an average distance of 400,000 kilometres or 250,000 miles. It is locked to Earth, so that it always has the same half facing Earth; the other half is called the "dark side of the moon". It takes about 27​1⁄3 days for the Moon to go all the way around Earth, but because Earth is moving around the Sun at the same time, it takes about 29​1⁄2 days for the Moon to go from dark to bright to dark again. This is where the word "month" came from, even though most months now have 30 or 31 days.
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+ Earth and the other planets formed about 4.6 billion years ago.[38] They were made of the leftover gas from the nebula that made the Sun. The Moon may have been formed after a collision between the early Earth and a smaller planet (sometimes called Theia). Scientists believe that parts of both planets broke off — becoming (by gravity) the Moon.[39]
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+ Earth's water came from different places. Condensing water vapour, and comets and asteroids hitting Earth, made the oceans. Within a billion years (that is at about 3.6 billion years ago) the first life evolved, in the Archaean era.[40] Some bacteria developed photosynthesis, which lets plants make food from the Sun's light and water. This released a lot of oxygen, which was first taken up by iron in solution. Eventually, free oxygen got into the atmosphere or air, making Earth's surface suitable for aerobic life (see Great Oxygenation Event). This oxygen also formed the ozone layer which protects Earth's surface from bad ultraviolet radiation from the Sun. Complex life on the surface of the land did not exist before the ozone layer.
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+ Earth's land and climate has been very different in the past. About 3 to 3.5 million years ago almost all land was in one place. This is called a supercontinent. The earliest known supercontinent was called Vaalbara. Much later, there was a time (the Cryogenian) when Earth was almost entirely covered by thick ice sheets (glaciers).[41] This is discussed as the Snowball Earth theory.[41]
22
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+ Earth is rocky. It is the largest of the rocky planets moving around the Sun by mass and by size. It is much smaller than the gas giants such as Jupiter.
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+ Overall, Earth is made of iron (32.1%), oxygen (30.1%), silicon (15.1%), magnesium (13.9%), sulfur (2.9%), nickel (1.8%), calcium (1.5%), and aluminium (1.4%). The 1.2% left over is made of many different kinds of other chemicals. Chemicals that are very uncommon (such as gold and platinum) can be very valuable.
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+ The structure of Earth changes from the inside to the outside. The center of earth (Earth's core) is mostly iron (88.8%), nickel (5.8%), sulfur (4.5%), and less than 1% other things.[42] The Earth's crust is largely oxygen (47%). Oxygen is normally a gas but it can join with other chemicals to make compounds like water and rocks. 99.22% of rocks have oxygen in them. The most common oxygen-having rocks are silica (made with silicon), alumina (made with aluminium), rust (made with iron), lime (made with calcium), magnesia (made with magnesium), potash (made with potassium), and sodium oxide, and there are others as well.[43]
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+ Earth's shape is a spheroid: not quite a sphere because it is slightly squashed on the top and bottom. The shape is called an oblate spheroid. As Earth spins around itself, centrifugal force forces the equator out a little and pulls the poles in a little. The equator, around the middle of Earth's surface, is about 40,075 kilometers or 24,900 miles long.[44]
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+ The highest mountain above sea level—the well-known Mount Everest (which is 8,848 metres or 29,029 feet above sea level)—is not actually the one that is the farthest away from the center of the Earth. Instead, the sleeping volcano Mount Chimborazo in Ecuador is; it is only 6,263 metres or 20,548 feet above sea level but it is almost at the equator. Because of this, Mount Chimborazo is 6,384 kilometres or 3,967 miles from the center of the Earth, while Mount Everest is 2 kilometres or 1.2 miles closer to it.[45][46][47] Similarly, the lowest point below sea level that we are conscious of is the Challenger Deep in the Mariana Trench in the Pacific Ocean. It is about 10,971 metres or 35,994 feet below sea level,[48] but, again, there are probably places at the bottom of the Arctic Ocean that are nearer to the center of the Earth.
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+ The deepest hole ever dug is only about 12.3 kilometers or 7.6 miles. We know something about the inside of the Earth, though, because we can learn things from earthquakes and the times when volcanoes erupt. We are able to see how quickly the shock waves move through Earth in different places.
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+ The inside of Earth is very different from the outside. Almost all of Earth's liquid water is in the seas or close to the surface. The surface also has a lot of oxygen, which comes from plants. Small and simple kinds of life can live far under the surface, but animals and plants only live on the surface or in the seas. The rocks on the surface of Earth (Earth's crust) are well known. They are thicker where there is land, between 30 to 50 km or 19 to 31 mi thick. Under the seas they are sometimes only 6 km or 3.7 mi thick.[49] There are three groups of rocks that make up most of the Earth's crust. Some rock is made when the hot liquid rock comes from inside the earth (igneous rocks); another type of rock is made when sediment is laid down, usually under the sea (sedimentary rocks); and a third kind of rock is made when the other two are changed by very high temperature or pressure (metamorphic rocks). A very few rocks also fall out of the sky (meteorites).
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+ Below the crust is warm and almost-liquid rock that is always moving around (the Earth's mantle). Then, there is a thin liquid layer of heated rock (the outer core). This is very hot: 7,000 °C or 13,000 °F or 7,300 K.[50] The middle of the inside of the Earth would be liquid as well but all the weight of the rock above it pushes it back into being solid. This solid middle part (the inner core) is almost all iron. This is what makes the Earth magnetic.
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+ The Earth's crust is solid but made of parts which move very slowly.[51] The thin level of hard rock on the outside of the Earth rests on hot liquid material below it in the deeper mantle.[52] This liquid material moves because it gets heat from the hot center of the earth. The slow movement of the plates is what causes earthquakes, volcanoes and large groups of mountains on the Earth.
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+ There are three ways plates can come together. Two plates can move towards each other ("convergent" plate edges). This can form islands (such as Japan), volcanoes, and high mountain ranges (such as the Andes and Himalayas).[53] Two plates can move away from each other ("divergent" plate edges). This gives the warm liquid rock inside the earth a place to come out. This makes special mountain ranges below the sea or large low lands like Africa's Great Rift Valley.[54][55] Plates are able to move beside each other as well ("transform" plate edges, such as the San Andreas Fault). This makes their edges crush against each other and makes many shocks as they move.[56]
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+ The outside of the Earth is not even. There are high places called mountains, and high flat places called plateaus. There are low places called valleys and canyons. For the most part, moving air and water from the sky and seas damages rocks in high places and breaks them into small pieces. The air and water then move these pieces to lower places. Because of this, the Earth would have been very flat a long time before now. The fundamental cause of the differences in the Earth's surface is plate tectonics. The shape of the entire planet itself is not even a ball. Because of its velocity, Earth has a slight bulge at the Equator. Other than that, Earth is shaped more like a pear than an actual sphere.
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+ All places on Earth are made of, or are on top of, rocks. The outside of the Earth is usually not uncovered rock. Over 70% of the Earth is covered by seas full of salty water.[57] This salty water makes up about 97​1⁄2% of all Earth's water. The fresh water people can drink is mostly ice. Only a very small amount is in rivers and under the Earth for people to drink and use.[58] The air above the Earth stops the water from going away into outer space. Also, much of the land on Earth is covered with plants, or with what is left from earlier living things. Places with very little rain are dry wastes called deserts. Deserts usually have few living things, but life is able to grow very quickly when these wastes have rainfall. Places with large amounts of rain may be large woods. Lately, people have changed the environment of the Earth a great deal.
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+ All around the Earth is a large amount of air (the atmosphere). The mass of the Earth pulls the gasses in the air down and does not let them go into outer space. The air is mostly made of nitrogen (about 78%) and oxygen (about 21%) but there are a few other gasses as well.[59] Most living things need the air (or parts of the air gripped in the water) to breathe and live. They use the gasses—especially oxygen and carbon dioxide—to make and use sugar and to give themselves power.
48
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49
+ The air animals and plants use to live is only the first level of the air around the Earth (the troposphere). The day to day changes in this level of air are named weather; the changes between places far away from each other and from year to year are named the climate. Rain and storms are both in this level. Both come about because this part of the air gets colder as it goes up. Cold air becomes thicker and falls, and warm air becomes thinner and goes up.[60] The turning Earth moves the air as well and air moves north and south because the middle of the Earth generally gets more power from the Sun and is warmer than the north and south points. At the same time, air over water (specially very warm water) gets water in it but, because cold air is not able to take in as much water, it starts to make clouds and rain as it gets colder. The way water moves around in a circle like this is called the water cycle.[60]
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51
+ Above this first level, there are four other levels. The air gets colder as it goes up in the first level; in the second level (the stratosphere), the air gets warmer as it goes up. This level has a special kind of oxygen called ozone. The ozone in this air keeps living things safe from damaging rays from the Sun. The power from these rays is what makes this level warmer and warmer. The middle level (the mesosphere) gets colder and colder with height; the fourth level (the thermosphere) gets warmer and warmer; and the last level (the exosphere) is almost outer space and has very little air at all. It reaches about half the way to the Moon. The three outer levels have a lot of electric power moving through them; this is called the ionosphere and is important for radio and other electric waves in the air. It is also where the Northern Lights are.
