Rideau River [SEP] mouth of the watercourse
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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
1652483
Ottawa


line, to be fully operational by early 2019. Ottawa is on the south bank of the Ottawa River and contains the mouths of the Rideau River and Rideau Canal. The older part of the city (including what remains of Bytown) is known as "Lower Town", and occupies an area between the canal and the rivers. Across the canal to the west lies "Centretown" and "Downtown Ottawa", which is the city's financial and commercial hub and home to the Parliament of Canada and numerous federal government
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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
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Kemptville Creek


, passes into North Grenville as it flows through the community of Bishop's Mills, before joining the main branch northeast of the community. Combined, the creek continues north through the community of Oxford Mills, where it goes over Oxford Mills Dam, flows under the Canadian Pacific Railway main line, heads through Kemptville, where it takes in the right tributary Barnes Creek, and reaches its mouth at the Rideau River. The Rideau River flows northward to the Ottawa River. The creek is navigable, for smaller watercraft, from the
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Peterson Creek (Cataraqui River)


Peterson Creek is a river in the Lake Ontario and Cataraqui River drainage basins in South Frontenac, Frontenac County and Rideau Lakes, Leeds and Grenville United Counties in eastern Ontario, Canada. It flows from Upper Peterson Lake to its mouth at Hart Lake. Peterson Creek begins at Upper Peterson Lake in South Frontenac township at an elevation of about north of the community of Keelerville. It flows northeast through Lower Peterson Lake to Gamble Bay on Crow Lake. The creek continues northeast through the lake into Rideau Lakes township and exits the lake
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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
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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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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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Little Cataraqui Creek


The Little Cataraqui Creek is a watercourse, much of which is a semi-urban wetland, that empties into Lake Ontario within the municipality of Kingston, Ontario, Canada. Further inland, just north of Highway 401, the creek has been dammed to form a reservoir that is part of the Little Cataraqui Creek Conservation Area. The adjective "little" distinguishes the creek from the (Greater) Cataraqui River 4.5 kilometers to the east, which forms the beginning of the Rideau Canal. Depending on the season, the creek is
18499309
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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Big Rideau Lake


heritage site in 2007. The primary inflow, at the southwest, is the Rideau River/Rideau Canal from Upper Rideau Lake via The Narrows channel and the Narrows lock and control structures. A second primary inflow is Black Creek at the west. The primary outflow, at the north, is also the Rideau River/Rideau Canal which leads via a channel to Lower Rideau Lake. The Rideau River and Canal flow to the Ottawa River and then to the Saint Lawrence River. The small community of Rideau Ferry is located at
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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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Rideau River


The Rideau River (), (Anishinàbemowin name: Pasapkedjinawong) is a river in Eastern Ontario, Canada. The river flows north from Upper Rideau Lake and empties into the Ottawa River at the Rideau Falls in Ottawa, Ontario. Its length is . The river was given the name "Rideau" (curtain) by Champlain, as he wrote in 1613, because of the appearance of the Rideau Falls. The Anishinàbemowin name for the river is "Pasapkedjinawong", meaning "the river that passes between the rocks."
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Ottawa


major rivers: the Ottawa River, the Gatineau River and the Rideau River. The Ottawa and Gatineau rivers were historically important in the logging and lumber industries and the Rideau as part of the Rideau Canal system for military, commercial and, subsequently, recreational purposes. The Rideau Canal (Rideau Waterway) first opened in 1832 and is long. It connects the Saint Lawrence River on Lake Ontario at Kingston to the Ottawa River near Parliament Hill. It was able to bypass the unnavigable sections of the Cataraqui and Rideau rivers and various
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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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Rideau Canal


The Rideau Canal, also known unofficially as the Rideau Waterway, connects Canada's capital city of Ottawa, Ontario, to Lake Ontario and the Saint Lawrence River at Kingston, Ontario. It is 202 kilometres in length. The name "Rideau", French for "curtain", is derived from the curtain-like appearance of the Rideau River's twin waterfalls where they join the Ottawa River. The canal system uses sections of two rivers, the Rideau and the Cataraqui, as well as several lakes. The Rideau Canal
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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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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
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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
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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
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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
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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
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Rideau Canoe Club


The Rideau Canoe Club (RCC) is a canoe club located on the Rideau River in Ottawa, Ontario, Canada. The club is located at Mooney's Bay, where the Rideau Canal splits away from the river prior to joining up with the Ottawa River. The club was founded in 1902 as the Rideau Aquatic Club with a clubhouse on the Rideau Canal near the Exhibition Grounds designed by Moses Chamberlain Edey in 1904-5. A memorial brass plaque on a flag pole is dedicated to the memory of the members who fell
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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
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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
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Upper Rideau Lake


