Missisquoi River [SEP] mouth of the watercourse
[{"answer": "Lake Champlain", "provenance": [{"wikipedia_id": "1997427", "title": "Missisquoi River", "start_paragraph_id": 1, "start_character": 0, "end_paragraph_id": 1, "end_character": 160, "bleu_score": 1.0, "meta": {}, "section": "Section::::Abstract."}]}]
North Yamaska River


reservoir, the North Yamaska flows: La Haute-Yamaska: Waterloo, Saint-Joachim-de-Shefford, Granby, and Saint-Alphonse-de-Granby; Brome-Missisquoi: Brigham. A multitude of creatures and plants of diverse shapes and sizes live within or depend on the North Yamaska river, these vary greatly from one season to the other. Because of its natural richness, the exploitation of this watercourse is common under commercial and recreational forms, in fact, its slow debit, the presence of many
17480486
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
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
15180333
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
Missisquoi River


South Branch join at Highwater, Quebec, just downriver from North Troy, Vermont. The river then runs in Quebec for approximately 15 miles (24 km), re-entering Vermont at Richford and thence to Lake Champlain's Missisquoi Bay. The name of the river is derived from an Algonquian Abenaki word "Masipskoik," meaning "[Place where there are] Large Rocks", referring to boulders found at the river's alluvial fan. . Alternative: Missisquoi Soil – Missisquoi is derived from the Abenaki word "masipskoik
19225415
Potton, Quebec


in Highwater with the South Branch of the Missisquoi River, forming the Missisquoi River which disembogues into Lake Champlain at Missisquoi Bay. The township is dotted with many mountains. Among the more prominent peaks are: Potton is well known for the many sugar bushes that produce maple syrup, considered among the most remarkable in the Quebec. Most of the bedrock underlying the township is Cambrian-era slate, schist, phyllite, greywacke and quartzite. There are bands of ultramafic rock near the Missisquoi River valley, and basalt also occurs.
2142570
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
9372594
Brattleboro, Vermont


called 'Wantastiquet' by the Abenaki people, a name meaning, according to various translations, "lost river", "river that leads to the west", or "river of the lonely way". Today known mostly by its English-translated name, the West River remains demarcated by New Hampshire's towering Mount Wantastiquet, rising 1,000 feet above water level directly opposite its mouth, and Lake Wantastiquet, near where it rises at its source. The Abenaki would transit this area annually between Missisquoi (their summer hunting
17167239
Missisquoi River


September 2008 the government of the United States approved a bill to study the Missisquoi and Trout rivers for potential designation as Wild and Scenic Rivers. It passed the House with bi-partisan support, and the rivers could potentially receive permanent protection in the National Wild and Scenic Rivers System. River sections being considered for Wild and Scenic designation are as follows: A Study Committee composed of local appointees and partner organizations has been evaluating the Wild and Scenic Designation of the upper Missisquoi and Trout rivers. The group's mission is to facilitate
19225420
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,
19632321
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
14223286
Missisquoi River Bridge


Historic Places in 1990. The Missisquoi River Bridge is located in northeastern Richford and southeastern Sutton, at a point where the Missisquoi River flows across the international border (an east-west line) in a roughly southwesterly direction. The bridge is just northwest of the small village of East Richford, with only Canada's Glen Sutton border station in the immediate vicinity north of the border. The bridge is a two-span metal Parker through truss structure, in length, and was assembled with riveted construction. The trusses rest on
524265
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
9690212
Missisquoi River


through Missisquoi National Wildlife Refuge in its lower 5 miles (8 km) before entering the south end of Missisquoi Bay, an arm of Lake Champlain that straddles the Canada-Vermont border. Named tributaries in Vermont are: Taft Brook in Westfield, Beetle Brook in Troy, Jay Brook in Jay, Stanhope Brook in Richford, the Trout River in Montgomery, Tyler Branch in Enosburg, Black Creek in Sheldon and Fairfield, and Hungerford Brook in Swanton and Highgate. The Abenaki people used the river as a canoe route between the
19225418
Missisquoi River


Lake Champlain drainage and the Saint-François River drainage. The river supports canoe traffic from Lake Champlain to Mansonville, Quebec, where there is a falls. From there, an ancient portage (carrying place) runs to Perkins Landing on Lake Memphremagog. Abenaki groups met seasonally on the bluffs at Eagle Point in Newport, Vermont, to catch and dry whitefish. The Missisquoi Valley was among the first areas of Southern Quebec's Eastern Townships to be taken by Loyalist refugees, who came upriver from camps on Missisquoi Bay. In
19225419
Missisquoi River Bridge