52
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53
+ Even though air seems very light, the weight of all of the air above the outside of the Earth (air pressure) is important. Generally, from sea level to the top of the outer level of the air, a space of air one cm2 across has a mass of about 1.03 kg and a space of air one sq in across has a weight of about 14.7 lb. The mass of the air also keeps the Earth safe when rocks (meteorites) hit it from outer space. Without the air, the damage meteorites do would be much greater. Because of the air, meteorites generally burn up long before they get to the earth.
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+ The air also keeps the Earth warm, specially the half turned away from the Sun. Some gasses – especially methane and carbon dioxide – work like a blanket to keep things warm.[61] In the past, the Earth has been much warmer and much colder than it is now. Since people have grown used to the heat we have now, though, we do not want the Earth to be too much warmer or colder. Most of the ways people create electric power use burning kinds of carbon—especially coal, oil, and natural gas. Burning these creates new carbon dioxide and can cause more warming. A large discussion is going on now about what people should do about the Earth's latest warming, which has gone on for about 150 years. So far, this warming has been good for people: plants have grown better and the weather has been better than when it was colder before. Some people who learn about science, though, say that many bad things will possibly come about if the warming goes on.
56
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57
+ About seven billion people live on Earth. They live in about 200 different lands called countries. Some, for example, Russia, are large with many large cities. Others, for example, Vatican City, are small. The five countries with the most people are China, India, the United States, Indonesia, and Brazil. About 90% of people live in the north half of the world, which has most of the land. Scientists think that people originally came from Africa. Now, 70% of all people do not live in Africa but in Europe and Asia.[62]
58
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+ People change the Earth in many ways. They have been able to grow plants for food and clothes for about ten thousand years. When there was enough food, they were able to build towns and cities. Near these places, men and women were able to change rivers, bring water to farms, and stop floods (rising water) from coming over their land. People found useful animals and bred them so they were easier to keep.
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1
+ Uranus is the seventh planet from the Sun in the Solar System. It is a gas giant. It is the third largest planet in the solar system.
2
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3
+ The planet is made of ice, gases and liquid metal. Its atmosphere contains hydrogen (1H), helium (2He) and methane. The temperature on Uranus is −197 °C (−322.6 °F; 76.1 K) near the top of its atmosphere, but its small solid core (about 55% the mass of Earth) is probably about 4,730 °C (8,540 °F; 5,000 K).
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+ The planet is tilted on its axis so much that it is sideways.[1] It has five big moons, many small ones, and a small system of 13 planetary rings.
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+ The distance between Uranus and the Sun is about 2.8 billion km. Uranus completes its orbit around the Sun in 84 earth years. It completes a spin around itself in 17 hours and 14 minutes. This means there are about 43,000 Uranian days in one Uranian year.[2]
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+ Uranus was discovered in 1781.[3] This planet can be seen with the naked eye under perfect conditions. John Flamsteed saw it decades earlier but mistook it for a star (34 Tauri).
10
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11
+ Uranus is named after the Greek god Uranus, who was a god of sky.
12
+
13
+ Uranus has 27 known moons. They are named for characters from the works of Shakespeare and Alexander Pope.[4][5] The five biggest moons are Miranda, Ariel, Umbriel, Titania and Oberon. Many moons have yet to be discovered.
14
+
15
+ In 1986, NASA's Voyager 2 visited Uranus. This is the only space probe that tried to investigate the planet from a short distance.
16
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17
+ Uranus is covered in blue clouds. The top clouds, made of methane, are difficult to see.[6] Lower clouds are thought to be frozen water. There are also violent storms. Wind speeds can reach 250 metres per second (900 km/h; 560 mph). Scientists are studying the clouds to try to understand the storms on the planet.[7]
18
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19
+ The planet Uranus has a system made of 13 rings which is far fewer than the rings of Saturn but more than those around Jupiter and Neptune. The rings of Uranus were discovered in 1977.[8] More than 200 years ago, William Herschel also reported observing rings, but modern astronomers do not believe that he saw them, because they are very dark and faint. Two additional rings were discovered in 1986 in images taken by Voyager 2,[9] and two outer rings were found in 2003–2005 by the Hubble Space Telescope.[10] The rings are probably mainly composed of frozen water.
20
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21
+ The rings of Uranus are thought to be relatively young, not more than 600 million years old. The Uranian ring system probably began from the collisional fragmentation of moons that once existed around the planet. After colliding, the moons probably broke up into many particles, which survived as narrow, optically dense rings only in zones of maximum stability.
22
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23
+ The ring system of Uranus has thirteen distinct rings. In order of increasing distance from the planet they are: 1986U2R/ζ, 6, 5, 4, α, β, η, γ, δ, λ, ε, ν, μ rings. They can be divided into three groups: nine narrow main rings (6, 5, 4, α, β, η, γ, δ, ε), two dusty rings (1986U2R/ζ, λ) and two outer rings (μ, ν). The rings of Uranus consist mainly of macroscopic particles and little dust, although dust is known to be present in 1986U2R/ζ, η, δ, λ, ν and μ rings.
24
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25
+ In addition to these well-known rings, there may be numerous optically thin dust bands and faint rings between them. These faint rings and dust bands may exist only temporarily. Some of them became visible during a series of ring plane-crossing events in 2007.[11] A number of dust bands between the rings were observed in forward-scattering [a] geometry by Voyager 2. All rings of Uranus show azimuthal brightness variations.
26
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27
+ The rings are made of an extremely dark material. The rings are slightly red in the ultraviolet and visible parts of the spectrum and grey in near-infrared.[12] They show no identifiable spectral features. The chemical composition of the ring particles is not known. However, they cannot be made of pure water ice like the rings of Saturn because they are too dark, darker than the inner moons of Uranus. This shows that they are probably a mixture of the ice and a dark material. The nature of this material is not clear, but it may be organic compounds considerably darkened by the charged particle irradiation from the Uranian magnetosphere. The rings' particles may consist of a heavily processed material which was initially similar to that of the inner moons.[12]
28
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29
+ As a whole, the ring system of Uranus is unlike either the faint dusty rings of Jupiter or the broad and complex rings of Saturn, some of which are composed of very bright material—water ice. However, there are similarities with some parts of the latter ring system; the Saturnian F ring and the ε ring are both narrow, relatively dark and are shepherded by a pair of moons. The newly discovered outer rings of Uranus are similar to the outer G and E rings of Saturn. Narrow ringlets existing in the broad Saturnian rings also resemble the narrow rings of Uranus. In addition, dust bands observed between the main rings of Uranus may be similar to the rings of Jupiter. In contrast, the Neptunian ring system is quite similar to that of Uranus, although it is less complex, darker and contains more dust. The Neptunian rings are also positioned further from the planet.
30
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31
+ Uranus revolves around the Sun once every 84 Earth years. Its average distance from the Sun is roughly 3 billion km (about 20 AU). The intensity of sunlight on Uranus is about 1/400 that on Earth.[13] Its orbital elements were first calculated in 1783 by Pierre-Simon Laplace.[14] With time, discrepancies began to appear between the predicted and observed orbits, and in 1841, John Couch Adams first proposed that the differences might be due to the gravitational tug of an unseen planet. In 1845, Urbain Le Verrier began his own independent research into Uranus's orbit. On September 23, 1846, Johann Gottfried Galle found a new planet, later called Neptune, at nearly the position predicted by Le Verrier.[15]
32
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33
+ The rotational period of the interior of Uranus is 17 hours, 14 minutes, clockwise (retrograde). As on all giant planets, its upper atmosphere experiences very strong winds in the direction of rotation. At some latitudes, such as about two-thirds of the way from the equator to the south pole, visible features of the atmosphere move much faster, making a full rotation in as little as 14 hours.[16]
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+ Notes
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1
+ Venus is the second planet from the sun.[3] It has a day longer than a year. The year length of Venus is 225 Earth days. The day length of Venus is 243 Earth days. It is a terrestrial planet because it has a solid, rocky surface like other planets in the inner solar system. Astronomers have known Venus for thousands of years. The ancient Romans named it after their goddess Venus. Venus is the brightest thing in the night sky except for the Moon. It is sometimes called the morning star or the evening star as at some elongations it is easily seen just before the sun comes up in the morning and, at other times, just after the sun goes down in the evening. Venus comes closer to the Earth than any other planet does.
2
+
3
+ Venus is sometimes called the sister planet of Earth as they are quite similar in size and gravity. In other ways the planets are very different. Venus' atmosphere (air) is mostly carbon dioxide with clouds of sulphuric acid.[4] Sulphuric acid is a chemical that is very poisonous to humans.
4
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5
+ The thick atmosphere has made it hard to see the surface, and until the twenty-first century many people thought things might live there. The pressure on Venus' surface is 92 times that of Earth. Venus has no moons. Venus spins very slowly on its axis and it spins in the opposite direction to the other planets.
6
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7
+ Venus is a terrestrial planet so, like the Earth, its surface is made of rock. Venus is much hotter than Earth. All the carbon dioxide in the atmosphere acts like a blanket, trapping heat from the Sun. This effect is called the greenhouse effect and it is very strong on Venus. This makes the surface of Venus the hottest of any planet's surface in the Solar System with an estimated average temperature of 1522 degrees farenheit.[5][6] This is hot enough to melt lead or zinc.
