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The Clyde River is a tributary of
Lake Memphremagog Lake Memphremagog (; french: Lac Memphrémagog) is a fresh water glacial lake located between Newport, Vermont, United States and Magog, Quebec, Canada. The lake spans both Quebec and Vermont, but is mostly in Quebec. Most of the watershed that ...
, over long, in northern
Vermont Vermont () is a state in the northeast New England region of the United States. Vermont is bordered by the states of Massachusetts to the south, New Hampshire to the east, and New York to the west, and the Canadian province of Quebec to ...
in the United States. It is the easternmost of the four major rivers in Orleans County. It is the most powerful of the four within Orleans County, powering several turbines at damsites. It is part of the
Northern Forest Canoe Trail The Northern Forest Canoe Trail (NFCT) is a marked canoeing trail in the northeastern United States and Canada, extending from Old Forge in the Adirondacks of New York to Fort Kent, Maine. Along the way, the trail also passes through the states ...
. It was named by one of the early surveyors from his partiality to a river of the same name in Scotland. The Route 105/114 junction to Clyde Road section of Clyde River in Vermont is long and is rated by American Whitewater as a class I-III section.


Geography

It drains the water from about . With the exception of three miles (5 km) of rapids near its mouth, this is a very sluggish stream, passing through in its course, several natural ponds of considerable size. Even during spring high water, there is barely a perceptible current.Trails
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Course

The river has its source in Spectacle Pond (length: ; altitude: ) in Brighton. The Southern part of Spectacle Pond is part of Brighton State Park. Spectacle Pond is actually a
kettle A kettle, sometimes called a tea kettle or teakettle, is a type of pot specialized for boiling water, commonly with a ''lid'', ''spout'', and ''handle'', or a small electric kitchen appliance of similar shape that functions in a self-contained ...
. It is only deep with a thick bottom of muck. From the mouth of Spectacle Pond, the Clyde river flows on as follows: Higher course of the river (segment of ) * toward Northwest up to East bank of Island Pond; * toward Northwest crossing the Island Pond (length: ; altitude: ) toward Island Pond up to the mouth of the pond * toward the Southwest crossing the city of Island Pond et passing at South of Bluff Mountain, up to the confluence of Pherrins River (coming from North). Pherrins River which is the main tributary of Clyde River, empties into the Clyde River from the north at below the outlet, frequently rises quite suddenly, swelling the waters of the latter so as to reverse its current and cause it to back up into Island Pond with great force for ten hours or more, until the pond is full, or the water subsides below, when it will again change and rush out.Gazetteer of Lamoille and Orleans Counties, VT.; 1883-1884, Compiled and Published by Hamilton Child; May 1887 Intermediary course of the river (segment of ) From the mouth of Pherrins River, the Clyde River flow as follow: * toward Southwest, up to Oswegatchie Pond (coming from South); * toward Northwest, snaking between Rosebrook Hill (located on South side) and Dollif Mountain (located on North side) up to the discharge of Mud Pounds (coming from North); * toward Northwest, up to the limit of Charleston; * toward Northwest in Charleston, up to the discharge (coming from North-East) of a lake; * toward Northwest, un to Lang Brook (coming from North); * toward North-West by passing an island at the end of this segment, up to Back Brook (coming from the South); * toward Northwest, up to Mad Brook (coming from South); * toward Northwest, passing at Northeast of Deer Hill (altitude of summit: ), up to the discharge (coming from North) of Lake Echo (altitude: ) and from Lake Seymour (altitude: ); the confluence of this discharge is located at the South of East Charleston village; * toward Northwest, splitting in two for bypassing an island (length: ), then snaking up to the discharge (coming from South) of Toad Pond; * (or in direct line) toward Northwest, up to South bank of Pensionner Pond. Lower course of the river (segment of ) * Northward crossing Pensioner Pond (altitude: ) up to the mouth where the lake is narrowing and curving to Northwest; * Northward up to the South bank of Charleston Pond; * Northward up to the dam at the mouth of Charleston Pond (altitude: ); * to Northwest up to South bank of a lake; * to Northwest up to the confluence of the lake which is linked to Lake Salem by a strait of ; * to Northwest crossing Lake Salem (altitude: ) up to the mouth; * Westward forming a curve to North, crossing the Interstate 91 and snaking up to the dam located at the Northeast end of Clyde Pond #1; * to Southwest, crossing Clyde Pond #1 (altitude: ), up to the dam on West bank of the pond; * to West up crossing the city of Newport up to the confluence at the South bank of the
Lake Memphremagog Lake Memphremagog (; french: Lac Memphrémagog) is a fresh water glacial lake located between Newport, Vermont, United States and Magog, Quebec, Canada. The lake spans both Quebec and Vermont, but is mostly in Quebec. Most of the watershed that ...
(altitude: ).


Charleston

The Clyde River is the largest in Charleston. It runs nearly through the center of the town. Some falls of importance are found on the stream, especially the Great Falls in the western part of the town, where the descent is more than in ; but its current is generally slow.


Derby

The Clyde River forms the principal water-course, flowing through the town from east to west. After exiting from Clyde Pond #1, it proceeds westward. It empties into Lake Salem from the south. It exits the northwest corner of this lake. It is then joined by an unnamed brook from Derby Pond from the north. It then empties into Clyde Pond #2 from the northeast. It exits this Pond west and into south Lake Memphremagog from the north. The mouth is just east of where US 5/Vermont 105 crosses Lake Memphremagog.


