Queanbeyan River [SEP] mouth of the watercourse
[{"answer": "Molonglo River", "provenance": [{"wikipedia_id": "2587820", "title": "Queanbeyan River", "start_paragraph_id": 5, "start_character": 443, "end_paragraph_id": 5, "end_character": 585, "bleu_score": 1.0, "meta": {}, "section": "Section::::River course.\n"}]}]
Molonglo River


it has been dammed by the Scrivener Dam to form Lake Burley Griffin. The river then flows to its mouth with the Murrumbidgee River, near Uriarra Crossing. Over its course the Molonglo River alternates between long broad floodplains and narrow rocky gorges several times. One of these floodplains is called the Molonglo Plain. From source to mouth, the river is traversed by the Captains Flat Road at , Briars-Sharrow Road in Carwoola, the Kings Highway between Queanbeyan and , the Yass Road, north of Queanbeyan, the Monaro Highway at
15421063
Garonne


most distant point (along watercourses from the river mouth) in the drainage basin from which water runs. The Ratera-Saboredo cirque is the "most distant point (along watercourses from the river mouth) in the drainage basin from which water runs", and the source of the Garonne, according to the United States Geological Survey, the National Geographic Society, and the Smithsonian Institution convention upon determining a stream's source. The Garonne follows the Aran Valley northwards into France, flowing via Toulouse and Agen towards Bordeaux, where
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Don River (Ontario)


The Don River is a watercourse in southern Ontario, that empties into Lake Ontario, at Toronto Harbour. Its mouth was just east of the street grid of the town of York, Upper Canada, the municipality that evolved into Toronto, Ontario. Of the various watercourses that drained Toronto, the Don, the Humber River, and the Rouge River have headwaters in the Oak Ridges Moraine. The Don is formed from two rivers, the East and West Branches, that meet about north of Lake Ontario while flowing southward into the
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Kolan River


then flows east and then finally north by east and reaches its mouth north of . The Kolan River is joined by nineteen tributaries including the main tributary, Gin-Gin Creek, a watercourse that is long. The lower reaches of the river are surrounded by sugar cane fields. The Mouth of Kolan River Regional Park is a protected area at the river mouth. The river descends over its course. Other water storage facilities that are supplied with water from the river include the Bucca Weir and the Kolan Barrage. "Macfadyena unguis
21876707
Queanbeyan railway bridges over Queanbeyan and Molonglo Rivers


The Queanbeyan railway bridges over Queanbeyan and Molonglo Rivers are two heritage-listed railway bridges on the Bombala railway line at Queanbeyan-Palerang Region, New South Wales, Australia. They were built in 1926. The first bridge crosses the Queanbeyan River from Queanbeyan to Queanbeyan East at , while the second bridge (approx to the east crosses the Molonglo River at Burbong (now Carwoola) at . The property is owned by RailCorp, an agency of the Government of New South Wales. It was added to the New South Wales State
21939017
Kampen, Overijssel


, the watercourse of the river IJssel was dredged several times, but the costs were relatively high and within a few years, the river silted up again. As the IJssel had several delta-like mouths here, the main route of the river shifted several times. In the 19th century, a new strategy was put in place to counter this problem: some watercourses were dammed to allow for more water at a higher speed through one or two main routes. This had the advantage that less sand and silt were deposited and
880447
Sepik


May 1885. But the river, in fact, did not yet have a European name. It was thus termed "Kaiserin Augustafluß" by the explorer and scientist Otto Finsch, after the German Empress Augusta. The word 'Sipik' was first reported by A. Full as one of two names for the watercourse—the other being 'Abschima'—used by the natives living at the mouth of the river. A few years later, Leonhard Schultze applied the term 'Sepik' to the entire watercourse, and it took, although Schultze
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Queanbeyan River


Queanbeyan River into a valley at the eastern end of the Limestone Plains near present-day Canberra. The Queanbeyan River was the main water supply for the towns of Queanbeyan and during its early history it was an integral element to its economy. Wool scouring (cleaning) was carried out in the river near presentday Oaks Estate, formerly a part of Queanbeyan. The first significant flood after European settlement of the site of Queanbeyan City was in 1851: others followed twice in 1852, twice in 1861, twice in 1870, 1891
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Josiah Gregg


the mouth of a watercourse which they called the Little River. After exploring slightly to the north, they turned south along the coast and camped at Trinidad. Leaving Trinidad, they crossed a large river, but the fed-up members of the exploring party did not wish to wait for Gregg to determine the latitude of the mouth, and so pushed off without him. When he caught up with the group, his temper flared, and they named the river Mad River due to the outburst. On 20 December 1849,
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Queanbeyan


west, and Queanbeyan has to some extent become a commuter town. The word "Queanbeyan" is the anglicised form of "Quinbean", an Aboriginal word meaning ""clear waters"". The town grew from a squattage held by ex-convict and inn keeper, Timothy Beard, on the banks of the Molonglo River in what is now Oaks Estate. The town centre of Queanbeyan is located on the Queanbeyan River, a tributary of the Molonglo River and approximately south-southeast of Oaks Estate. Queanbeyan was officially
15690884
List of islands within the Murray River in South Australia


List of islands within the Murray River in South Australia is a list of islands located within the watercourse of the Murray River within the Australian state of South Australia from the mouth of the river at Encounter Bay in the south to the borders with the states of New South Wales and Victoria in the east including the following lakes located adjacent to the river's mouth - Coorong, Lake Albert and Lake Alexandrina. The following list includes islands (listed from west to east) in the Coorong as well as the following two channels connecting
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Queanbeyan railway bridges over Queanbeyan and Molonglo Rivers


Heritage Register on 2 April 1999. The bridges were first built by contractors Johnston & Co. in 1885-87 along with the extension of the railway from Bungendore to Michelago through Queanbeyan. The Molonglo River bridge was completed in May 1886 and the Queanbeyan River bridge in July 1887, both opening with the line in September 1887. The original bridges consisted of arched hardwood timber girders on brick piers and stone abutments, featuring four spans (Molonglo River) and five spans (Queanbeyan River) of 80ft each. The stone for
21939018
Queanbeyan River


vicinity of Googong Dam, and native Macquarie perch, which extended to at least the headwaters of Googong Dam. Due to this abundance of native fish, the Queanbeyan River, along with the Molonglo River, was often known as the "Fish River" in the early days of settlement. Sometimes the Queanbeyan River was further distinguished by being called the "South Fish River". On more than one occasion in the late 19th and early 20th centuries floods deposited live Murray Cod in the main streets of Queanbeyan. A variety of
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Goat Rock Beach