Upper Rideau Lake is located in the municipality of Rideau Lakes, United Counties of Leeds and Grenville in Eastern Ontario, Canada. It is in the Saint Lawrence River Drainage Basin, and geographically the highest lake on the Rideau Canal System. Upper Rideau Lake is the summit of the Rideau Canal system, with a surface elevation of 124.65m above sea level. Despite having the highest elevation, Upper Rideau Lake is not the top of the watershed. Water flows north to the Rideau River, there is no flow south to the
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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
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Upper Rideau Lake


Cataraqui River. Inflow is from Westport Sand Lake, part of the Rideau Lake Subwatershed. Outflow, through the Narrows Lock, is to the Big Rideau Lake, which eventually flows to the Saint Lawrence River via the Ottawa River. The Rideau Lake Fault (an ancient fracture in the Earth's crust due to tension) explains the large exposure of granite that can be observed on much of Upper Rideau Lake's northern shore. The northern half of Upper Rideau Lake is located in the Algonquin Highlands. Bedrock in this hilly,
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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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Rideau Falls


The Rideau Falls are two waterfalls located in Ottawa, Ontario, Canada, where the Rideau River empties into the Ottawa River. The falls are divided by Green Island, with Ottawa's Old City Hall just to the south. To the west of the falls is the headquarters of the National Research Council while to the east are the Canada and the World Pavilion and the French Embassy. The falls were named by the early French for their resemblance to a curtain, or "rideau" in French. The Rideau River was later
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Rideau River


The Rideau Canal, which allows travel from Ottawa to the city of Kingston, Ontario on Lake Ontario, was formed by joining the Rideau River with the Cataraqui River. The river diverges from the Canal at Hog's Back Falls in Ottawa. In early spring, to reduce flooding on the lower section of the river, workers from the city of Ottawa use ice blasting to clear the ice which covers the river from Billings Bridge to Rideau Falls by cutting "keys" through the ice and using explosives to break off large sheets
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Jock River


municipality of Montague in Lanark County. It flows north under the Canadian Pacific Railway main line into the municipality of Beckwith, passes under Ontario Highway 15 and past the community of Franktown into the Goodwood Marsh. It then turns east into the City of Ottawa at the community of Ashton, flows through the community of Richmond, heads under Ontario Highway 416, and reaches its mouth at the Rideau river north of the community of Manotick. The Jock River watershed drains of land. For one weekend each spring, the popular Annual Jock
7911217
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
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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
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Kingston, Ontario


Kingston is a city in Eastern Ontario, Canada. It is on the eastern end of Lake Ontario, at the beginning of the St. Lawrence River and at the mouth of the Cataraqui River (south end of the Rideau Canal). The city is midway between Toronto, Ontario and Montreal, Quebec. The Thousand Islands tourist region is nearby to the east. Kingston is nicknamed the "Limestone City" because of the many heritage buildings constructed using local limestone. Growing European exploration in the 17th century and the desire for the
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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
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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
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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
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
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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
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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
History of Ottawa


of the early future town, and the Chaudière Falls (named by Champlain) in the west, which would later become employed in the lumber industry. Unlike some parts of Gatineau, and areas much further upstream, there are no indications of any settlement at all in present-day Ottawa for the next two centuries, however the river and the Rideau River had been used for travel. Chaudière was, and still is impassable by any water traffic, so there were portage paths around it on trips from the mouth of the
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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
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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
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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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Rideau View


Rideau View (also spelled Rideauview) is a sub-neighbourhood of Carleton Heights in River Ward, in the west-end of Ottawa, Ontario, Canada, located near the Rideau River. It is bordered by Meadowlands Drive to the south, Claymor Avenue to the west and Dynes Road to the north. Debra Avenue is the main road that runs through the neighbourhood and there is some residential housing on Eiffel Avenue. Some of parts of the neighbourhoods are east of Prince of Wales Drive and runs parallel along the Rideau River
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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
11832704
Capital Pathway


where the canal meets the Rideau river and the trail continues on its east side until Mooney's Bay Park. South of that it resumes, continuing to Ottawa's south boundary. This pathway is almost unknown by tourists but frequented by residents. It starts at Rideau Falls where the Rideau River meets the Ottawa River. It goes southward through New Edinburgh then along Riverside Drive until it reaches Billings Bridge. Here is a park where ducks frequent. From Billings Bridge, it continues south until it meets up with the Rideau Canal at
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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
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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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List of bridges in Ottawa