The Mississquoi River Bridge is a steel truss bridge, spanning the Missisquoi River between Richford, Vermont and Sutton, Quebec on the Canada–United States border. It connects Chemin de la Vallée Missisquoi in Sutton with Vermont Route 105A in Richford, between the border stations of the East Richford–Glen Sutton Border Crossing. The bridge was built by the state of Vermont in 1929, and is one of two in the state built by the Pittsburgh-Des Moines Steel Company. It was listed on the United States National Register of
524264
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
309139
Missisquoi Bay


Missisquoi Bay is a large extension in the northern part of Lake Champlain, at the East of the output of the latter in Richelieu River. It takes the form of a violin head, handle leaving the head of the lake and having about in diameter. The bay is divided between Quebec in Canada and Vermont in United States. The main town on its banks is Venise-en-Québec, a major summer resort. The river of the same name flows into the bay and the Missisquoi National Wildlife Refuge is located on
16987644
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
18069608
Central Vermont Railway


renamed the property the New England Central Railroad. RailTex was merged into RailAmerica in 2000. Genesee & Wyoming acquired RailAmerica at the end of 2012. Operations have continued to the present as before. This line was formed as the Missisquoi Railroad, then became the Missisquoi Valley Railroad, and then the Missisquoi Valley Division, before gaining its final name. Operations continued on the entire length until 1984, when a derailment on the bridge spanning the Missisquoi River near Sheldon, Vermont, forced the dismantlement of one of three spans. Operations
17329799
Missisquoi River


," which means “where there is flint” or “where flint is”. The name originates from an Abenaki chert quarry located near Missisquoi Bay on Lake Champlain. The South Branch of the Missisquoi rises in western Orleans County, Vermont, southwest of Lowell near Belvidere Mountain, then flows north past Troy and North Troy. It enters Quebec at Highwater, where it joins the North Branch. The North Branch of the Missisquoi rises in Lake Eastman, Quebec, and runs about through Eastman, Bolton Centre, East Bolton
19225416
Bridge 9 (Sheldon, Vermont)


Bridge 9 is a historic Parker through truss bridge, carrying Shawville Road across the Missisquoi River in Sheldon, Vermont. Built in 1928 after Vermont's devastating 1927 floods, it is one of the few surviving Parker truss bridges on the Missisquoi. It was listed on the National Register of Historic Places in 2007. Bridge 9 is located just northeast of the village of Sheldon Springs, carrying Shawville Road over the Missisquoi River between that village and the rural hamlet of Shawville. It is a single-span Parker through truss structure,
17721906
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
13244322
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
Jay Peak (Vermont)


part of the northern Green Mountains. The mountain is flanked to the southwest by Big Jay, and to the north by North Jay Peak (3,438 ft / 1,048 m). The mountain is in the watershed of the Missisquoi River, which drains into Lake Champlain, thence into Canada's Richelieu River, the Saint Lawrence River, and into the Gulf of Saint Lawrence. The south side of the mountain drains into Jay Brook, thence west into the Trout River and the Missisquoi River. The northwest side of the mountain drains
18653704
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
Simon Metcalfe


Surveyor in the Province of New York by 1770. In 1771, Governor Dunmore of New York granted of land to Simon Metcalfe and his wife. This land was called Prattsburgh and is now part of Swanton and Highgate in Vermont. His family settled on this land and he established a fur trading post at the mouth of the Missisquoi River. During the American Revolutionary War Metcalfe supported the American cause. He was taken prisoner by the British and held in Montreal. Three of his children were born in Montreal around 1777, 1779
11639215
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
16332847
Missisquoi County, Quebec


the northwest by Rouville County, and to the west by Iberville County and the Richelieu River (Saint-Jean County is on the other side of the river). The northernmost point of the county is at 45°21' N and 73° W and is also the junction of the borders of Missisquoi County, Rouville County and Iberville County. The westernmost point of the county is on the Richelieu River at the Canada–US border at 45° N and 73°20' W. The county is divided into four
2143153
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
10510129
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
14180440
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
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
15275387
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
Bridge 12


Bridge 12 is a historic Parker through truss bridge, carrying Boston Post Road across the Missisquoi River in Enosburg, Vermont. Built in 1929 in the wake of Vermont's devastating 1927 floods, it is one a shrinking number of surviving truss bridges on the river. It was listed on the National Register of Historic Places in 2007. Bridge 12 is located in a rural area of northern Enosburg, northeast of the village of Enosburgh Falls. It carries Boston Post Road (Town Highway 2) across the Missisquoi River, just south
17893921
Richford (CDP), Vermont