, especially in the pupping season. The Russian River, with its mouth at the north end of Goat Rock Beach, is Sonoma County's largest watercourse, both in flow rate and lineal extent. Immediately beyond the Russian River discharge to the Pacific Ocean is the coastal town of Jenner. North of the mouth of the Russian River is Jenner Beach. Goat Rock protrudes into the Pacific at the south end of Goat Rock Beach. Visitors can access the base of Goat Rock via a low lying isthmus of land which has been
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Queanbeyan River


The Queanbeyan River, a perennial stream that is part of the Molonglo catchment within the Murray–Darling basin, is located in the Monaro and Capital Country regions of New South Wales and the Australian Capital Territory, in Australia. The river is in length with a catchment area of . The Queanbeyan River and the Cotter River meet the potable water supply needs of the Canberra and Queanbeyan region and whose water quality is specifically protected under Federal legislation. It is believed that the local Aboriginal Ngarigo people used a word that sounded like "
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Queanbeyan River


queanbeyan" to describe the river, said to mean "clearwater". The headwaters of the Queanbeyan River rise east-southeast of Queanbeyan and about northeast of the township of Bredbo, near the village of Jerangle. Fourteen tributaries upstream of the Googong Dam contribute to the river flow including the Burra, Urialla, Tinderry, Ballinafad, Groggy, Woolpack, Sherlock, Lyons, Towneys and Mile Creeks. The major river crossings above Googong Dam are the Boolboolma causeway on the Tinderry Road and a road bridge on the Captain's Flat
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Queanbeyan East


Queanbeyan East is a suburb of Queanbeyan in New South Wales, Australia. It is on the north eastern side of the Queanbeyan River, with the river forming its western boundary. At the , it had a population of 3,936. The suburb is a mixed residential and industrial zone, incorporating Queanbeyan's (and one of the region's largest) manufacturing and general industrial hubs along the eastern length of Yass Road. East Queanbeyan is predominantly residential however, featuring a mix of high density units and free standing homes. In recent
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Queanbeyan River


ills including introduction of exotic fish such as trout, overfishing, willow encroachment, siltation, and weirs blocking migration saw native fish populations in the Queanbeyan River close to extinction by the time Googong Dam was built. Under the , the Government of New South Wales guaranteed the Australian Capital Territory access to resources including water by protecting and not polluting the waters of the Queanbeyan River. The condition of the river as a native habitat below Googong Dam has been seen as unhealthy in recent years by the Queanbeyan City Council, with the river
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City of Queanbeyan


Queanbeyan City was a local government area located in south eastern New South Wales, Australia. The former area is located adjacent to Canberra and the Australian Capital Territory, the Queanbeyan River, the Molonglo River, the Kings Highway and the Sydney-Canberra railway. On 12 May 2016 the Minister for Local Government announced dissolution of Queanbeyan City with immediate effect. Together with the Palerang Council the combined council areas were merged to establish the Queanbeyan-Palerang Regional Council. The last Mayor of the Queanbeyan City Council was Tim Overall, an
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Queanbeyan River


with scores of bodies washed downstream into Lake Burley Griffin. In December 2010 the Queanbeyan River peaked at and broke its banks, flooding the Queanbeyan Riverside tourist park. All schools in the area were closed and some local schools were used as shelter for evacuated residents of around 100 houses and businesses. Following extensive rains in the catchment, in March 2012 there were flooding alerts, however the river did not breach its banks. The Queanbeyan River was renowned as a beautiful river abounding in native Murray Cod, which once extended to the
6804804
King Sound


King Sound is a large gulf in northern Western Australia. It expands from the mouth of the Fitzroy River, one of Australia's largest watercourses, and opens to the Indian Ocean. It is about 120 km long, and averages about 50 km in width. The port town of Derby lies near the mouth of the Fitzroy River on the eastern shore of King Sound. King Sound has the highest tides in Australia, and amongst the highest in the world, reaching a maximum tidal range of 11.8 metres at Derby. The
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Queanbeyan River


-Jerangle Road. Once inside the city precinct of Queanbeyan, the river is crossed by several bridges, including the Canberra-Goulburn railway, Morisset Street bridge, the Queens Bridge on Monaro Street (which becomes Bungendore Road or Kings Highway), and by a pedestrian footbridge near Isabella Street in East Queanbeyan. Queens Bridge was opened by Wal Fife MP, Minister for Transport and Highways on the 21 July 1975, according to a plaque on the bridge. The Queanbeyan River meets the Molonglo River at a confluence located in Oaks
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Queanbeyan railway bridges over Queanbeyan and Molonglo Rivers


the abutments came from the quarries at Pyrmont in Sydney. A temporary bridge over the Queanbeyan River during construction was reported at the time to be the largest temporary railway bridge ever constructed in New South Wales. The bridges were completely rebuilt in 1926-27 at a cost of £19,000, reusing the foundations of the original bridge. Both bridges were of the Warren deck steel truss type, consisting of four 44ft. steel spans on the approaches to each side with three (Queanbeyan River) and two (Molonglo River)
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Waswanipi River


of Chibougamau. A bridge spans the river at the village of Waswanipi. From its source, the course of the river flows over distributed as follows: The mouth of the Waswanipi River is located at: As early as XVIIIth century, the designation "Waswanipi" means a lake Waswanipi, two rivers and a Native American group. The river has already been referred to as "Olga River". A map of 1898 indicates "R. Waswanipi" for this watercourse. At the beginning of the XXth century, during a voyage
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Queanbeyan railway bridges over Queanbeyan and Molonglo Rivers


spans of 90ft comprising the main bridge. The timbers of the original bridge were still in "a remarkable state of preservation" when replaced, such that it could not be cut in some cases. The bridge upgrade allowed a heavier type of engine to be run on the line. The Molonglo River bridge is sometimes known as the Burbong bridge, Burbong being a historical name for its location. The Queanbeyan rail bridges over Queanbeyan and Burbong Rivers was listed on the New South Wales State Heritage Register on 2 April 1999 having
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Queanbeyan River