This is a list of bridges in the city of Ottawa, Ontario, Canada. They are listed from west to east for the Ottawa River or North to South for the Rideau River and Canal. Bridges spanning the Ottawa River from west to east: Bridges spanning the Rideau River from north to south: Bridges spanning the Rideau Canal from north to south: Bridges not spanning the above water courses: Eight bridges crossing the Jock River are not listed. The Sir George-Étienne Cartier Parkway has four bridges. From west to
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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
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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
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Tay Canal


army and a miller in Perth was awarded the contract to build the canal. The route would lead from Perth to the mouth of the Tay River. The locks were to be smaller than those on the Rideau, only , and a depth in the channel of . This was a less expensive option and it was felt that it would accommodate most of the commercial traffic of the day. By the end of 1834, five locks, six dams (with timber slides), two swing bridges and several embankments were built.
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Hog's Back Falls


The Hog's Back Falls, officially known as the Prince of Wales Falls, but rarely referred to by this name, are a series of artificial waterfalls on the Rideau River in Ottawa, Ontario, Canada. The falls are located just north of Mooney's Bay and the point where the Rideau Canal splits from the Rideau River. Prior to the construction of the Rideau Canal, these were a gentle set of rapids originally known as Three Rock Rapids. The name Hog's Back came into use shortly before canal construction. Civil
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Rideau Canal


3 metres wide on its Assiniboine River and Red River at The Forks. In response, the Rideau Canal was rebranded as "the world's largest skating rink". The Rideau Canal Skateway was added to the Guinness Book of World Records in 2005 for being the largest naturally frozen ice rink in the world. The Skateway is open 24 hours a day. The length of the season depends on the weather, but typically the Rideau Canal Skateway opens in January and closes in March. In 1971–1972, the Skateway's second winter
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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
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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
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Ottawa


small lakes along the waterway due to flooding techniques and the construction of 47 water transport locks.The Rideau River got its name from early French explorers who thought the waterfalls at the point where the Rideau River empties into the Ottawa River resembled a "curtain". Hence they began naming the falls and river "rideau" which is the French equivalent of the English word for curtain. During part of the winter season the Ottawa section of the canal forms the world's largest skating rink, thereby providing both a recreational venue and
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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
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Green Island (Rideau River)


Green Island in Ottawa, Ontario, Canada, is an island at the junction of the Rideau River, just off Sussex Drive in Ottawa at the Rideau Falls at the confluence with the Ottawa River. It is situated near the neighbourhood of New Edinburgh. To the west of the island is the National Research Council, and Global Affairs Canada (formerly Foreign Affairs, Trade and Development Canada); to the east is 24 Sussex Drive and the embassy of France. On either side of the falls are facilities for a hydroelectric power
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Ottawa Rowing Club


River between the University of Ottawa and McMaster University. From 1957 to 1972, the P.D. Ross Memorial trophy was awarded to the winner of the Club Eight (8+) event. Since 1998, the annual race is now between mixed women and men’s varsity and alumni crews from University of Ottawa and Carleton University either on the Rideau Canal or the Ottawa River. The third race is Head of the Rideau (distance of 5 km) which is held at the end of September on the Rideau River. At its first
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Hog's Back Falls


the Rideau River at that point by 12.5 metres (41 feet). To accommodate the natural flow of the Rideau River and to prevent damage from spring flooding, a large waste water weir was constructed. The water from this flows through a channel that was excavated in the eastern bank of the Rideau River. This created the Hogs Back Falls that we see today. The head of the original rapids is now buried beneath the canal dam, but the lower section of the rapids can still be seen today. This location marks
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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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Otter Lake (Rideau Lakes, Leeds and Grenville United Counties, Ontario)


Lake is not part of the Rideau Canal system. It is part of the Otter Creek / Hutton Creek Complex which is an area with a large north-eastern drainage pattern towards the mid-part of the Rideau River. The catchment area draining into the lake is about 36 square km and the shoreline length is about 20 km. The lake is 124 meters above mean sea level and is part of the Rideau River drainage basin. There are several parent streams flowing into Otter Lake and one primary outlet, which is Otter
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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
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Dutchy's Hole Park


Dutchy's Hole Park or Robinson Park is a park on the Rideau River in Ottawa, Ontario, Canada. It is part of the downtown Ottawa neighbourhood of Sandy Hill. The park has a wading pool, playground, and a football field, called Robinson Field. Pathways connect the park with Strathcona Park, the Rideau Campus of the University of Ottawa and via a former train bridge with "Parc Riverain"/River Road Park across the Rideau River in Vanier. The park includes a football field, called Robinsonfield, the Dutchie's Hole
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Sand Lake (Leeds and Grenville United Counties, Ontario)


the flowed through Morton Bay on its way to Lower Beverley Lake and from there to Gananoque. It was part of a native travel route that led from the Ottawa River, up the Rideau River, through the Rideau lakes and then to the St. Lawrence River at Gananoque. The lake was a bit smaller then than today, it was lower than it is today. The name, Sand Lake, first appears on an 1816 map of the Rideau waterway done by Lt. Joshua Jebb, Royal Engineer. In about 1820,
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Capital Pathway


the Hog's Back Falls. The more well known part is on the east side of the Rideau River. Besides the Rideau Canal Pathway, Ottawa River Pathway, and Rideau River Pathway, the following pathways are also part of the Capital Pathway in Ottawa: Aylmer is home to an effective and generally well-maintained network of bicycle paths that encircle the central portion of the area and run past many scenic locations, such as the Aylmer Marina and the Deschênes Rapids. The bike trail becomes very steep going northwards into Gatineau Park
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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
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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
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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
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Lower Town


