where did martians land in war of the worlds
The War of the Worlds The narrative opens by stating that as humans on Earth busied themselves with their own endeavours during the 1890s, aliens on Mars began plotting an invasion of Earth to replenish their limited resources. In 1899 the narrator is invited to an astronomical observatory at Ottershaw where explosions are seen on the surface of the planet Mars, creating much interest in the scientific community. Later, a "meteor" lands on Horsell Common, near the unnamed narrator's home in Woking, Surrey. He is among the first to discover that the object is an artificial cylinder that opens, disgorging Martians who are "big" and "greyish" with "oily brown skin", "the size, perhaps, of a bear", each with "two large dark-coloured eyes", and lipless "V-shaped mouths" which drip saliva and are surrounded by two "Gorgon groups of tentacles". The narrator finds them "at once vital, intense, inhuman, crippled and monstrous".[7] They briefly emerge, have difficulty in coping with the Earth's atmosphere and gravity, and rapidly retreat into their cylinder. A human deputation (which includes the astronomer Ogilvy) approaches the cylinder with a white flag, but the Martians incinerate them and others nearby with a heat-ray before beginning to assemble their machinery. Military forces arrive that night to surround the common, including Maxim guns. The population of Woking and the surrounding villages are reassured by the presence of the British Army. A tense day begins, with much anticipation of military action by the narrator.
Tharsis Geologic evidence, such as the flow direction of ancient valley networks around Tharsis, indicates that the bulge was largely in place by the end of the Noachian Period,[24] some 3.7 billion years ago.[26] Although the bulge itself is ancient, volcanic eruptions in the region continued throughout Martian history and probably played a significant role in the production of the planet's atmosphere and the weathering of rocks on the planet's surface.[27] By one estimate, the Tharsis bulge contains around 300 million km3 of igneous material. Assuming the magma that formed Tharsis contained carbon dioxide (CO2) and water vapor in percentages comparable to that observed in Hawaiian basaltic lava, then the total amount of gases released from Tharsis magmas could have produced a 1.5-bar CO2 atmosphere and a global layer of water 120 m thick.[24] Martian magmas also likely contain significant amounts of sulfur and chlorine. These elements combine with water to produce acids that can break down primary rocks and minerals. Exhalations from Tharsis and other volcanic centers on the planet are likely responsible for an early period of Martian time (the Theiikian[28]) when sulfuric acid weathering produced abundant hydrated sulfate minerals such as kieserite and gypsum.