Estate, within the boundary of the Australian Capital Territory. The river descends over its course. The river's catchment area is , more than double that of the Cotter River. The Queanbeyan Weir was constructed originally in 1901-2 which provided a pool in the Queanbeyan River near the centre of the town for the town's water supply. It is now a place for town beautification with several parks located along the river, such as Blundell Park, Queen Elizabeth Park, and Ray Morton Park. The weir also provides for
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Queanbeyan


Queanbeyan is a city in south-eastern region of the Australian state of New South Wales, located adjacent to the Australian Capital Territory in the Southern Tablelands region. Located on the Queanbeyan River, the city is the council seat of the Queanbeyan-Palerang Regional Council. At the , the Queanbeyan part of the Canberra–Queanbeyan built-up area had a population of 36,348. Queanbeyan's economy is based on light construction, manufacturing, service, retail and agriculture. Canberra, Australia's capital, is located just to the
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Queanbeyan


's first newspaper and was founded in 1860 by John Gale. In 1880 the residence of John James Wright, the first mayor of Queanbeyan, was constructed along the edge of the Queanbeyan River. In 1982 that building became the Queanbeyan Art Centre. The Salvation Army claimed an outpost in Queanbeyan in 1884. Queanbeyan, an increasingly successful primary producing district, was proclaimed a Municipality in February 1885 incorporating an area of . The railway reached Queanbeyan railway station in 1887 and it became the junction for the lines going to Canberra and Bombala
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Sableuse River


The Sableuse River is a watercourse in the Matapedia Valley, in administrative region of Bas-Saint-Laurent, in Quebec, Canada. Its origin lies in the Sableuse ponds in Saint-Vianney while its mouth lies in the Sableuse River Bay on Lake Matapedia. This river flows into the regional county municipalities (RCM): This course river of the Matapedia Valley is descending towards the Southwest; it passes through the territory of Sainte-Paule and Matapedia Lake (at the Eastern boundary of the territory of Sayabec). The
13244144
Tartigou River


The Tartigou River is a watercourse over long in the Matapedia Valley in Quebec, Canada. Its origin lies in the Bon-Dieu Lake in Saint-Moïse, while its mouth is on the Saint Lawrence in Baie-des-Sables. The name "Tartigou" comes from a transcription of the Mi'kmaq word "tlagatigotj". "Tartig" means "river of the little colony" or "little river of the colony." The Tartigou River takes its water from the Matapedia Valley in the Bas-Saint-Laurent
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Cooum River


and Chinese coins on the banks of the river. In the late eighteenth century, Pachaiyappa Mudaliar, the renowned philanthropist, bathed in this river before offering prayers at the Komaleeswarar Temple in Komaleeswaranpet. Cooum River and the nearby Elambore River (or North River), which flows into the Cooum at its mouth, were running very close to each other near the former Central Jail area opposite Chennai Central. During floods, both the watercourses inundated the whole area. In the 1700s, the two rivers were linked by a cut to
18984612
Vrbas (river)


the river Sava. The Vrbas river appears at the southern slope of the Vranica mountain near the town of Gornji Vakuf, at around above sea level and it drains central part of the northern slopes of the Dinaric mountain massif. It empties into the Sava river at around above sea level. Total length of the main watercourse is around . Average annual rainfall is around 800 l/m at the mouth of the Vrbas to the Sava river and up to 1500 l/m in the southern part of the basin. Characteristic mean
12890336
Santry River


two watercourses are the Fox Stream, reaching the sea at the end of Fox's Lane, and the Blackbanks Stream, with its mouth where Howth Road and the James Larkin Road meet. As part of the management of the river, the Santry river is one of the third tier rivers being numerically mapped within the Greater Dublin Strategic Drainage Study, with floodplain hydraulics computed (the other rivers being the Carrickmines, Deansgrange or Kill of the Grange, Poddle, Camac, Finglas and Mayne, along with one of the two second
14637618
Nata River


The Nata River or Manzamnyama River is a natural watercourse in Southern Africa. It is an ephemeral river flowing in Zimbabwe and Botswana. It has a length of 330 km from its source to mouth, 210 km in Zimbabwe and 120 km in Botswana. Its total catchment area is 24,585 km. The river originates in Sandown (S20.425036˚, E28.180660˚), a small farming town located on the Zimbabwean central watershed 50 km south west of Bulawayo and ends in the Makgadikgadi Pans (S20.348816˚, E26.240166˚) in Botswana. There is no
15291292
Sand River (Limpopo)


The Sand River or Polokwane River () is a watercourse in Limpopo Province, South Africa, a right hand tributary of the Limpopo River. Its new name "Polokwane River" is homonymous with the name of the town of Polokwane, formerly Pietersburg, about upriver from its mouth. The Sand River flows by the western edge of this town. It has its source south of Mokopane and flows northwards across central Limpopo Province until it cuts across the Soutpansberg through a deep gorge, the Waterpoort. Then it meanders northwards across the
2902236
Humber


. The estuary appears in some Latin sources as (A name used by Edmund Spenser in "The Faerie Queene"). This is possibly a Latinisation of the Celtic form (Welsh for river mouth or estuary), but is erroneously given as a name for both the Humber and The Ouse as one continuous watercourse. Both and may record an older Indo-European word for water or river, (as in the ‘Five Rivers’ of the Punjab). An alternative derivation may be from the Latin verb meaning black
14140060
List of rivers of Europe


) The choice of the source obviously has an impact. Here we attempt to list the most distant source. When that involves a tributary nearer the mouth of the river, the length of the nominal river is listed as well, if it meets the above criteria. 3) Rivers flowing into estuaries have an arbitrary end. Its channel through an estuary is usually included in the length when it is exposed at low tide. 4) The length of a watercourse through a reservoir or lake is open for interpretation. For this
19519261
Ayr


meaning "watercourse" or "strong river". This name was used before the establishment of the Julian calendar in reference to the River Ayr. The town was formerly known as 'Inverair' or 'Inverayr', meaning "mouth of the river Ayr", yet this was later abbreviated to 'Air', and then to 'Ayr'. Elements of the old name remain present within the Scottish Gaelic name for Ayr – "Inbhir Air". The areas surrounding modern day Ayr were known to have been occupied
10090348
Akerselva