Richford is a census-designated place comprising the main settlement in the town of Richford, Franklin County, Vermont, United States. Its population was 1,361 as of the 2010 census, out of 2,308 people in the entire town of Richford. The Richford CDP is located in the northwest part of the town of Richford, along the Missisquoi River. Vermont Route 105 passes through the community, staying on the south side of the river; it leads east over the Green Mountains to North Troy and southwest down the Missisquoi River valley
8068250
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
Missisquoi Valley Rail Trail


from St. Albans City to Richford, passing through the towns of Swanton, Fairfield, Sheldon, Enosburg and Berkshire. The trail passes through forest, farmland and several villages, including Sheldon Springs, Sheldon Junction, Enosburg Falls, and East Berkshire. With a crushed limestone surface, it parallels the Missisquoi River along much of the eastern portion, and never exceeds a grade of three percent. The Central Vermont Railway's Richford Branch was built during the 1870s as the Missisquoi Railroad. In June 1984 a derailment damaged a bridge over
6914211
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
Vermont Route 105


in. The route runs southeast out of Sheldon Springs, paralleling the tracks, and crossing Missisquoi River. VT 105 reaches the hamlet of Sheldon Junction and an intersection with the eastern end of VT 78. Crossing through Sheldon Junction, the route makes a curve to the northeast again, paralleling the Missisquoi River. VT 105 becomes a rural roadway again, continuing near the river into a junction with VT 120 (Kane Road). VT 105 continues northeast along the riverside before beginning an eastbound wind through Sheldon. Passing an intersection
19413850
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
12430006
Abenaki


Vermont, with tribal headquarters in Brownington, and the Elnu Abenaki are located in southeastern Vermont with tribal headquarters in Jamaica, Vermont. The Elnu Abenaki tribe focuses mainly on carrying on the traditions of their ancestors through their children and teaching about their culture. The chief and political leader of the Nulhegan Band is Don Stevens. The Sokoki (the Abenaki Nation at Missisquoi) are located along the Missisquoi River in northwestern Vermont, with tribal headquarters in Swanton. Their traditional land is along the river, extending to its outlet at Lake
10281268
Missisquoi County, Quebec


fringes of the Appalachian foothills, giving it a rolling landscape on its eastern part. The western part of the county is situated on the Richelieu River plains. Missisquoi County is bound entirely on the south for 51 km by the Canada–US border (45° N) from 72°40.5' W to the middle of the Richelieu River (73°20.8' W), to the east by Brome County for 23 km along the meridian defined by 72°40.5' W, to the northeast by Brome County and
2143152
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
Richford, Vermont


, is to the east. Richford, the primary community, is in the northwest part of the town along the Missisquoi River. Vermont Route 105 passes through the center of town, leading east across the Green Mountains to North Troy and southwest to Enosburg Falls. Vermont Route 139 leads north from the center of Richford to the international border. According to the United States Census Bureau, the town has a total area of , of which is land and , or 0.61%, is water. The Missisquoi River enters from Canada
11202986
Central Vermont Railway


Though chartered as an independent entity in 1867, control of the Missisquoi Railroad was gained shortly thereafter, and it was formally leased in July 1873, providing a branch from St. Albans northeast to Richford, Vermont. It was operated until November 15, 1877, when the Connecticut and Passumpsic Rivers Railroad took it over. The company was reorganized in December 1886 as the Missisquoi Valley Railway, and was once again leased to the Central Vermont. The Montpelier and White River Railroad opened in 1876 and was leased to the Central Vermont,
17329791
Missisquoi River


The Missisquoi River is a tributary of Lake Champlain, approximately 80 mi (130 km) long, in northern Vermont in the United States and southern Quebec in Canada. It drains a rural area of the northern Green Mountains along the Canada–US border northeast of Lake Champlain, and an area of Quebec's Eastern Townships. The South Branch rises in Vermont and runs generally from southeast to northwest; the North Branch rises in Lake d'Argent in Eastman, Quebec, and runs from north to south. The North Branch and the
19225414
Highwater, Quebec