Natural history

Beavers Beavers are large, semiaquatic rodents in the genus ''Castor'' native to the temperate Northern Hemisphere. There are two extant species: the North American beaver (''Castor canadensis'') and the Eurasian beaver (''C. fiber''). Beavers a ...
populate the countryside and sometimes undercut the streamside
silver maple ''Acer saccharinum'', commonly known as silver maple, creek maple, silverleaf maple, soft maple, large maple, water maple, swamp maple, or white maple, is a species of maple native to the eastern and central United States and southeastern Canad ...
, toppling them into the water and creating logjams. The river winds through farm country, with silver maple and
alder Alders are trees comprising the genus ''Alnus'' in the birch family Betulaceae. The genus comprises about 35 species of monoecious trees and shrubs, a few reaching a large size, distributed throughout the north temperate zone with a few sp ...
dominating the shoreline. Northern white cedar, an occasional
willow Willows, also called sallows and osiers, from the genus ''Salix'', comprise around 400 speciesMabberley, D.J. 1997. The Plant Book, Cambridge University Press #2: Cambridge. of typically deciduous trees and shrubs, found primarily on moist so ...
, and a variety of shrubs line the wide waterway, and vegetation dips right into the water.


Geology

The river is in the Nulhegan Basin of northeastern Vermont.


History


Toponymy

The term "Clyde" is a popular first name with English origin. This term is also used as surname. This toponym was officialized on October 29, 1980 at Geographic Names Information System (GNIS) of US federal government.


Dams

In the early 19th century a mill dam constructed at Arnolds Falls. In 1883 a dam was constructed at the outlet to Lake Memphremagog. In 1918 the Newport Dam (Clyde Pond #2) was constructed. This dam was also known as Prouty Dam (after Governor Prouty). It was long. This was also known as the Clyde Pond dam. The Echo Lake dam is not used for hydroelectric power. Construction was completed in 1922. It has a normal surface area of . It is owned by Great Bay Hydro Corporation. The dam is concrete. The core is homogeneous concrete. The foundation is rock. The height is . Maximum discharge is per second. Its capacity is . Normal storage is . It drains an area of . In 1928 a dam was constructed at West Charleston. In 1929 a dam was built at Pensioner's Pond. In 1957 #11 Dam was constructed. It was located below the current hydro generation station off Clyde Street. In 1994 the #11 Dam was breached. In 1996 the #11 Dam was removed. In 2007 a fish (salmon) passage was built at the Newport Dam. Salmon fishing in Lake Memphremagog and the Clyde nearly stopped when the dam was constructed. It has improved since the dam's removal. The State of Vermont stocks the river with 30,000 salmon annually. 6,000 perish immediately from predators. Of those that make the journey to Lake Memphremagog, 18,000 return to spawn. The remainder assumed to be caught by fishermen.


Lists


Tributaries

The following dams are on tributaries (watershed) that feed into the Clyde, and not the Clyde itself: Lake Seymour is on a tributary which drains into Echo Lake, which in turn drains into the Clyde. It is not used for hydroelectric power. Construction of the original dam was completed in 1928. The lake has a normal surface area of . It is owned by Great Bay Hydro Corporation. This dam is stone, and concrete. The core is concrete. The foundation is soil. Its height is by long. Maximum discharge is per second. The capacity is . Normal storage is . It drains an area of .


List of cities and towns

In upstream order: * Newport, Vermont *
Derby, Vermont Derby is a town in Orleans County, Vermont, United States. The population was 4,579 at the 2020 census, making it the most populous community in Orleans County. The town contains four unincorporated villages: Beebe Plain, Clyde Pond, Lake Sa ...
* Charleston, Vermont **West Charleston (village) **East Charleston (village) *
Brighton, Vermont Brighton is a town in Essex County, Vermont, United States. The population was 1,157 at the 2020 census. The town was named "Gilead" in its original grant in 1780. The town was sold to a group consisting primarily of soldiers commanded by Colo ...
**
Island Pond, Vermont Island Pond is a census-designated place (CDP) in the town of Brighton in Essex County, Vermont, United States. The population was 750 at the 2020 census. It is part of the Berlin, NH–VT Micropolitan Statistical Area. Geography Islan ...


See also

* Pherrins River, Vermont *
Lake Memphremagog Lake Memphremagog (; french: Lac Memphrémagog) is a fresh water glacial lake located between Newport, Vermont, United States and Magog, Quebec, Canada. The lake spans both Quebec and Vermont, but is mostly in Quebec. Most of the watershed that ...
*
List of rivers of Vermont This is a list of rivers in the U.S. state of Vermont, sorted by drainage basin, and ordered from lower to higher, with the towns at their mouths: Connecticut River The Connecticut River flows south towards Long Island Sound in Connecticut ...


Footnotes


References and external links


Map of Clyde River
* {{authority control Rivers of Vermont Lake Memphremagog Derby, Vermont Charleston, Vermont Brighton, Vermont Island Pond, Vermont Newport (city), Vermont Northeast Kingdom, Vermont Bodies of water of Essex County, Vermont Rivers of Orleans County, Vermont Tributaries of the Saint Lawrence River Northern Forest Canoe Trail