Akerselva or Akerselven () is a river which flows through Oslo. It starts at Maridalsvannet in Oslomarka, and follows the urban areas Nordre Aker, Sagene, Grünerløkka, Oslo centre and Grønland, whereby it finally ends at Paulsenkaien and Oset in Bjørvika. The river is considered to be a part of the Nordmarkvassdraget, and has the watercourse number 006.Z. The entire river is about long, and has a difference in elevation between source and mouth of approximately . Earlier, the river gave power to numerous industry companies in Oslo. Akerselven
20829471
Narran River


Narran River, a watercourse of the Barwon catchment within the Murray–Darling basin, is located in the Southern Downs district of Queensland and Orana district of New South Wales, Australia. The river rises south west of Dirranbandi, as a branch of the Balonne River in Queensland, and flows generally to the south and south-west, before reaching its mouth at Narran Lake, between Brewarrina and Walgett in New South Wales; descending over its course. In March 2010 the Narran River flooded the Angledool Lake at Angledool and then
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Googong Dam


Googong Dam is a minor ungated earth and rock fill with clay core embankment dam with concrete chute spillway plus a nearby high earthfill saddle embankment across the Queanbeyan River upstream of Queanbeyan in the Capital Country region of New South Wales, Australia. The dam's purpose includes water supply for Canberra and Queanbeyan. The impounded reservoir is called Googong Reservoir. Googong Dam was created through enabling legislation enacted via the passage of the . Completed in 1979, the Googong Dam is a minor dam on the Queanbeyan River and Bradleys Creek and is located
17700761
List of rivers of County Dublin


There are more than 130 named rivers and streams in County Dublin, Ireland, which comprises the city of Dublin and the surrounding administrative counties. The rivers and streams are listed in one table, with systems such as the Liffey (and that of its major sub-system, the Dodder), Broadmeadow, Tolka and Shanganagh identified within the table. The name of each watercourse, the location of its mouth or confluence point and whether, for tributaries, they enter their parent on the right or left bank, is noted
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Roi Et Province


(101) and the provincial name was written accordingly. Later, people took "๑๐๑" to mean 'one hundred and one' and have since then called it "Roi Et". Most of the province is covered by plains about 130–160 meters above sea level, drained by the Chi River. In the north are the hills of the Phu Phan mountain range. The Yang River is the major watercourse. In the south is the Mun River, which also forms the boundary with Surin. At the mouth of the
7190138
Wimmera River


Dividing Range below , between and , and flows generally north and west, through , , and , also forming the eastern boundary of the Little Desert National Park. It is joined by fourteen minor tributaries, including the Mackenzie River, before reaching its mouth at Lake Hindmarsh, near Jeparit. The river descends over its course. On the rare occasions that Lake Hindmarsh overflows, water flows via Outlet Creek to Lake Albacutya. In most years the Wimmera River's flow does not reach these terminal lakes, and the watercourse itself contracts
11861037
Jadro


The Jadro is a watercourse in Dalmatia, Croatia that discharges to the Adriatic Sea. The upper reaches of the Jadro River, as well as its source, Jadro Spring, are protected as an ichthyological nature reserve, partly due to the presence of an endemic species of soft-mouthed trout. The headwaters of the Jadro River were the original water supply for the ancient city comprised by Diocletian's Palace (now an area within the present day city of Split). Contemporary studies indicate favourable water quality levels of the river near
12127374
Toronto waterway system


Bay Park East. The Source of the River is the Huber Spring Pond and the basin is 903 km . The Don River is a watercourse in southern Ontario, that empties into Lake Ontario, at Toronto Harbour. Its mouth was just east of the street grid of the town of York, Upper Canada, the municipality that evolved into Toronto, Ontario. The Don is formed from two rivers, the East and West Branches, that meet about 7 kilometres (4 mi) north of Lake Ontario while flowing southward into the
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Dinan


Petit Fort. This river has moderate turbidity and its brownish water is somewhat low in velocity due to the slight gradient of the watercourse; pH levels have been measured at 8.13 within the city of Dinan and electrical conductivity of the waters have tested at 33 micro-siemens per centimetre. In the centre of Dinan the Rance summer flows are typically in the range of . For many years, the bridge over the River Rance at Dinan was the most northerly crossing point on the river, but the tidal power station at the mouth
17693802
Acari River (Rio de Janeiro)


The Acari River is located in Rio de Janeiro state in southeastern Brazil. It is one of the major watercourses of the city of Rio de Janeiro. The name is of Guarani origin, a corruption of "aqûâ-ára-i", meaning "enduring current". It is not related to the Loricariidae "Acari" fish. The Acari River rises in the Serra do Gericinó with its mouth on the Rio Meriti which separates the city of Rio from Duque de Caxias. The Acari flows through the city from the
22091328
River Thaw


damage to 4 properties in Cowbridge, 4 in Aberthin, and 17 in Llanblethian. The flooding was caused by flood water over-topping the banks of main rivers and ordinary watercourses, and restrictions to flow in channels and surcharging of drains. The river meets the Bristol Channel at a shingle beach called Leys Beach, at Breaksea Point, one of the southernmost points of Wales. It flows through the village of Aberthaw. At its mouth is the Aberthaw Power Station, which is split into two complexes, Aberthaw A and Aberthaw
4080277
Wiese


in turn deflected by an existing Nagelfluh gravel bank, which resulted the striking 90° bend in the lower reaches of the Wiese. Up to the beginning of the 19th century, the Wiese flowed largely unregulated from its source in the Black Forest to its mouth on the Rhine, swinging between the scarp of the lower river terrace and carving its way through the gravel and sandbanks of the river meadows. The annual floods frequently resulted in a change in the course of the river. Only the Wiesewuhre, an artificial watercourse that used
4112702
Karabar