Lower Town (also spelled "Lowertown" () is a neighbourhood in Rideau-Vanier Ward in central Ottawa, Ontario, Canada, to the east of downtown. It is the oldest part of the city. It is bounded by Rideau Street to the south, the Ottawa River to the west and north and the Rideau River to the east. It includes the commercial Byward Market area in the south-western part, and is predominantly residential in the north and east. It was historically French Canadian and Irish (as
14527333
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.
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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
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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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New Edinburgh


New Edinburgh is a neighbourhood in Rideau-Rockcliffe Ward, in Ottawa, Ontario, Canada. It is located to the northeast of the downtown core. It is bordered on the west by the Rideau River, to the north by the Ottawa River, to the south by Beechwood Avenue, and on the east by Princess Avenue, Lisgar Road, Rideau Terrace and Springfield Road. The area is an older, affluent neighbourhood. The Governor General of Canada's large residence and grounds are located in New Edinburgh, as is 24
3691096
Rideau Canal


Board at Jones Falls Lockstation commemorating Lieutenant Colonel John By, Royal Engineer, the superintending engineer in charge of the construction of the Rideau Canal. The plaque notes the Rideau Canal, built as a military route and incorporating 47 locks, 16 lakes, two rivers, and a , dam at Jones Falls (Jones Falls Dam), was completed in 1832. Other plaques to the canal erected by the Ontario Heritage Trust are at Kingston Mills, Smiths Falls, and Rideau Lakes. The of the Rideau Canal incorporate sections of the
380065
Watercourse


A watercourse is the channel that a flowing body of water follows. In the UK, some aspects of criminal law, such as The Rivers (Prevention of Pollution) Act 1951, specify that a watercourse includes those rivers which are dry for part of the year. In some jurisdictions, owners of land over which the water flows may have rights to some or much of the water in a legal sense. These include estuaries, rivers, streams, anabranches and canals. If it is navigable, it is also a "
16466851
Sandy Hill, Ottawa


Sandy Hill () is a neighbourhood in Ottawa, Ontario, located just east of downtown. The neighbourhood is bordered on the west by the Rideau Canal, and on the east by the Rideau River. To the north it stretches to Rideau Street and the Byward Market area while to the south it is bordered by the Queensway highway and Nicholas Street. The area is named for its hilliness, caused by the river, and its sandy soil, which makes it difficult to erect large buildings. It is home to a number
4609695
Naniken River


"lagoon" (also known as Crab Water or Raheny Lake) behind North Bull Island. The line of the Naniken from its mouth marks the boundary of the civil parish of Raheny with that of Clontarf, and the beginning of the Raheny portion of the Bull Island. As with many of Dublin's smaller watercourses, the upper and middle reaches of the Naniken were culverted over time, the covering of the stretch from Coolgariff Road to Kilmore Road being mentioned in parliamentary proceedings in 1960 by Neil Blaney, for example. There
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Česma


appears numerous springs, that in the dry part of the year losing water. It has a small drop (small difference in altitude between the source and the mouth) which was causing frequent floods before the regulation of the riverbed. The area around the watercourse of Česma till a hundred years ago was subject of flooding, which is why it was swampy. After that, Česma river and its tributaries was channelized, embankments were built for flood protection, and the soil is dried to obtain arable land as well as the fight
18242510
New Cut, Bristol


sections of the original course of the river Avon at either end, connecting Netham weir and Totterdown basin, and the Underfall sluices to the mouth of the Entrance lock at Cumberland Basin, the overall watercourse length is . No ships have navigated the cut on a regular basis since the 1930s, but it is still possible for boats to proceed as far as Netham weir with care. The Bristol Docks Company was formed to construct the Floating Harbour following the passage of an Act of Parliament in 1803, sponsored by the City Corporation and
2499853
Rideau Canal


Rideau and Cataraqui rivers, as well as several lakes, including the Lower, Upper and Big Rideau lakes. About of the route is man-made. Communities along the waterway include Ottawa, Manotick, Kars, Burritts Rapids, Merrickville, Smiths Falls, Rideau Ferry, Portland, Westport, Newboro, Seeleys Bay and Kingston. Communities connected by navigable waterways to the Rideau Canal include Kemptville and Perth. Since World War I and the construction of more extensive rail lines into rural Ontario, only pleasure craft make use of the
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