8
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+ Venus has no oceans because it is much too hot for water. Venus' surface is a dry desert. Because of the clouds, only radar can map the surface. It is about 80% smooth, rocky plains, made mostly of basalt. Two higher areas called continents make up the north and south of the planet. The north is called Ishtar Terra and the south is called Aphrodite Terra. They are named after the Babylonian and Greek goddesses of love.[7]
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+ Venus' atmosphere is mostly carbon dioxide and nitrogen gas with clouds of sulphuric acid. Because the atmosphere is so thick or dense the pressure is very high. The pressure is 92 times the pressure on Earth, enough to crush many things.
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+ It is impossible to see the planet's surface from space as the thick cloud layer reflects 60% of the light that hits it. The only way scientists are able to see it is by using infrared and ultraviolet cameras and radar.
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+ Venus can sometimes be seen passing between the Sun and Earth. Venus looks like a black dot when seen through a special telescope. These passages are called "transits". These "transits" happen in pairs eight years apart. Then it is more than a hundred years to the next pair.
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+ Venus is the second planet from the sun.[3] It has a day longer than a year. The year length of Venus is 225 Earth days. The day length of Venus is 243 Earth days. It is a terrestrial planet because it has a solid, rocky surface like other planets in the inner solar system. Astronomers have known Venus for thousands of years. The ancient Romans named it after their goddess Venus. Venus is the brightest thing in the night sky except for the Moon. It is sometimes called the morning star or the evening star as at some elongations it is easily seen just before the sun comes up in the morning and, at other times, just after the sun goes down in the evening. Venus comes closer to the Earth than any other planet does.
2
+
3
+ Venus is sometimes called the sister planet of Earth as they are quite similar in size and gravity. In other ways the planets are very different. Venus' atmosphere (air) is mostly carbon dioxide with clouds of sulphuric acid.[4] Sulphuric acid is a chemical that is very poisonous to humans.
4
+
5
+ The thick atmosphere has made it hard to see the surface, and until the twenty-first century many people thought things might live there. The pressure on Venus' surface is 92 times that of Earth. Venus has no moons. Venus spins very slowly on its axis and it spins in the opposite direction to the other planets.
6
+
7
+ Venus is a terrestrial planet so, like the Earth, its surface is made of rock. Venus is much hotter than Earth. All the carbon dioxide in the atmosphere acts like a blanket, trapping heat from the Sun. This effect is called the greenhouse effect and it is very strong on Venus. This makes the surface of Venus the hottest of any planet's surface in the Solar System with an estimated average temperature of 1522 degrees farenheit.[5][6] This is hot enough to melt lead or zinc.
8
+
9
+ Venus has no oceans because it is much too hot for water. Venus' surface is a dry desert. Because of the clouds, only radar can map the surface. It is about 80% smooth, rocky plains, made mostly of basalt. Two higher areas called continents make up the north and south of the planet. The north is called Ishtar Terra and the south is called Aphrodite Terra. They are named after the Babylonian and Greek goddesses of love.[7]
10
+
11
+ Venus' atmosphere is mostly carbon dioxide and nitrogen gas with clouds of sulphuric acid. Because the atmosphere is so thick or dense the pressure is very high. The pressure is 92 times the pressure on Earth, enough to crush many things.
12
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13
+ It is impossible to see the planet's surface from space as the thick cloud layer reflects 60% of the light that hits it. The only way scientists are able to see it is by using infrared and ultraviolet cameras and radar.
14
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15
+ Venus can sometimes be seen passing between the Sun and Earth. Venus looks like a black dot when seen through a special telescope. These passages are called "transits". These "transits" happen in pairs eight years apart. Then it is more than a hundred years to the next pair.
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1
+ Wikipedia does not yet have an article with this name.
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1
+ Carnivorous plants are plants which get nutrients from trapping and eating animals. They are often called insectivorous plants, because they usually trap insects. Since they get some of their food from animals, carnivorous plants can grow in places where the soil is thin, or poor in nutrients. This is true for soils with little nitrogen, such as acidic bogs and rock outcrops. Charles Darwin wrote the first well-known book on carnivorous plants in 1875.[1]
2
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+ This ability of plants to catch animals is true carnivory. There are more than twelve genera in five families. These include about 625 species that attract and trap prey, produce digestive enzymes, and use their nutrients. In addition, there are more than 300 species in several genera that show some but not all of these characteristics. These are usually called protocarnivorous plants.
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+
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+ Insectivorous plants have leaves that are made like pitchers or bladders which catch insects. Today, five different ways of trapping are known
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+ These traps are all classified as active or passive. Triphyophyllum is a liana (a climber in tropical forests). It has three types of leaves. When needed, it puts out long leaves. These are passive 'flypapers' which hide mucus. The leaves of the plant do not grow or move as a response to moving prey. The Sundew Drosera, on the other hand, is an active flypaper. All species of Sundew are able to move their sticky tentacles in response to a contact. The tentacles are very sensitive and will bend toward the center of the leaf in order to bring the insect into contact with as many stalked glands as possible. According to Darwin, the touch of legs of a small gnat with a single tentacle is enough to cause this response.[1] This helps the catch and digestion of prey.
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+ The Venus flytrap, Dionaea muscipula, is one of a very small group of plants able to move fast. When an insect or spider crawls along the leaves and touches a hair, the trap closes only if a different hair is contacted within twenty seconds of the first touch. The two-touch trigger avoids wasting energy on objects with no food value.
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+ A carnivorous plant must attract, kill and digest prey.[2][3] It must then also benefit from digesting the prey. In most cases, this will yield amino acids and ammonium ions. There are some cases, where plants catch the prey, but they do not digest it. Rather, they have a symbiosis with another organism, which feeds on the prey. One such case is the species of the sundew Roridula, which forms a symbiosis with the assassin bug. The bugs eat the trapped insects. The plant benefits from the nutrients in the bugs' faeces.[4]
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+ Few fossil carnivorous plants have been found, and then usually as seed or pollen. Carnivorous plants are generally herbs, without wood or bark. True carnivoury has probably evolved independently at least six times.[2]
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+
15
+ Some think all trap types have a similar basic structure—the hairy leaf.[5] Hairy leaves do catch and hold drops of rainwater, which helps bacterial growth. Insects land on the leaf, are caught by the surface tension of the water, and suffocate. Bacteria start to decay the insect, and release nutrients from the corpse. The plant then absorbs the nutrients through its leaves. This 'leaf feeding' can be found in many non-carnivorous plants. Plants that were better at holding water and insects therefore had a selective advantage. Rainwater can be retained by cupping the leaf, leading to pitfall traps. Alternatively, insects can be caught by making the leaf stickier, leading to flypaper traps.
ensimple/4659.html.txt ADDED
@@ -0,0 +1,45 @@
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
1
+
2
+
3
+ Plants are one of six big groups (kingdoms) of living things. They are autotrophic eukaryotes, which means they have complex cells, and make their own food. Usually they cannot move (not counting growth).
4
+
5
+ Plants include familiar types such as trees, herbs, bushes, grasses, vines, ferns, mosses, and green algae. The scientific study of plants, known as botany, has identified about 350,000 extant (living) species of plants. Fungi and non-green algae are not classified as plants.
6
+
7
+ Most plants grow in the ground, with stems in the air and roots below the surface. Some float on water. The root part absorbs water and some nutrients the plant needs to live and grow. These climb the stem and reach the leaves. The evaporation of water from pores in the leaves pulls water through the plant. This is called transpiration.
8
+
9
+ A plant needs sunlight, carbon dioxide, minerals and water to make food by photosynthesis. A green substance in plants called chlorophyll traps the energy from the Sun needed to make food. Chlorophyll is mostly found in leaves, inside plastids, which are inside the leaf cells. The leaf can be thought of as a food factory. Leaves of plants vary in shape and size, but they are always the plant organ best suited to capture solar energy. Once the food is made in the leaf, it is transported to the other parts of the plant such as stems and roots.[5][6]
10
+
11
+ The word "plant" can also mean the action of putting something in the ground. For example, farmers plant seeds in the field.
12
+
13
+ Photosynthesis is a process that is taken place by the leaves on the plant. The leaves are the only parts of a plant that can do this process (as they adapted). This is also known as how the plant gets its food.You can make the process quicker by adding more CO2, light and chlorophyll.
14
+
15
+ Green algae:
16
+
17
+ Land plants (embryophyte)
18
+
19
+ At least some plant cells contain photosynthetic organelles (plastids) which enable them to make food for themselves. With sunlight, water, and carbon dioxide, the plastids make sugars, the basic molecules needed by the plant. Free oxygen (O2) is produced as a by-product of photosynthesis.[7]
20
+
21
+ Later, in the cell cytoplasm, the sugars may be turned into amino acids for proteins, nucleotides for DNA and RNA, and carbohydrates such as starch. This process needs certain minerals: nitrogen, potassium, phosphorus, iron and magnesium.[8]
22
+
23
+ Plant nutrition is the study of the chemical elements that are necessary for plant growth.
24
+
25
+ Macronutrients:
26
+
27
+ Micronutrients (trace elements) include:
28
+
29
+ The roots of plants perform two main functions. First, they anchor the plant to the ground. Second, they absorb water and various nutrients dissolved in water from the soil. Plants use the water to make food. The water also provides the plant with support. Plants that lack water become very limp and their stems cannot support their leaves. Plants which specialise in desert areas are called xerophytes or phreatophytes, depending on the type of root growth.