Highwater is a village in the Potton township of the Eastern Townships of Quebec, Canada, in Memphrémagog Regional County Municipality of the Estrie region, north of the Canada–United States border from North Troy, Vermont. The Portland-Montreal Pipe Line crosses the border and there is pumping station on the Highwater side . Highwater was the site of the Space Research Corporation test site. The confluence of the North Branch and the South Branch of the Missisquoi River is in Highwater; this forms the Missisquoi River which flows into Lake Champlain
20070531
Missisquoi River Bridge


state to be built by that firm. The bridge exhibits characteristics of standardized design developed by the state to speed construction of bridges at the time. The border crossing point was at the time economically important, providing access to the markets of southern Quebec to the industries in Richford. The bridge is currently closed and is being rehabilitated, with a re-opening date scheduled for 2018-10-16. The East Richford–Glen Sutton Border Crossing connects the towns of Sutton, Quebec and Richford, Vermont via the Missisquoi River
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Franklin, Vermont


, is water. Lake Carmi occupies the eastern part of the town, with Lake Carmi State Park on the southeast shore. The lake drains from its northeast end to the Pike River, which flows north and west through Quebec to Missisquoi Bay on Lake Champlain. The Rock River flows through the western part of the town, also to Missisquoi Bay. As of the census of 2000, there were 1,268 people, 429 households, and 343 families residing in the town. The population density was 32.8 people per square mile (
11144095
Bridge Number VT105-10


Bridge Number VT105-10 is a historic bridge, carrying Vermont Route 105 across the Missisquoi River in Sheldon, Vermont. Built in 1947 and rehabilitated in 1980, it is the state's oldest surviving four-span girder bridge. It was listed on the National Register of Historic Places in 2018. Bridge Number VT105-10 is located just west of the village of Sheldon Junction, which occupies a bend on the north side of Missisquoi River in central western Sheldon. Vermont Route 105, a major roadway that roughly parallels the
19884432
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
7024312
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
East Richford–Glen Sutton Border Crossing


bridge, built in 1926, was destroyed only a year later in the Great Vermont Flood of 1927. The US station is open 24 hours; the Canadian station is open daily from 8:00am to 4:00pm. The border crossing is set in a rural area, where the international boundary is a straight east-west line. The border is crossed by the Missisquoi River, which flows southwest from Quebec into Vermont. The actual crossing is on the Missisquoi River Bridge, a metal truss bridge built in 1929 after the previous bridge was
14938454
Douglas & Jarvis Patent Parabolic Truss Iron Bridge


The Douglas & Jarvis Patent Parabolic Truss Iron Bridge is a historic bridge across the Missisquoi River in Highgate, Vermont. Located at the end of Mill Hill Road, it is at one of the longest bridges of its type in the northeastern United States. It was built in 1887, and was listed on the National Register of Historic Places in 1974. The Douglas & Jarvis Patent Parabolic Truss Iron Bridge stands south of Highgate Falls village, at the end of Mill Hill Road, where it formerly crossed the Missisquoi River to meet
18784253
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
Brome—Missisquoi


, Iberville, Missisquoi and Saint-Jean ridings. The electoral district was abolished in 1966 when it was redistributed between Missisquoi and Saint-Jean ridings. In 1970, Missisquoi was renamed "Brome—Missisquoi". In 1976, "Brome—Missisquoi" was abolished and became part of a new "Missisquoi riding", which was renamed "Brome—Missisquoi" in 1983. The 2012 electoral redistribution saw this riding stay mostly the same, but it lost a small fraction of territory to Shefford. This riding has elected
17446716
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
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
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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
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
Missisquoi Bay


adopts the form "Missisquoi" to designate the county and the region. This is an in-ground by glaciers Bay ago years and then cast their monitoring dewatering of the Champlain Sea there are approximately years. The maximum depth of the bay is about 4.75 m and its bottom is made of regional marine deposits. The bay waters draining south into the Champlain Lake and the Richelieu River. Until the late 2000s, the water of the bay was stagnant and the bay was dying. At the opening of the new bridge on
16987646
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
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
11832706
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
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
15349528
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
Swanton (town), Vermont


in the north-central part of the town, and the community of Fonda is in the south-central part. Both communities are along US 7. A large portion of the Missisquoi National Wildlife Refuge, where the Missisquoi River enters Lake Champlain, is in the northwestern part of the town. As of the census of 2000, there were 6,203 people, 2,329 households, and 1,700 families residing in the town. The population density was 128.1 people per square mile (49.5/km). There were 2,689 housing units
17166984
Sheldrake River


these watercourses must meet standards that enable those uses. Class C watercourses also are suitable for primary and secondary contact recreation even though other factors may limit the use for that purpose. Water quality standards for Class C watercourses include limitations on fecal coliform, pH, total dissolved solids, and dissolved oxygen. Two principal tributaries enter the Mamaroneck River, one from the east and one from the west. The East Branch of the Mamaroneck River is the furthest upstream tributary along the Mamaroneck River and originates in north Harrison near the intersection of
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