Karabar is a suburb of Queanbeyan, New South Wales. It is at the southern part of the developed area of Queanbeyan—-bordering the suburbs of Queanbeyan East, Jerrabomberra, Googong and Queanbeyan. The eastern border of the suburb is defined by the Queanbeyan River. As well as a shopping centre it contains netball courts, several ovals and a public high and primary schools. It is dominated by Mount Jerrabomberra, which overlooks the suburb. At the , Karabar had a population of 8,247 people. The Karabar High School and Distance Education Centre
4999942
Kawaree


and Charles Throsby Smith came upon two small streams forming a single river winding through a valley at the eastern end of the Limestone Plains. These were later named the Molonglo River and the Queanbeyan River. The first non-Aboriginal use of land at Queanbeyan was by an unauthorised occupant, Timothy Beard, who called his property "Quinbean" which is thought to be an Aboriginal word for "clear water". This gave the city its modern name, Queanbeyan. The area became a natural stop for travellers crossing into the Monaro
21938561
Queanbeyan Showground


search of the Murrumbidgee River and "discovered" the Molonglo Plains. Severe drought during the 1820s impelled colonists to search for more pasture land and in 1828 Major H. C. Antill from Picton sent his cattle and sheep to Molonglo Plains. The town of Queanbeyan grew up on the lands owned by innkeeper Timothy Beard, who had a collection of huts on the banks of Molonglo River. The town centre later shifted to the Queanbeyan River about one mile east and was officially proclaimed as a township in 1838 with a population of 50.
21938671
Queanbeyan Nature Reserve


recorded. The reserve is managed by the NSW National Parks and Wildlife Service. The Queanbeyan area is part of the traditional lands of the Ngunawal people. European settlement in the Queanbeyan area commenced in the 1820s and the township developed on the Queanbeyan River, about from the current Queanbeyan Nature Reserve. The land now protected by the reserve was largely used for grazing sheep and cattle. Evidence of early settlement include a windbreak of large pines on the western boundary, dating to the early 1900s, and the site of a former dwelling
19563031
Integrated urban water management in Buenos Aires, Argentina


the world's fifth largest river basin – the La Plata, extending over 3.1 million km, five countries (Argentina, Bolivia, Brazil, Paraguay, and Uruguay), almost 50 major cities, and supporting over 100 million inhabitants. The mouth of the La Plata River is 230 km wide and separates Argentina from Uruguay. The three main watercourses that form the base structure for the region's drainage network are the Luján, Reconquista, and Matanza-Riachuelo Rivers. The Luján River, 128 km, has the largest catchment
10044671
Santa Clara River (Utah)


near the river's mouth. Archaeological evidence shows that Ancestral Puebloans (also known as the Virgin Anasazi) lived in the area from 700 B.C. to A.D. 1200 and that they had developed irrigation for their farmed crops. Their population increased until about A.D. 1200, when all Anasazi populations collapsed. They were replaced by the Southern Paiute, who also farmed along the watercourse. The first Europeans to see the river were Fathers Escalante and Dominguez on the Dominguez-Escalante Expedition. When they arrived on the upper Virgin River watershed on October
1293327
Greenough River


Geraldton–Dongara railway line, to the vicinity of Rudds Gully. Both watercourses then flowed north to discharge into the Chapman River. Later, Rudds Gully cut its own path to the ocean, and the Greenough River discharged into it; and later still, the Greenough cut its own path through the limestone ridge at Walkaway, thus forming its own course. The well-documented strong winds at Greenough have resulted in large mobile dune systems both to the south and north of the Greenough River mouth. Both are gradually moving northwards
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River source


definition of a river source specifically uses the most distant point (along watercourses from the river mouth) in the drainage basin from which water runs year-around (perennially), or, alternatively, as the furthest point from which water could possibly flow ephemerally. The latter definition includes sometimes-dry channels and removes any possible definitions that would have the river source "move around" from month to month depending on precipitation or ground water levels. This definition, from geographer Andrew Johnston of the Smithsonian Institution, is also used
20534038
HMS Endeavour


harbour in which to make repairs. On 13 June, the ship came to a broad watercourse that Cook named the Endeavour River. Cook attempted to enter the river mouth, but strong winds and rain prevented "Endeavour" from crossing the bar until the morning of 17 June. She grounded briefly on a sand spit but was refloated an hour later and warped into the river proper by early afternoon. The ship was promptly beached on the southern bank and careened to make repairs to the hull. Torn sails and rigging were also
14042976
Lunan Water


The Lunan Water is an easterly flowing river in Angus, Scotland, that discharges to the North Sea north of the town of Arbroath. Draining chiefly agricultural lands, this stream has a moderate level of turbidity and a pH level of approximately 8.7. Other nearby watercourses discharging to the North Sea include River North Esk and River South Esk, both to the north. At its mouth the Lunan Water meets the North Sea at the hamlet of Lunan, upon Lunan Bay. The beach at Lunan Bay was voted the "best beach
3598019
Patawalonga River


before European settlement, a tidal estuary. The river is serviced by a catchment area that exists in metropolitan Adelaide, with its mouth at the suburb of Glenelg. The Patawalonga serves as an outlet for the Keswick and Brownhill creeks and the Sturt River (also known as Sturt Creek), the latter being a former natural creek comprising for a significant part of its length now as a large concrete storm-drain. The catchment includes the Cowandilla-Mile End drainage network, the construction of which has replaced numerous small natural watercourses
9459104
Parish of Carwoola


Carwoola Parish is a parish of Murray County, a cadastral unit for use on land titles. It is located to the south of the Australian Capital Territory and to the south-east of Queanbeyan. The original northern and eastern boundary was the Molonglo River; this is still the boundary for most of the parish, except in the north, where the relatively small area north of the Queanbeyan-Goulburn railway line (at ) was transferred to the ACT in 1909. The south-western boundary is the Queanbeyan River. Captain
22208488
Queanbeyan East


years a number of new mini housing estates have been completed (or are under construction), adding significantly to the population, and providing new housing stock. Additionally a new high density residential complex has been completed adjacent to the Queanbeyan River. The Goulburn-Bombala railway passes from east to west through the north of the suburb. The suburb contains a small general shopping strip, consisting of several major brand outlets. Queanbeyan East Public School and Queanbeyan TAFE both reside in East Queanbeyan, as do a number of significant and popular
15807534
Dora Creek


