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La Chute River


FieldValue
nameLa Chute River
image377 lachute river.jpg
image_captionThe river near Ticonderoga, New York
mapCarrillonAbercrombieRoute1758.png
map_captionFall River Route
pushpin_mapNew York Adirondack Park#USA
pushpin_map_captionLocation within New York
subdivision_type1Country
subdivision_name1United States
subdivision_type2State
subdivision_name2New York
subdivision_type3Region
subdivision_name3Adirondacks
subdivision_type4County
subdivision_name4Essex
subdivision_type5City
subdivision_name5Ticonderoga
length6 km
source1Lake George
source1_coordinates
source1_elevation318 ft
mouthLake Champlain
mouth_coordinates
mouth_elevation92 ft

between Lakes George and Champlain. (1758)

The La Chute River, also known as Ticonderoga Creek, is a short, fast-moving river, near the Vermont–New York border. It is now almost wholly contained within the municipality of Ticonderoga, New York, connecting the northern end and outlet of the 32 mi long Lake George and the southern end of the 172 km long Lake Champlain through many falls and rapids. The river drops about 230 feet (70 m) in its three and a half-mile (6 km) course, which is a larger drop than Niagara Falls (167 ft (52 m)).

Part of the Lake Champlain Valley and the St. Lawrence River drainage basin, ultimately its waters flow out of Lake Champlain through the 106 mi length of the Richelieu River into the St. Lawrence River and then into the North Atlantic Ocean north of Nova Scotia.

Geology and physiography

The Champlain Valley is among the northernmost valleys considered part of the Great Appalachian Valley, reaching from the province of Quebec, Canada somewhat northeast of Montreal at the outlet of the Richelieu River to Alabama. The Champlain Valley is a physiographic section of the larger Saint Lawrence Valley which in turn is part of the larger Appalachian physiographic division.

Lake Champlain is situated in the Champlain Valley between the Green Mountains of Vermont and the Adirondack Mountains of New York, and Lake George is located in the Adirondack Park and mountain range north of the lower Berkshire Hills arrayed to the south and east, which give land routes through the region accessibility into the Hudson River and Connecticut River drainage basins.

Footnotes

References

  1. {{cite gnis
  2. {{cite gnis
  3. "Lake Champlain | lake, Canada-United States | Britannica".
  4. "Physiographic divisions of the conterminous U. S.". U.S. Geological Survey.
Wikipedia Source

This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.

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