30
+
31
+ Water is transported from the roots to the rest of the plant through special vessels in the plant. When the water reaches the leaves, some of it evaporates into the air. Many plants need the help of fungi to make their roots work properly. This plant/fungi symbiosis is called mycorrhiza. Rhizobia bacteria in root nodules help some plants get nitrogen.[9]
32
+
33
+ Flowers are the reproductive organ only of flowering plants (Angiosperms). The petals of a flower are often brightly colored and scented to attract insects and other pollinators. The stamen is the male part of the plant. It is composed of the filament (a stalk) that holds the anther, which produces the pollen. Pollen is needed for plants to produce seeds. The carpel is the female part of the flower. The top part of the carpel contains the stigma. The style is the neck of the carpel. The ovary is the swollen area at the bottom of the carpel. The ovary produces the seeds. The sepal is a leaf that protects a flower as a bud.
34
+
35
+ The process by which pollen gets transferred from one flower to another flower is called pollination. This transfer can happen in different ways. Insects such as bees are attracted to bright, scented flowers. When bees go into the flower to gather nectar, the spiky pollen sticks to their back legs. The sticky stigma on another flower catches the pollen when the bee lands or flies nearby it.
36
+
37
+ Some flowers use the wind to carry pollen. Their dangling stamens produce lots of pollen that is light enough to be carried by the wind. Their flowers are usually small and not highly coloured. The stigmas of these flowers are feathery and hang outside the flower to catch the pollen as it falls.[10]
38
+
39
+ A plant produces many spores or seeds. Lower plants such as moss and ferns produce spores. The seed plants are the Gymnosperms and Angiosperms. If all the seeds fell to the ground besides the plant, the area might become overcrowded. There might not be enough water and minerals for all the seeds. Seeds usually have some way to get to new places. Some seeds can be dispersed by the wind or by water. Seeds inside juicy fruits are dispersed after being eaten. Sometimes, seeds stick to animals and are dispersed that way.[11]
40
+
41
+ The question of the earliest plant fossils depends on what is meant by the word "plant".
42
+
43
+ By the Silurian, fossils of whole plants are preserved, including the lycophyte Baragwanathia. From the Devonian, detailed fossils of rhyniophytes have been found. Early fossils of these ancient plants show the individual cells within the plant tissue. The Devonian period also saw the evolution of the first tree in the fossil record, Wattezia. This fern-like tree had a trunk with fronds, and produced spores.
44
+
45
+ The coal measures are a major source of Palaeozoic plant fossils, with many groups of plants in existence at this time. The spoil heaps of coal mines are the best places to collect; coal itself is the remains of fossilised plants, though structural detail of the plant fossils is rarely visible in coal. In the Fossil Forest at Victoria Park in Glasgow the stumps of Lepidodendron trees are found in their original growth positions.
ensimple/466.html.txt ADDED
@@ -0,0 +1,36 @@
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
1
+
2
+
3
+ Australopithecus [1] is a genus of extinct hominids closely related to humans.
4
+
5
+ The first Australopithecus described was the Taung Child, discovered by Raymond Dart, and described in 1925.
6
+
7
+ Their remains are mostly found in East Africa, and the first fossil is from 3.9 million years ago (mya). The split from other apes would have taken place earlier, perhaps about 5 mya.
8
+
9
+ It is widely believed that the group of which they are part gave rise to the genus Homo, and hence to human beings.[2]
10
+
11
+ The genus Australopithecus originally included two rather different forms. One form was lightweight: the gracile australopithecines. The other form was bulkier, the robust australopithecines.
12
+
13
+ It is still under discussion whether they should be put in separate genera. Here we treat the gracile forms; the robust forms are described elsewhere as Paranthropus.
14
+
15
+ Gracile australopithecines shared several traits with modern apes and humans. They were widespread throughout Eastern and Northern Africa 3.9 to 3 million years ago.
16
+
17
+ The brains of most species of Australopithecus were roughly 35% of the size of that of a modern human brain. This is not much more than the brain of a chimpanzee. Brain size in hominins does not increase significantly until the arrival of the genus Homo.
18
+
19
+ The Taung specimen had short canine teeth, and the position of the foramen magnum was evidence of bipedal locomotion.[3]
20
+
21
+ Most species of Australopithecus were diminutive and gracile, usually standing between 1.2 and 1.4 m tall (approx. 4 to 4.5 feet). There is a considerable degree of sexual dimorphism. Modern hominids do not show sexual dimorphism to the same degree — particularly, modern humans display a low degree of sexual dimorphism, with males being only 15% larger (taller, heavier) than females, on average.
22
+
23
+ In Australopithecus, however, males can be up to 50% larger than females, though usually less pronounced than this.[4]
24
+
25
+ The skeleton, the fossil footprints found at Laetoli,[5] Tanzania, the canine teeth and the foramen magnum all show that these apes had achieved bipedalism.
26
+
27
+ Australopithecus africanus used to be regarded as ancestral to the genus Homo (in particular Homo erectus).
28
+
29
+ However, fossils assigned to the genus Homo have been found that are older than A. africanus. Thus, the genus Homo either split off from the genus Australopithecus at an earlier date (the latest common ancestor being A. afarensis or an even earlier form, possibly Kenyanthropus platyops), or both developed from a common ancestor independently.
30
+
31
+ According to the Chimpanzee Genome Project, both human (Ardipithecus, Australopithecus and Homo) and chimpanzee (Pan troglodytes and Pan paniscus) lineages diverged from a common ancestor about 5 to 6 million years ago, if we assume a constant rate of evolution.
32
+
33
+ However, hominins discovered more recently are somewhat older than the molecular clock would suggest. Sahelanthropus tchadensis, commonly called "Toumai" is about 7 million years old and Orrorin tugenensis lived at least 6 million years ago. Since little is known of them, they remain controversial because the molecular clock in humans has determined that humans and chimpanzees had an evolutionary split at least a million years later.
34
+
35
+ One theory suggests that the human and chimpanzee lineages diverged somewhat at first, then some populations interbred around one million years after diverging.[6] More likely, the assumptions behind molecular clocks do not hold exactly. The key assumption behind the technique is that, in the long run, changes in molecular structure happen at a steady rate.
36
+ Researchers such as Ayala have challenged this assumption.[7][8][9]
ensimple/4660.html.txt ADDED
@@ -0,0 +1,45 @@
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
1
+ Parasitism is a form of one-sided symbiosis.[1][2] The parasites live off the host. They may, or may not, harm the host. Parasitoids, on the other hand, usually kill their hosts. A parasitic relationship is the opposite of a mutualistic relationship.[3] Examples of parasites in humans include tapeworms and leeches. World-wide, the most serious cause of human death by a parasite is malaria.
2
+
3
+ A definition:
4
+
5
+ "Humans are hosts to nearly 300 species of parasitic worms and over 70 species of protozoa, some derived from our primate ancestors and some acquired from the animals we have domesticated or come in contact with during our relatively short history on Earth. Our knowledge of parasitic infections extends into antiquity".[5]
6
+
7
+ When the above definition is applied, many organisms which eat plants can be seen as parasites, because they feed largely or wholly on one individual plant. Examples would include many herbivorous insects: the Hemiptera or true bugs (leafhoppers, froghoppers, aphids, scale insects and whiteflies). The larvae of Lepidoptera usually feed and mature on a single individual of the host plant species, and what they eat accounts for most of the food for their complete life span. Moreover, caterpillars can and often do serious damage to the host's foliage. Other orders also have many parasitic herbivores: Thysanoptera (thrips), Coleoptera (beetles), Diptera (flies).
8
+
9
+ Parasites of larger animals account for much research done for veterinarian and medical purposes. These parasites include viruses, bacteria, protozoa, flatworms (flukes and tapeworms), nematodes (roundworms), arthropods (crustacea, insects, mites). Parasitic wasps and flies are of great interest to the entomologist, and may be used in biological control.
10
+
11
+ On the other hand, many blood-sucking insects (such as mosquitoes) have only brief contact with a host, and so perhaps should not be regarded as parasites.[6]p5
12
+
13
+ A huge number of species are parasitic. A survey of the feeding habits of British insects showed that about 35% were parasites on plants, and slightly more were parasites on animals.[7] That means that nearly 71% of insects in Britain are parasitic. Since British insects are better known than those elsewhere (because of the length of time they have been studied), this means that the majority of insect species throughout the world are parasitic. Also, there are several other invertebrate phyla which are wholly or largely parasitic. Flatworms and roundworms are found in virtually every wild species of vertebrate. Protozoan parasites are also ubiquitous.[8] Hence parasitism is almost certainly the most common feeding method on Earth.