Dora River is a watercourse that is located in the Upper Central Coast/Lower Hunter regions of New South Wales, Australia. Dora Creek River rises below Watagan Mountains west of Martinsville, and flows generally southeast by south, joined by two minor tributaries, before reaching its river mouth within Lake Macquarie, near the town of Dora Creek. The river descends over its course. The merged flows of Dora Creek together with Lake Macquarie reaches the Tasman Sea of the South Pacific Ocean at Swansea. The F3 Freeway crosses the creek,
2471331
River Continuum Concept


to be more predictable as to the biological properties of the water. The concept was first developed in 1980 by Robin L. Vannote, with fellow researchers at the Stroud Water Research Center. The River Continuum Concept is based on the idea that a watercourse is an open ecosystem that is in constant interaction with the bank, and moving from source to mouth, constantly changing. Basis for this change in the overall system is due to the gradual change of physical environmental conditions such as the width, depth, water, flow characteristics,
15291764
River Adur


the English Channel at Shoreham-by-Sea. The mouth of the Adur is now two miles (3 km) from the town centre of Shoreham due to longshore drift. The Baybridge Canal uses part of the Adur's watercourse. The name "Adur" is a relatively recent (probably 1612s) invention, based on the name of the Roman fort Portus Adurni which was mistakenly believed to be at Shoreham. The river had previously been known as the "Bramber", and was also recorded as the "Sore"
9660167
Klamath River


of beaver from 1915–1917 on High Prairie Creek at the mouth of the Klamath River near Requa, California. Within a matter of years, the plentiful beavers in the Klamath Basin had been mostly wiped out. Beaver dams had previously been an important factor in stream habitat in the Klamath River watershed, helping to moderate the power of floods and creating extensive wetlands. The loss of the beaver dams resulted in detrimental consequences for watercourses in the basin, exacerbating the power of winter floods, and causing severe erosion. Trapping parties eventually moved
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Oaks Estate, Australian Capital Territory


Oaks Estate is a township situated immediately on the northern side of the New South Wales - Australian Capital Territory border abutting the township of Queanbeyan in south-eastern New South Wales, Australia. The estate covers an area of approximately 40 hectares and is bound by the Molonglo River to the north, the Queanbeyan River to the east, 'The Oaks' to the west, and the Queanbeyan-Cooma railway to the south. Oaks Estate is located 12 kilometres from the centre of Canberra. The village is also noteworthy as the
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Queanbeyan River


minor irrigation requirements. A buttressed concrete gravity wall which was long, raised an extra to the height of in 1951-1952. The weir has had serious impacts on native fish migration in the Queanbeyan River. The Googong Dam is located upstream of the town of Queanbeyan. The dam was completed in 1979 and has a maximum carrying capacity of . The Commonwealth Government owns the dam, which is operated by ACTEW Corporation, the water utility provider, that is an ACT government-owned corporation. ACTEW also manages the dam foreshores
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Ordinary watercourse


An ordinary watercourse is one of the two types of watercourse in statutory language in England and Wales. Ordinary watercourses include every river, stream, ditch, drain, cut, dyke, sluice, sewer (other than a public sewer) and passage through which water flows and which does not form part of a main river. An internal drainage board where relevant, or lead local authority has permissive powers to carry out flood defence works for ordinary watercourses at their discretion. An ordinary watercourse is one of the two types of watercourse
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Cotter River


The Cotter River, a perennial river of the Murrumbidgee catchment within the Murray-Darling basin, is located in the Australian Capital Territory, Australia. The Cotter River, together with the Queanbeyan River, is one of two rivers that provides potable water to the Canberra and Queanbeyan region. The river rises on the eastern slopes of the Brindabella Ranges in the south-west of the Australian Capital Territory (ACT), within Namadgi National Park, and flows generally north, joined by six minor tributaries, including Paddys River, before
10415892
The Queanbeyan Age


The Queanbeyan Age is a weekly newspaper based in Queanbeyan, New South Wales, Australia. It has had a number of title changes throughout its publication history. First published on 15 September 1860 by John Gale and his brother, Peter Francis Gale, "The Golden Age", as it was known at the time, was the first newspaper of the small township on the banks of the Queanbeyan River. It was named due to the short-lived Kiandra goldrush, which generated large amounts of gold-based traffic through the
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Oaks Estate, Australian Capital Territory


and Queanbeyan Rivers. His station huts which he named ‘Queenbeeann’were located two kilometres downstream from the Molonglo/Queanbeyan River junction in what is today the abattoir paddock. The township of Queanbeyan was established in 1838 about south east of Oaks Estate. In 1877 John Bull, a farmer and grazier from Tarago NSW purchased from Charles Campbell, the son of Robert, 100 acres of land including the building known as ‘The Oaks’. He operated the inn as the ‘Elmsall Inn’. In the same year John Bull established
11317420
Queanbeyan River


. Lower flows in the river downstream of the dam since its construction, together with below average rainfall for the past decade, have modified the river channel and led to an increase in colonisation by willows and river plants which enjoy low flows. Management of the river includes eradication of these weeds. The Queanbeyan region is the traditional home of the Ngunnawal and the Ngarigo peoples. The first Europeans visitors to the area were led by Charles Throsby. While searching for the Murrumbidgee River in 1820, his party followed the course of the
6804801
Peter Pond


to its mouth; the watercourse, now called the Mackenzie River, did in fact flow to the Northwest Passage section of the Arctic Ocean. Peter Pond had contributed to the mapping of Canada by drawing the general outline of the river basin that Mackenzie recorded in 1789. The maps that Peter Pond subsequently drew, based on his explorations and on the information provided to him by First Nations peoples, ultimately gained international recognition for Pond at the end of the 18th century. In 1790, Pond sold his shares in the North West
13387093
Petite Rivière de Jacmel


The Petite Rivière de Jacmel is a watercourse running in Haiti through the Sud-Est department and the arrondissement of Jacmel. The Petite Rivière de Jacmel takes its source in the foothills of the mountain range called "Chaîne de la Selle", and set in Hispaniola's Tiburon Peninsula. Over approximately 10 kilometers long, the river then runs Eastwards, to meet South with the Caribbean Sea at the level of its mouth in the bay of the port-city of Jacmel. Along its path in the mountain, the river turns
2380076
Fort Kaskaskia State Historic Site


