Appalachian Gap
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Appalachian Gap
The Appalachian Gap is a mountain pass in the Green Mountains of Vermont. The highest point of the pass is located in Chittenden County, about west of the boundary between Chittenden and Washington County. The pass is in the Camel's Hump State Park. On the east side, Appalachian Gap is drained by Mill Brook, which drains into the Mad River, the Winooski River, and into Lake Champlain. To the west, the gap is drained by Beaver Meadow Brook, which drains into the Huntington River, another tributary of the Winooski River. Lake Champlain drains into the Richelieu River in Quebec, thence into the Saint Lawrence River, and into the Gulf of Saint Lawrence. The Long Trail, a hiking trail running the length of Vermont, crosses Appalachian Gap between Stark Mountain to the south, and Baby Stark Mountain to the north. The Gap is a very popular route for tourists and affords excellent views of the Champlain Valley, Lake Champlain and the Adirondack Mountains. It is also a popular m ...
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Buels Gore, Vermont
Buels Gore is a gore in Chittenden County, Vermont, United States. The population was 29 at the 2020 census, down from 30 in 2010. In Vermont, gores and grants are unincorporated portions of a county which are not part of any town and have limited self-government (if any, as many are uninhabited). Geography Buels Gore is located at the southern tip of Chittenden County, bordered by the town of Huntington to the north, Fayston in Washington County to the east, and Starksboro in Addison County to the west. The crest of the Green Mountains, followed by the Long Trail, runs through the eastern side of the gore, and Vermont Route 17 crosses the gore from east to west, cresting the mountains at Appalachian Gap. According to the United States Census Bureau, Buels Gore has a total area of , of which , or 0.08%, is water. The name in history The gore was chartered by the Vermont General Assembly on November 4, 1780. It is named for Major Elias Buel (in some references "Buell") w ...
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Tributary
A tributary, or affluent, is a stream or river that flows into a larger stream or main stem (or parent) river or a lake. A tributary does not flow directly into a sea or ocean. Tributaries and the main stem river drain the surrounding drainage basin of its surface water and groundwater, leading the water out into an ocean. The Irtysh is a chief tributary of the Ob river and is also the longest tributary river in the world with a length of . The Madeira River is the largest tributary river by volume in the world with an average discharge of . A confluence, where two or more bodies of water meet, usually refers to the joining of tributaries. The opposite to a tributary is a distributary, a river or stream that branches off from and flows away from the main stream."opposite to a tributary"
PhysicalGeography.net, Michael Pidwir ...
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Mountain Passes Of Vermont
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ...
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Ski Area
A ski area is the terrain and supporting infrastructure where skiing and other snow sports take place. Such sports include alpine and cross-country skiing, snow boarding, tubing, sledding, etc. Ski areas may stand alone or be part of a ski resort. Scope of activities The US Forest Service defines a ski area as: "a site and associated facilities that has been primarily developed for alpine or Nordic skiing and other snow sports, but may also include, in appropriate circumstances, facilities necessary for other seasonal or year-round natural resource-based recreation activities, provided that a preponderance of revenue generated by the ski area derives from the sale of alpine and Nordic ski area passes and lift tickets, revenue from alpine, Nordic, and other snow sport instruction, and gross revenue from ancillary facilities that support alpine or Nordic skiing and other snow sports." Notable examples Ski areas can extend over several municipalities (ex: La Plagne in France, Alt ...
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Mad River Glen
Mad River Glen is a ski area in Fayston, Vermont. Located within the Green Mountain range, it sits in the Mad River Valley. Though not considered a large ski area, it has a vertical drop of , which ranks 14th in New England, and its terrain was ranked by ''Ski'' magazine as the most challenging on the east coast of the United States. Mad River Glen averages over of snow a year and maintains a traditional form of New England skiing that emphasizes snow preservation on narrow trails with little grooming instead of man-made snow on wide boulevards. It has one of only two single chairlifts left in the country and does not allow snowboarding. It is one of a very limited number of ski cooperatives. Individuals purchase publicly available shares and attend regular "Town Hall" meetings, voting on issues regarding the area and management of the cooperative. History Mad River Glen was founded in 1947 by Roland Palmedo who led a group of investors that included members of the Rocke ...
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