14
+
15
+ Parasites are adapted to small, separated habitats. For a parasite, each host is an island surrounded by a hostile environment.[9] For a small organism, the distances between hosts, or groups of hosts, is a hazard. Adaptations to bridge this hazard are:
16
+
17
+ So parasites exist in small, genetically similar groups with little flow of genes between them. In consequence, they have adaptations to solve their problems of dispersal and reproduction.[6]
18
+
19
+ Parasites face an environment which varies in time and space. Consequently, both local (geographic) races and polymorphism occur. Both may occur in the same species. Parasites are very specialised feeders: many species have only one host at any stage of their life cycle. A few use more than two host species.[6]
20
+
21
+ Many parasites have complex life-cycles. Tremadodes, the flukes, are a parasitic class of flatworms (Platyhelminths), with over 20,000 species. Most of them infect molluscs in the first part of the life-cycle, and vertebrates in the second part. The biology of scrub typhus is even more complex. It involves these factors:[11]
22
+
23
+ The occurrence of all these factors together would be limited in space, and brief in time. This is typical of the ecology of parasitic infections.
24
+
25
+ Both evolutionary rates and speciation rates can be high. Sibling species are very common in the bug Erythroneura, in which about 150 transfers from one host to another has resulted in about 500 species in the genus.[12]
26
+
27
+ The clearest evidence comes from the large size of many parasitic families.
28
+
29
+ Sometimes there is good evidence of the speed of speciation. For example, five or more species of the moth Hedylepta must have evolved within 1000 years in Hawaii, because they are specific to banana, which was only introduced then.[13]
30
+
31
+ Adaptive radiation in parasites is extensive. Its development in each taxon (group) depends on:
32
+
33
+ Diversity of hosts is a big factor. If many related species of host are available, then many related species of parasite will evolve. Mites on Lepidoptera families or fleas on mammals and birds are good examples. Eichler's rule goes as follows:
34
+
35
+ The two British oaks support some 439 species of parasite directly, and indirectly many hundred more which parasitise these parasites. "It would certainly be an underestimate to say that the two British species of oak are the primary products for a thousand species of parasite".[6]p28 Obviously, the large size of these trees is a factor in the number of parasite species. In general, this holds whether the host is a plant or an animal. A larger bird will harbour more species of ectoparasite than a small bird.
36
+
37
+ One of the reasons large trees have so many parasites is that they may have lived a long time in a particular area compared with other types of plant. They have had longer to accumulate parasites.
38
+
39
+ Parasites can be most useful in sorting out the phylogenetic relationships of their hosts. Sibling host species have been discovered when their parasites diverged. Common ancestors of present-day parasites were themselves parasites of the common ancestors of present-day hosts.
40
+
41
+ As the host evolves defences, so the parasite evolves to cope with this. This is co-evolution.
42
+
43
+ Consider two families of host plants, the Umbellifers (fennel, cumin, parsley, hemlock) and the Gramineae (grasses). The umbellifers have many aromatic species, and are chemically diverse and pharmaceutically interesting. Their resins and oils are defences against herbivory and parasitism. On the other hand, grasses have one big defence to herbivores: their stony inclusions in their cells wear down the teeth of herbivorous mammals, but they have few chemical defences. Both families are attacked by leaf-miner flies. There are four times as many grass species as there are umbellifers, but there are twice as many leaf-miner species on the umbellifers.
44
+
45
+ This is speciation which does not require geographical isolation. Ernst Mayr, the chief exponent of geographical speciation, admitted that host races of phytophagous animals "constitute the only known case indicating the possible occurrence of incipient sympatric speciation".[15]
ensimple/4661.html.txt ADDED
@@ -0,0 +1,45 @@
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
1
+
2
+
3
+ Plants are one of six big groups (kingdoms) of living things. They are autotrophic eukaryotes, which means they have complex cells, and make their own food. Usually they cannot move (not counting growth).
4
+
5
+ Plants include familiar types such as trees, herbs, bushes, grasses, vines, ferns, mosses, and green algae. The scientific study of plants, known as botany, has identified about 350,000 extant (living) species of plants. Fungi and non-green algae are not classified as plants.
6
+
7
+ Most plants grow in the ground, with stems in the air and roots below the surface. Some float on water. The root part absorbs water and some nutrients the plant needs to live and grow. These climb the stem and reach the leaves. The evaporation of water from pores in the leaves pulls water through the plant. This is called transpiration.
8
+
9
+ A plant needs sunlight, carbon dioxide, minerals and water to make food by photosynthesis. A green substance in plants called chlorophyll traps the energy from the Sun needed to make food. Chlorophyll is mostly found in leaves, inside plastids, which are inside the leaf cells. The leaf can be thought of as a food factory. Leaves of plants vary in shape and size, but they are always the plant organ best suited to capture solar energy. Once the food is made in the leaf, it is transported to the other parts of the plant such as stems and roots.[5][6]
10
+
11
+ The word "plant" can also mean the action of putting something in the ground. For example, farmers plant seeds in the field.
12
+
13
+ Photosynthesis is a process that is taken place by the leaves on the plant. The leaves are the only parts of a plant that can do this process (as they adapted). This is also known as how the plant gets its food.You can make the process quicker by adding more CO2, light and chlorophyll.
14
+
15
+ Green algae:
16
+
17
+ Land plants (embryophyte)
18
+
19
+ At least some plant cells contain photosynthetic organelles (plastids) which enable them to make food for themselves. With sunlight, water, and carbon dioxide, the plastids make sugars, the basic molecules needed by the plant. Free oxygen (O2) is produced as a by-product of photosynthesis.[7]
20
+
21
+ Later, in the cell cytoplasm, the sugars may be turned into amino acids for proteins, nucleotides for DNA and RNA, and carbohydrates such as starch. This process needs certain minerals: nitrogen, potassium, phosphorus, iron and magnesium.[8]
22
+
23
+ Plant nutrition is the study of the chemical elements that are necessary for plant growth.
24
+
25
+ Macronutrients:
26
+
27
+ Micronutrients (trace elements) include:
28
+
29
+ The roots of plants perform two main functions. First, they anchor the plant to the ground. Second, they absorb water and various nutrients dissolved in water from the soil. Plants use the water to make food. The water also provides the plant with support. Plants that lack water become very limp and their stems cannot support their leaves. Plants which specialise in desert areas are called xerophytes or phreatophytes, depending on the type of root growth.
30
+
31
+ Water is transported from the roots to the rest of the plant through special vessels in the plant. When the water reaches the leaves, some of it evaporates into the air. Many plants need the help of fungi to make their roots work properly. This plant/fungi symbiosis is called mycorrhiza. Rhizobia bacteria in root nodules help some plants get nitrogen.[9]
32
+
33
+ Flowers are the reproductive organ only of flowering plants (Angiosperms). The petals of a flower are often brightly colored and scented to attract insects and other pollinators. The stamen is the male part of the plant. It is composed of the filament (a stalk) that holds the anther, which produces the pollen. Pollen is needed for plants to produce seeds. The carpel is the female part of the flower. The top part of the carpel contains the stigma. The style is the neck of the carpel. The ovary is the swollen area at the bottom of the carpel. The ovary produces the seeds. The sepal is a leaf that protects a flower as a bud.
34
+
35
+ The process by which pollen gets transferred from one flower to another flower is called pollination. This transfer can happen in different ways. Insects such as bees are attracted to bright, scented flowers. When bees go into the flower to gather nectar, the spiky pollen sticks to their back legs. The sticky stigma on another flower catches the pollen when the bee lands or flies nearby it.
36
+
37
+ Some flowers use the wind to carry pollen. Their dangling stamens produce lots of pollen that is light enough to be carried by the wind. Their flowers are usually small and not highly coloured. The stigmas of these flowers are feathery and hang outside the flower to catch the pollen as it falls.[10]
38
+
39
+ A plant produces many spores or seeds. Lower plants such as moss and ferns produce spores. The seed plants are the Gymnosperms and Angiosperms. If all the seeds fell to the ground besides the plant, the area might become overcrowded. There might not be enough water and minerals for all the seeds. Seeds usually have some way to get to new places. Some seeds can be dispersed by the wind or by water. Seeds inside juicy fruits are dispersed after being eaten. Sometimes, seeds stick to animals and are dispersed that way.[11]
40
+
41
+ The question of the earliest plant fossils depends on what is meant by the word "plant".
42
+
43
+ By the Silurian, fossils of whole plants are preserved, including the lycophyte Baragwanathia. From the Devonian, detailed fossils of rhyniophytes have been found. Early fossils of these ancient plants show the individual cells within the plant tissue. The Devonian period also saw the evolution of the first tree in the fossil record, Wattezia. This fern-like tree had a trunk with fronds, and produced spores.
44
+
45
+ The coal measures are a major source of Palaeozoic plant fossils, with many groups of plants in existence at this time. The spoil heaps of coal mines are the best places to collect; coal itself is the remains of fossilised plants, though structural detail of the plant fossils is rarely visible in coal. In the Fossil Forest at Victoria Park in Glasgow the stumps of Lepidodendron trees are found in their original growth positions.
ensimple/4662.html.txt ADDED
@@ -0,0 +1,23 @@
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
1
+ Plate tectonics is a theory of geology. It explains movement of the Earth's lithosphere: this is the earth's crust and the upper part of the mantle. The lithosphere is divided into plates, some of which are very large and can be entire continents.
2
+
3
+ Heat from the mantle is the source of energy driving plate tectonics. Exactly how this works is still a matter of debate.[1]
4
+
5
+ The outermost part of the Earth's interior is made up of two layers. The lithosphere, above, includes the crust and the uppermost part of the mantle.