Lieutenant Governor. During much of the 19th century and especially after the American Civil War, the Mississippi River cut through many of its former oxbows and shortened its channel considerably. In 1881, during a flood, the moving water of the Mississippi "discovered" a much smaller, parallel riverbed, the mouth of the Kaskaskia. Kaskaskia's bed was a few feet lower than the Mississippi's bed, so the whole river shifted to the new watercourse, cutting across the head of a former oxbow to do so. For the
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Queanbeyan


proclaimed a township in 1838 when the population was about 50. The local parish was also known by that name and later still the member for the electorate of Queanbeyan held a seat in the legislative assembly of the colony of NSW. On 28 November 1837 the Colonial Secretary announced the appointment of Captain Alured Tasker Faunce as resident police magistrate at Queanbeyan. His homestead, called Dodsworth, was situated on the banks of the Queanbeyan river opposite the town. Traces of gold were discovered in 1851 and lead and silver mines also flourished briefly
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Queanbeyan River


, 1910, 1922, 1925, 1952, 1974, 1975 and 1976. A timeline compiled by a member of the Queanbeyan and District Historical Museum Society gives similar dates, extending to 2012. It is yet to be updated to record another 6-metre (19.7 feet) flood on 6 June 2016. During the 1976 flood the half completed Googong Dam was at risk of collapse under the weight of water behind it. In this eventuality low lying parts of Queanbeyan and Canberra would have been inundated. The Queanbeyan Cemetery was flooded,
6804803
Main river


Main rivers () are a statutory type of watercourse in England and Wales, usually larger streams and rivers, but also include some smaller watercourses. A main river is defined as a watercourse marked as such on a main river map, and can include any structure or appliance for controlling or regulating the flow of water in, into or out of a main river. The Environment Agency's powers to carry out flood defence works apply to main rivers only. In England main rivers are designated by Defra. The Welsh Government performs
11408337
2018 Nigeria Federation Cup


Supreme Court Final Table: Round 1 [Sep 24] Kwara United 5-1 Abia Warriors Kano Pillars 3-2 Rivers United Round 2 [Sep 26] Kano Pillars 1-2 Abia Warriors Rivers United 0-1 Kwara United Round 3 [Sep 28] Kano Pillars 2-1 Kwara United Rivers United 0-1 Abia Warriors Final Table: Round 1 [Sep 24] Akwa United 1-0 Wikki Tourists Nasarawa United 0-0 Kogi United Round 2 [Sep 26] Kogi United 0-1 Akwa
8216896
Molonglo River


The Molonglo River, a perennial river that is part of the Murrumbidgee catchment within the Murray–Darling basin, is located in the Monaro and Capital Country regions of New South Wales and the Australian Capital Territory, in Australia. The river rises on the western side of the Great Dividing Range, in Tallaganda State Forest at and flows generally from south to north before turning northwest, through Carwoola and the outskirts of Queanbeyan, where it has confluence with its major tributary, the Queanbeyan River, and then continues through Canberra, where
15421062
Ashley County, Arkansas


northwestern boundary of the county before emptying into the Ouachita River, which serves as the southwestern boundary. The Port of Crossett is positioned just south of the Saline River's mouth. Within the county, Bearhouse Creek, Chemin-a-haut Bayou, Fountain Creek, Flat Creek, Mill Creek, and Overflow Creek are important watercourses. Ashley County contains Overflow National Wildlife Refuge, part of the Felsenthal National Wildlife Refuge, and four Wildlife Management Areas (WMAs) under Arkansas Game and Fish Commission jurisdiction. Beryl Anthony Lower Ouachita
11853161
San Diego Creek


century, the watershed was used for agriculture. Increased runoff from farmlands resulted in extensive erosion, which led to the creation of a stream channel that ran northwestwards into the Santa Ana River channel and thence the Upper Newport Bay. As siltation problems plagued the bay, the Bitter Point Dam was constructed to divert the Santa Ana River to its present mouth at Huntington Beach, leaving the Cienega/San Diego Creek as the main watercourse flowing into the bay. To support irrigation, farmers drilled numerous wells to tap the region's abundant
17239627
Cotter River System


The Cotter River System (CRS) is located in the Australian Capital Territory and was constructed in 1912. A feature of the Namadgi National Park, the Cotter River System is one of two main sources for the Australian Capital Territory's water supply, the other being the Queanbeyan River located north of the Australian Capital Territory in New South Wales. Nevertheless, the Cotter River System is a larger catchment area and due to recent drought conditions the Queanbeyan River has been seen as obsolete in comparison. Comprising three primary dams, the Cotter
16407004
Oaks Estate, Australian Capital Territory


Hazelbrook Works, a wool washing works and fellmonger near the junction of the Queanbeyan and Molonglo rivers. In 1885 George Tompsitt bought Hazelbrook Works and renamed it the Hazelbrook Wool Scouring Works, Tannery and Wholesale Produce Warehouses. With a major business expansion Oaks Estate became the nucleus of Queanbeyan industry. The Queanbeyan Railway Station opened in September 1887 and the auction of the sale of the first residential allotments in Oaks Estate took place a few months later. In the early 1890s a local businessman established the Queanbeyan Roller Flour Mill in the Oaks
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Queanbeyan River


being overrun with carp and reeds. The Queanbeyan Council has put in place a resource development scheme to clean out the river, including a 'catch a carp' competition where the winners won $500 or fishing gear. European carp have not penetrated the river above Googong Dam, providing an excellent trout and native fish catchery in both the dam and the river upstream. Carp are present the entire length of the river, but in small quantities. Since construction of Googong Dam in 1979, the endangered Macquarie perch has been very
6804807
Internal drainage board