6
+
7
+ Below the lithosphere is the asthenosphere. The asthenosphere is like a solid or a hot viscous liquid. It can flow like a liquid on long time scales. Large convection currents in the asthenosphere transfer heat to the surface, where plumes of less dense magma break apart the plates at the spreading centers. The deeper mantle below the asthenosphere is more rigid again. This is caused by extremely high pressure.
8
+
9
+ There are two types of tectonic plates: oceanic and continental.
10
+
11
+ An oceanic plate is a tectonic plate at the bottom of the oceans. It is primarily made of mafic rocks, rich in iron and magnesium. It is thinner than the continental crust (generally less than 10 kilometers thick) and denser. It is also younger than continental crust. When they collide, the oceanic plate moves underneath the continental plate because of its density. As a result, it melts in the mantle and reforms. The oldest oceanic rocks are less than 200 million years old.
12
+
13
+ Continental plate is the thick part of the earth's crust which forms the large land masses. Continental rock has lower density than oceanic rock. They are mostly made of felsic rocks. These have granite, with its abundant silica, aluminum, sodium and potassium. Continental plates are rarely destroyed. Their oldest rocks seem to be 4 billion years old. Oceanic plates cover about 71 percent of Earth’s surface, while continental plates cover 29 percent.
14
+
15
+ Ocean lithosphere varies in thickness. Because it is formed at mid-ocean ridges and spreads outwards, it gets thicker as it moves further away from the mid-ocean ridge. Typically, the thickness varies from about 6 kilometres (3.7 mi) thick at mid-ocean ridges to greater than 100 kilometres (62 mi) at subduction zones.[1]
16
+
17
+ Continental lithosphere is about 200 kilometres (120 mi) thick. It varies between basins, mountain ranges, and the stable cratonic interiors of continents. The two types of crust differ in thickness, with continental crust being much thicker than oceanic: 35 kilometres (22 mi) vs. 6 kilometres (3.7 mi).[1]
18
+
19
+ The lithosphere consists of tectonic plates. There are seven major and many minor plates. The lithospheric plates ride on the asthenosphere (aesthenosphere). The plate boundary is where two plates meet. When movement occurs, the plates may create mountains, earthquakes, volcanoes, mid-oceanic ridges and oceanic trenches, depending on which way the plates are moving.[2][3][4][5][6]
20
+
21
+ Earthquakes, volcanic activity, mountain-building, and oceanic trench formation occur along plate boundaries. The lateral movement of the plates varies from:
22
+
23
+ Depending on how they are defined, seven or eight major plates are usually listed:
ensimple/4663.html.txt ADDED
@@ -0,0 +1,23 @@
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
 
1
+ Plate tectonics is a theory of geology. It explains movement of the Earth's lithosphere: this is the earth's crust and the upper part of the mantle. The lithosphere is divided into plates, some of which are very large and can be entire continents.
2
+
3
+ Heat from the mantle is the source of energy driving plate tectonics. Exactly how this works is still a matter of debate.[1]
4
+
5
+ The outermost part of the Earth's interior is made up of two layers. The lithosphere, above, includes the crust and the uppermost part of the mantle.
6
+
7
+ Below the lithosphere is the asthenosphere. The asthenosphere is like a solid or a hot viscous liquid. It can flow like a liquid on long time scales. Large convection currents in the asthenosphere transfer heat to the surface, where plumes of less dense magma break apart the plates at the spreading centers. The deeper mantle below the asthenosphere is more rigid again. This is caused by extremely high pressure.
8
+
9
+ There are two types of tectonic plates: oceanic and continental.
10
+
11
+ An oceanic plate is a tectonic plate at the bottom of the oceans. It is primarily made of mafic rocks, rich in iron and magnesium. It is thinner than the continental crust (generally less than 10 kilometers thick) and denser. It is also younger than continental crust. When they collide, the oceanic plate moves underneath the continental plate because of its density. As a result, it melts in the mantle and reforms. The oldest oceanic rocks are less than 200 million years old.
12
+
13
+ Continental plate is the thick part of the earth's crust which forms the large land masses. Continental rock has lower density than oceanic rock. They are mostly made of felsic rocks. These have granite, with its abundant silica, aluminum, sodium and potassium. Continental plates are rarely destroyed. Their oldest rocks seem to be 4 billion years old. Oceanic plates cover about 71 percent of Earth’s surface, while continental plates cover 29 percent.
14
+
15
+ Ocean lithosphere varies in thickness. Because it is formed at mid-ocean ridges and spreads outwards, it gets thicker as it moves further away from the mid-ocean ridge. Typically, the thickness varies from about 6 kilometres (3.7 mi) thick at mid-ocean ridges to greater than 100 kilometres (62 mi) at subduction zones.[1]
16
+
17
+ Continental lithosphere is about 200 kilometres (120 mi) thick. It varies between basins, mountain ranges, and the stable cratonic interiors of continents. The two types of crust differ in thickness, with continental crust being much thicker than oceanic: 35 kilometres (22 mi) vs. 6 kilometres (3.7 mi).[1]
18
+
19
+ The lithosphere consists of tectonic plates. There are seven major and many minor plates. The lithospheric plates ride on the asthenosphere (aesthenosphere). The plate boundary is where two plates meet. When movement occurs, the plates may create mountains, earthquakes, volcanoes, mid-oceanic ridges and oceanic trenches, depending on which way the plates are moving.[2][3][4][5][6]
20
+
21
+ Earthquakes, volcanic activity, mountain-building, and oceanic trench formation occur along plate boundaries. The lateral movement of the plates varies from:
22
+
23
+ Depending on how they are defined, seven or eight major plates are usually listed:
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1
+ A platelet is a cell fragment that circulates in the blood. Platelets are involved in hemostasis through the making of blood clots. A low platelet count (number of platelets in the blood) can cause a person to bleed without their blood clotting (making scabs). A high platelet count can increase the risk of thrombosis (blood clots inside blood vessels), which stops blood from flowing properly.
2
+
3
+ Platelets do not have a cell nucleus. They are disc-shaped, and are 1.5 to 3 micrometers in diameter. The body does not have a lot of platelets, so they can all be used up quickly. They contain RNA, a canalicular system, and several different types of granules; lysosomes (containing acid hydrolases), dense bodies (containing ADP, ATP serotonin and calcium) and alpha granules (containing fibrinogen, factor V, vitronectin, thrombospondin and von Willebrand factor), the contents of which are released when the platelet is activated.
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1
+ Plasma could mean:
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1
+ Platinum is a soft, heavy, white metal. It is a precious metal . It usually costs more than gold.
2
+ In chemistry, platinum is element number 78, and its atoms have an atomic weight of 195 a.m.u.. The symbol for platinum is Pt, from Spanish platina meaning "little silver".
3
+
4
+ Platinum is very malleable and ductile, which means it can be hammered into thin sheets and it can be pulled into wire. Platinum is very stable. Acids do not affect platinum.
5
+
6
+ The most common use of Platinum is in a vehicle's catalytic converter.
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1
+ Plato was one of the greatest classical Greek philosophers. He lived from 427 BC to 348 BC. Plato created the first university school, called "The Academy". Plato was a student of Socrates (who did not write) and the teacher of Aristotle, who founded another university, known as the Lyceum. Plato wrote about many ideas in philosophy that are still talked about today. He wrote about ideas of deductive reasoning. One modern philosopher, Alfred North Whitehead, said that all philosophy since Plato has just been comments on his works.
2
+
3
+ Plato wrote his books in the form of dialogues with two people or more talking about ideas, and sometimes disagreeing about them.
4
+
5
+ Socrates is usually the main person in Plato's dialogues. Usually, Socrates talks with people about their ideas, and tries to see if they believe anything that is illogical. Other people in the stories often become angry with Socrates because of this. People who study Plato argue about whether Socrates really said the same things that Plato makes him say, or whether Plato just used Socrates as a character, to make the ideas he was talking about seem more important.
6
+
7
+ Plato opposed the rhetorics of sophism and insisted on true justice and equality in his work Gorgias, and on immortality of soul in Phaedo.
8
+
9
+ One of Plato's most famous works is The Republic (in Greek, Politeia, or 'city'). In that work, he describes Socrates's vision of an "ideal" state. The method of questioning in this dialogue, called the Socratic method, is as important as the content. The Republic contains ideas of Socrates: "Socrates said it, Plato wrote it."
10
+
11
+ The Laws is Plato's longest dialogue and probably his last.[1]
12
+
13
+ There are many dialogues that were supposed to be written by Plato. This list includes those he probably did write.
14
+
15
+ Sources:
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1
+ Titus Macchius Plautus wrote plays in Ancient Rome. Many people just call him Plautus. He was probably born in Sarsina (a city in Romagna) around 254 BC. His comedies are among the earliest works of Latin literature that has not been lost. He is also one of the earliest writers of musical theater.