) of these rivers and watercourses is therefore an essential component of the whole life cycle of these watercourses. Accommodating sustainability within the design and maintenance process for lowland rivers and watercourses has to address three essential elements: Many IDBs are redesigning watercourses to create a two-stage or bermed channel. These have been extensively created in the Lindsey Marsh Drainage Board area of East Lincolnshire to accommodate the three elements of lowland watercourse sustainability. Berms are created at or near to the normal retained water level in the system. It is sometimes replanted
10718132
List of watercourses in the San Francisco Bay Area


numbered clockwise from Monticello Dam: Watercourses which feed into Suisun Bay and Grizzly Bay, listed clockwise from Benicia to Martinez: "For tributaries of the Sacramento and San Joaquin Rivers, see List of rivers in California." Watercourses which feed into the Carquinez Strait or San Pablo Bay between the Benicia-Martinez Bridge and Point San Pablo, numbered east to west: Watercourses which feed into the east shore of San Francisco Bay between Point San Pablo and the Bay Bridge, numbered north to south: Watercourses which feed into the east
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Monkey River


Monkey River is a coastal watercourse in southern Belize that rises in the Maya Mountains and discharges to the Caribbean Sea near Monkey River Town. One of Belize's major rivers, Monkey River has northern headwaters which originate in the Cockscomb Basin Wildlife Sanctuary, where the Swasey Branch drains the East Basin of that wildlife sanctuary. Further south, the Bladen Branch watercourse drains the eastern slopes of the Maya Mountains including the ancient Mayan settlement areas of Lubaantun and Nim Li Punit. These two watercourses join to form the Monkey River approximately 16 kilometres
2619521
Oshawa Creek


Oshawa Creek is a watercourse that flows from its headwaters in the Oak Ridges Moraine to its mouth on Lake Ontario, at Oshawa, Ontario. It drains a watershed of . In its lowest reaches, in Oshawa, two tributaries, Goodman's Creek and Montgomery Creek, join the watercourse. To the west it borders Lynde Creek, which also has its headwaters in the Oak Ridges Moraine, and the shorter watercourses Pringle Creek and Corbett Creek. Bowmanville Creek, to the east, also has its headwaters in the Oak Ridges Moraine
15142259
Maceió


international flights. The city is home to the Federal University of Alagoas. The name "Maceió" has origin in the term tupi maçayó or maçaio-k, that means "what it covers the swamp". The Aurélio Dictionary says that the term "maceió" means a temporary and cyclic lagoon that is located at the edge of the sea at the mouth of a watercourse small enough to be interrupted by a silicate bar until the high tide opens the way temporarily cyclically related to the season, river flow, lunar seasons
9117059
Karkheh River


that while the Karkheh flows a kilometre or two west of Susa, another major watercourse flows parallel to the Karkheh within a few kilometres "east" of Susa. When these rivers are in flood stage, the entire area south of Susa can be flooded, as the waters of the two watercourses mingle. The watercourse a kilometre or two east of Susa, now called the Shaur, flows east between the Haft Tepe and Shaur ridges into the Dez River, north of where the Dez and Karun rivers merge. At some previous
15088817
Canberra


and the Googong Dam on the Queanbeyan River. Although the Googong Dam is located in New South Wales, it is managed by the ACT government. ACTEW Corporation owns Canberra's two wastewater treatment plants, located at Fyshwick and on the lower reaches of the Molonglo River. Electricity for Canberra mainly comes from the national power grid through substations at Holt and Fyshwick (via Queanbeyan). Power was first supplied from a thermal plant built in 1913, near the Molonglo River, but this was finally closed in 1957. The ACT has
6793634
Land District of Queanbeyan


The Land District of Queanbeyan was one of the around 100 land districts of New South Wales which were introduced with the Crown Lands Act of 1884. It was based around the town of Queanbeyan, and included the area from near Lake George in the north, to Colinton in the south, and west to the Goodradigbee River and beyond it. In 1909, a large part of the district was transferred to the Commonwealth government to become the Australian Capital Territory. The district was located in the Eastern Division, and included land in
21988679
River Poddle


water diverted from the River Dodder at the great weir at Balrothery in Firhouse, and carried by the three-kilometre first section of the City Watercourse. The ancient artificial watercourse was made not later than the 1240s, with the sanction of the English administration in Ireland. The watercourse takes an interesting bend after it crosses under Wellington Lane. This looks like the reuse of an existing ditch around an earlier ecclesiastical site. Often roads follow the boundaries of such sites. This would be a rare example of a watercourse doing so.
11405304
Ishëm (river)


The Ishëm (or "Ishmi") is a river in western Albania, which brings water to the area north of the Albanian capital, Tirana. It forms part of a watercourse (Tiranë-Gjole-Ishëm), but only the lower third of the watercourse is known as the Ishëm. The Ishëm proper is formed at the confluence of the rivers Gjole and Zezë, a few km northwest of Fushë-Krujë. It flows into the Adriatic Sea near the town Ishëm. The length of the watercourse is recorded in
6555377
Nea-Nidelvvassdraget


Nea-Nidelvvassdraget is a watercourse in the municipalities of Tydal, Selbu, Klæbu, and Trondheim in Trøndelag county, Norway. The total area of the watershed is and it runs for about from the source in the Sylan mountains to its mouth in Trondheimsfjorden. Trondheim Energiverk has fourteen power stations along the water course which are highly regulated, with a total production (in 2004) of . Development of the area had already begun in 1890 with the development of the Øvre Leirfoss power station. Important rivers in the Nea-Nidelvvassdraget
1382567
Sully, Vale of Glamorgan


equivalent. It has been suggested that "Abersili" would be a more appropriate Welsh name, and an unofficial referendum has shown significant support for that view amongst residents. But it is unclear whether the name "Abersili" has ever been in common use; the earliest known example is by Iolo Morganwg, a notoriously untrustworthy source. Furthermore, "Abersili" means 'the mouth of the river Sili', but Sully Brook (assuming that that is the watercourse in question) does not reach the sea at Sully, but
16569567
Ordinary watercourse


have permissive power to carry out flood defence works at their discretion. This implies that a residual responsibility to maintain ordinary watercourses, and to report any issues with them to lead local flood authorities, (county councils or unitary authorities) rests in tort with riparian owners, that is owners of land adjoining such watercourses. Such watercourses were historically defined as non-navigable watercourses however their designation has changed to those watercourses not included on a 'main rivers map' and whose bed is not owned by an authority. Critical Ordinary Watercourses
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