2
+
3
+ Little is known about Plautus' early life. When Plautus was young, he built stages for plays.[1] He also helped change the scenes.[1] This might be when he started to love the theatre. People noticed that he was a talented actor. He called himself "Macchius" (a clownish character in popular farces), and "Plautus" (a term meaning "flat-footed"). Tradition also says that after some time, he made enough money to start working in the shipping business. He started something, but he was not successful. He then is said to have worked as someone who worked with his hands. He learned about Greek drama – particularly the New Comedy of Menander – in his free time. His studies led to his plays being shown. The plays were first shown between c. 205 BC and 184 BC. Plautus' comedies are mostly adaptations of Greek plays for Roman people. They are usually based on the works of the Greek playwrights.[2]
4
+
5
+ H. M. Tolliver talks about the state gods of Rome and what their importance was in the Theatre of Plautus. These gods were an important part of the Romans' lives in Plautus’ time - people were supposed to worship them. Tolliver tells us that the gods were not exactly like the gods worshipped today. They were worshipped but also stood as a national symbol. State religion also served as a political tool. If the gods supported a bad leader, the people should too.
6
+
7
+ Plautus is sometimes accused of teaching the public indifference and mockery of the gods. Any character in his plays could be compared to a god. Whether to honour a character or to mock him, these references were demeaning to the gods. These references to the gods include a character comparing a mortal woman to a god, or saying he would rather be loved by a woman than by the gods. Pyrgopolynices from Miles Gloriosus (vs. 1265), in bragging about his long life, says he was born one day later than Jupiter. In Pseudolus, Jupiter is compared to Ballio the pimp. It is not uncommon, either, for a character to scorn the gods. This can be seen in Poenulus and Rudens.
8
+
9
+ Usually the only characters that scorn a god are those of low standing, like a pimp. Plautus perhaps does this to further demoralize the characters. Soldiers often bring ridicule among the gods. Young men, meant to represent the upper social class, often make fun of the gods in their remarks. Parasites, pimps, and courtesans often praise the gods with little ceremony. Tolliver argues that drama both reflects and foreshadows social change. It is likely that there was already much skepticism about the gods in Plautus’ time. Plautus did not make up or encourage irreverence to the gods, but used the ideas of his time. The state controlled stage productions, and Plautus’ plays would have been banned, had they been too risky.[3]
10
+
11
+ Gnaeus Naevius was another Roman playwright of the late third century BC. He wrote tragedies and even founded the fabula praetexta (history plays), in which he dramatized historical events. He fought in the First Punic War and his birth, therefore, is placed around the year 280 B.C.E.[4] His first tragedy took place in 235 B.C.E. Plautus would have been living at the exact time as Naevius, but began writing later.[5] Naevius is most famous for having been imprisoned by the Metelli and the Scipiones – two powerful families of the late third century. Naevius’ imprisonment and eventual exile is a case of state censorship. This fear of censorship may have influenced Plautus’ choice of what he wrote about and how he wrote about it.
12
+
13
+ While hundreds of plays have been attributed to Plautus' name, the canon consists of 20 surviving plays. To be able to use a more diverse set of characters, he developed what is called a stock character. He sometimes used typical situations where these characters could be used as well. He always used the same kinds of stock characters, especially if he could amuse the audience. As Walter Juniper wrote, “Everything, including artistic characterization and consistency of characterization, were sacrificed to humor, and character portrayal remained only where it was necessary for the success of the plot and humor to have a persona who stayed in character, and where the persona by his portrayal contributed to humor.”[6]
14
+
15
+ For example, in Miles Gloriosus, the titular “braggart soldier” Pyrgopolynices only shows his vain and immodest side in the first act, while the parasite Artotrogus exaggerates Pyrgopolynices’ achievements. Artotrogus creates more and more ludicrous claims that Pyrgopolynices agrees to without question. These two are perfect examples of the stock characters of the pompous soldier and the desperate parasite that appeared in Plautine comedies.
16
+
17
+ In this way, Plautus could greatly simplify complex characters and give the audience what it wanted. “The audience to whose tastes Plautus catered was not interested in the character play,”[7] instead it wanted humor that was easy to understand by many people. Stock setups offered such humor. Plautus used puns, he played with words, or he gave the words another meaning. Usually, the humorous characters in Plautine plays are of low social standing. This helps the comedy overall, because lower-class characters were often taken less seriously, and had to be less careful what they said.[8]
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1
+ The PlayStation 2 is Sony's second video game console. It was released in March of 2000. The one before this was PlayStation (or PS1). The next PlayStation is PlayStation 3 which was released in November 2006. The controllers of the PlayStation 2 and PlayStation 3 are the same but the PlayStation 3 is used wirelessly and doesn't have an analog button. Some games are online e.g. Call of Duty World at War Final Fronts and a few connect with the PlayStation Portable (or PSP). The PS2 is very successful and games are still made for it. The PlayStation 2 is the world's best-selling console. It has sold around 150 million units since its launch in March 2000, and is fully compatible with PlayStation (PS1) games. It competed with the Nintendo GameCube and the Microsoft Xbox. Sony announced that they had discontinued the PlayStation 2 in Japan on December 28, 2012 and worldwide on January 4, 2013.[1]
2
+
3
+ The PSX was released in 2003. It was a video recorder that allowed you to play PlayStation 2 games. It had a built-in hard drive (up to 250 GB). It did not sell well, because it cost too much money, so was not released outside of Japan.[2]
4
+ Grand Theft Auto: San Andreas became the most sold game, with over 27.5 million copies sold.
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1
+
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+
3
+ Australopithecus [1] is a genus of extinct hominids closely related to humans.
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+
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+ The first Australopithecus described was the Taung Child, discovered by Raymond Dart, and described in 1925.
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+
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+ Their remains are mostly found in East Africa, and the first fossil is from 3.9 million years ago (mya). The split from other apes would have taken place earlier, perhaps about 5 mya.
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+
9
+ It is widely believed that the group of which they are part gave rise to the genus Homo, and hence to human beings.[2]
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+
11
+ The genus Australopithecus originally included two rather different forms. One form was lightweight: the gracile australopithecines. The other form was bulkier, the robust australopithecines.
12
+
13
+ It is still under discussion whether they should be put in separate genera. Here we treat the gracile forms; the robust forms are described elsewhere as Paranthropus.
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+
15
+ Gracile australopithecines shared several traits with modern apes and humans. They were widespread throughout Eastern and Northern Africa 3.9 to 3 million years ago.
16
+
17
+ The brains of most species of Australopithecus were roughly 35% of the size of that of a modern human brain. This is not much more than the brain of a chimpanzee. Brain size in hominins does not increase significantly until the arrival of the genus Homo.
18
+
19
+ The Taung specimen had short canine teeth, and the position of the foramen magnum was evidence of bipedal locomotion.[3]
20
+
21
+ Most species of Australopithecus were diminutive and gracile, usually standing between 1.2 and 1.4 m tall (approx. 4 to 4.5 feet). There is a considerable degree of sexual dimorphism. Modern hominids do not show sexual dimorphism to the same degree — particularly, modern humans display a low degree of sexual dimorphism, with males being only 15% larger (taller, heavier) than females, on average.
22
+
23
+ In Australopithecus, however, males can be up to 50% larger than females, though usually less pronounced than this.[4]
24
+
25
+ The skeleton, the fossil footprints found at Laetoli,[5] Tanzania, the canine teeth and the foramen magnum all show that these apes had achieved bipedalism.
26
+
27
+ Australopithecus africanus used to be regarded as ancestral to the genus Homo (in particular Homo erectus).
28
+
29
+ However, fossils assigned to the genus Homo have been found that are older than A. africanus. Thus, the genus Homo either split off from the genus Australopithecus at an earlier date (the latest common ancestor being A. afarensis or an even earlier form, possibly Kenyanthropus platyops), or both developed from a common ancestor independently.
30
+
31
+ According to the Chimpanzee Genome Project, both human (Ardipithecus, Australopithecus and Homo) and chimpanzee (Pan troglodytes and Pan paniscus) lineages diverged from a common ancestor about 5 to 6 million years ago, if we assume a constant rate of evolution.
32
+
33
+ However, hominins discovered more recently are somewhat older than the molecular clock would suggest. Sahelanthropus tchadensis, commonly called "Toumai" is about 7 million years old and Orrorin tugenensis lived at least 6 million years ago. Since little is known of them, they remain controversial because the molecular clock in humans has determined that humans and chimpanzees had an evolutionary split at least a million years later.
34
+
35
+ One theory suggests that the human and chimpanzee lineages diverged somewhat at first, then some populations interbred around one million years after diverging.[6] More likely, the assumptions behind molecular clocks do not hold exactly. The key assumption behind the technique is that, in the long run, changes in molecular structure happen at a steady rate.
36
+ Researchers such as Ayala have challenged this assumption.[7][8][9]
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1
+ The PlayStation (often known as the PS1 or the PSX) is a video game console made by Sony. At the time, it was competing against the Nintendo 64 and the Sega Saturn. PlayStation games were stored on CDs. The controllers that were first released with the console had no analog joysticks on them, but analog joysticks and a vibration feature were added to later controllers. A slimmer version of the console called the PSOne was released in 2000. It was white instead of grey.
2
+
3
+ The PlayStation and the PSOne have sold over 120 million consoles.[1]
4
+
5
+ The PocketStation was a very small games console released as a peripheral (an extra accessory) for the PlayStation. It had a clock, an LCD display and four buttons. It could be used as a memory card.[2] It wasn't released in the United States, because it did not sell well.[3]
ensimple/4671.html.txt ADDED
@@ -0,0 +1,5 @@
 
 
 
 
 
 
1
+ The PlayStation (often known as the PS1 or the PSX) is a video game console made by Sony. At the time, it was competing against the Nintendo 64 and the Sega Saturn. PlayStation games were stored on CDs. The controllers that were first released with the console had no analog joysticks on them, but analog joysticks and a vibration feature were added to later controllers. A slimmer version of the console called the PSOne was released in 2000. It was white instead of grey.
2
+
3
+ The PlayStation and the PSOne have sold over 120 million consoles.[1]
4
+
5
+ The PocketStation was a very small games console released as a peripheral (an extra accessory) for the PlayStation. It had a clock, an LCD display and four buttons. It could be used as a memory card.[2] It wasn't released in the United States, because it did not sell well.[3]
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1
+ Lead (pronounce: "/'lɛd/") is a chemical element. Its chemical symbol is Pb, which comes from plumbum, the Latin word for lead.[3] Its atomic number is 82, atomic mass is 207.2 and has a melting point of 327.8°C. It is a very poisonous and heavy metal.
2
+
3
+ Lead is a shiny, gray-blue poor metal. It gets tarnished easily to a dull gray color. It is soft and malleable. It is very shiny when it is melted. It is very heavy. It is very corrosion-resistant. It is made stronger by adding antimony or calcium. It can form an alloy with sodium. It is toxic to people and animals when swallowed.
4
+
5
+ Lead burns in air with a grayish-white flame, making toxic fumes of lead(II) oxide. Only the surface is corroded by air. It dissolves in nitric acid to make lead(II) nitrate. It does not dissolve in sulfuric or hydrochloric acid. It reacts with sodium nitrate to make lead(II) oxide and sodium nitrite. It reacts with chlorine to make lead(II) chloride. Lead(II) oxide reacts with lead sulfide to make lead metal and sulfur dioxide.
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+
7
+ Lead makes chemical compounds in two main oxidation states: +2 and +4. +2 compounds, also known as lead(II) compounds or plumbous compounds, are weak oxidizing agents. +4 compounds, also known as lead(IV) compounds or plumbic compounds, are strong oxidizing agents. Lead compounds are toxic just like the element. The lead halides do not dissolve in water. Lead(IV) oxide is the most common lead(IV) compound. It is a black solid. The lead oxides are all colored, while the other salts are white or colorless. Lead nitrate and lead(II) acetate are the soluble compounds of lead.
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+
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+ This state is more common than the +4 state. These are weak oxidizing agents. All but the oxides are colorless or white.
10
+
11
+ Mixed oxidation state compounds contain lead in the +2 and +4 oxidation state.
12
+
13
+ These are less common. They are strong oxidizing agents.
14
+
15
+ Lead(II) chloride
16
+
17
+ Lead(II) nitrate
18
+
19
+ Lead(IV) oxide
20
+
21
+ Lead(II,IV) oxide
22
+
23
+ Lead(II) oxide
24
+
25
+ Lead found in the ground
26
+
27
+ Galena
28
+
29
+ Lead is found very rarely in the earth's crust as a metal. Normally, lead is in the mineral galena. Galena is lead sulfide. Galena is the main lead ore.
30
+
31
+ Lead was used for thousands of years because it is easy to get from the ground and easy to shape and work with. The Romans used lead very commonly. They used it for pipes, drinking vessels, and fasteners.
32
+
33
+ Lead is made from galena. Galena is made pure by froth flotation to get all the impurities out. Then the lead sulfide is roasted in a furnace to make lead(II) oxide. The lead(II) oxide is heated with coke to make liquid lead metal.
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+
35
+ Lead is used in the ballast of sailboats. It is also used in weight belts for scuba diving. It is also used to make shotgun pellets and bullets for small arms. Some printing presses use lead type because it can be easily shaped. It can be used outside because it does not corrode in water.
36
+
37
+ Most lead is used in lead acid batteries, though. The lead is oxidized, making electricity. Sheets of lead are used to block sound in some places. Lead is used in radiation shielding. Molten lead can be used as a coolant in nuclear reactors. It used to be mixed with tin to make the pipes in pipe organs. Different amounts of lead make different sounds. In addition, lead has found its usage in solder.
38
+
39
+ It is used in some solder. It is used in covering for wires that carry high voltage. Some tennis rackets have lead in them to make them heavier. It is used to balance wheels of cars, to make statues, and to make decorative looks in buildings.
40
+
41
+ Many lead compounds are used to make colored glazes in ceramics. Lead can be used in PVC pipes. Lead compounds are added to candles to make them burn better. Lead glass has lead(II) oxide in it. Lead compounds are still used as pigments in some places. Lead compounds were added to gasoline, but are now outlawed. Some lead compounds are semiconductors and are used in photodetectors.
42
+
43
+ Lead was used in many red, yellow, and white pigments in paints. Lead was also used in pesticides. Lead used to be used in pipes carrying water, but now it is not because lead can leach into the water.
44
+
45
+ Although it can be safely touched, exposure to lead should be avoided – it is very toxic to humans and other animals when swallowed, and its use is restricted in many countries.
46
+
47
+ If someone is exposed to lead for a long time, it ruins their kidneys and gives them abdominal pains. Lead also ruins the nervous system. Lead paint was being eaten by children and they were getting lead poisoning.
48
+
49
+ The best way to understand lead and its properties is to read its MSDS.
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1
+ Rain is a kind of precipitation. Precipitation is any kind of water that falls from clouds in the sky, like rain, hail, sleet and snow. It is measured by a rain gauge. Rain is part of the water cycle.
2
+
3
+ Clouds will often absorb smoke to create rain, commonly referred to as "nature's laundry" due to this process.
4
+
5
+ Some places have frequent rain. This makes rainforests. Some have little rain. This makes deserts.
6
+
7
+ A rainstorm is a sudden heavy fall of rain. It may cause flash floods in valleys. Heavy rain for a long time may make floods that destroy houses and drown people. Also, landslides may happen.
8
+
9
+ When the Sun heats the Earth's surface, the ground heats the air above it. Convection makes the air rise and cool. When it cools to the dew point, clouds form and rain follows.This usually occurs on flat land. This type of rainfall often causes summer showers and thunderstorms.
10
+
11
+ Relief rain usually occurs along coastal areas where a line of hills runs along the coast. When wet onshore wind from the sea meets a mountain, hill or any other sort of barrier, it is forced to rise along the slope and cools. When the air temperature falls to its dew point, water vapour condenses to form clouds. When the clouds can no longer hold the water droplets, relief rain begins to fall on the windward slope of the mountain. On the leeward slope, air sinks, it is warmed and further dried by compression. Therefore, the leeward slope is known as rain shadow. Moist winds blow in from the sea and are forced to rise over the land. The air cools and the water vapour condenses, forming rain drops. The rainiest places in the world are places that have relief rainfall.
12
+
13
+ Frontal rain happens when cooler air and warmer, humid air meet in a weather front. The less dense warm air rises and condenses forming clouds. These clouds grow and eventually create rain. In some places on the northern temperate zone the cold air front tends to come from the north west and the warm air front comes from the south west.
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1
+ Feathers are the things which cover birds. They help keep birds warm. Feathers also protect them from injury. In most kinds of birds, feathers help them to fly.
2
+
3
+ The main feathers which cover the outside of a bird are called vaned feathers. Vaned feather have a stiff center, with soft barbs on the side, which seem like hairs. The center is called a quill. This type of feather is called pennaceous (= like a pen).
4
+
5
+ Young birds have small feathers, called down, which keep them warm, but cannot be used for flying. Down is very soft. Adult birds have down, but also have vaned feathers on top of the down. Down is also used in blankets. Down feathers are just one example of plumaceous feathers (the word means 'fluffy'). Another example is the feathers on flightless birds such as the ostrich.
6
+
7
+ Birds lose their feathers at certain times. This is called moulting. By moulting, a bird can replace old feathers with new ones. Many birds moult once every year.
8
+
9
+ Feathers give birds colour. The function of colour in birds is extremely important. It includes:
10
+
11
+ People use feathers for many purposes. In the past, quills were commonly used as pens, and colorful feathers were worn on hats. Many pillows, cushions, mattresses, coats, and quilts are stuffed with down. Feathers are also used by people of many tribes for decoration.
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1
+ Feathers are the things which cover birds. They help keep birds warm. Feathers also protect them from injury. In most kinds of birds, feathers help them to fly.
2
+
3
+ The main feathers which cover the outside of a bird are called vaned feathers. Vaned feather have a stiff center, with soft barbs on the side, which seem like hairs. The center is called a quill. This type of feather is called pennaceous (= like a pen).
4
+
5
+ Young birds have small feathers, called down, which keep them warm, but cannot be used for flying. Down is very soft. Adult birds have down, but also have vaned feathers on top of the down. Down is also used in blankets. Down feathers are just one example of plumaceous feathers (the word means 'fluffy'). Another example is the feathers on flightless birds such as the ostrich.
6
+
7
+ Birds lose their feathers at certain times. This is called moulting. By moulting, a bird can replace old feathers with new ones. Many birds moult once every year.
8
+
9
+ Feathers give birds colour. The function of colour in birds is extremely important. It includes:
10
+
11
+ People use feathers for many purposes. In the past, quills were commonly used as pens, and colorful feathers were worn on hats. Many pillows, cushions, mattresses, coats, and quilts are stuffed with down. Feathers are also used by people of many tribes for decoration.