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Snake Mountain (Vermont)
Snake Mountain, also called Grand View Mountain, is an isolated mountain in the U.S. state of Vermont. The mountain straddles the Addison-Weybridge town line in Addison County. Most of the mountain, including the summit, is part of the Snake Mountain Wildlife Management Area (WMA) administered by the Vermont Fish & Wildlife Department. Adjacent to the WMA is the Wilmarth Woods Natural Area protected by The Nature Conservancy. Snake Mountain is one of a series of scattered hills extending into the Champlain Valley from the greater Taconic Mountains along Vermont's southwestern edge. Seen from the west, the prominent sheer cliffs of the mountain rise dramatically out of the valley making it easy to distinguish from other nearby hills and mountains. From the summit, there is an open vista of Lake Champlain and the Adirondack Mountains to the west. The view from the summit is sometimes called "Grand View.” History Over 400 million years ago, the Champlain thrust fault placed ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taconic Mountains
The Taconic Mountains or Taconic Range () are a range of the Appalachian Mountains, running along the eastern border of New York State and adjacent New England from northwest Connecticut to western Massachusetts, north to central western Vermont. A physiographic region of the larger New England province, the range includes notable summits, including its high point, Mount Equinox in Vermont, and Mount Greylock, the highest point in Massachusetts.''Day Hiker's Guide to Vermont'' 5th ed. (2006). Green Mountain Club: Waterbury Center, VermontRaymo, Chet and Raymo, Maureen E. (1989). ''Written in Stone: A Geologic History of the Northeastern United States.'' Chester, Connecticut: Globe Pequot.Doll, Charles G. Centennial Geologic Map of Vermont' (1961). United States Geological Survey: Washington The Taconics contain several hundred miles of trails, including sections of the Appalachian Trail, and over sixty designated areas of land protected by federal, state, county, and municipal, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Champlain Valley
The Champlain Valley is a region of the United States around Lake Champlain in Vermont and New York extending north slightly into Quebec, Canada. It is part of the St. Lawrence River drainage basin, drained northward by the Richelieu River into the St. Lawrence at Sorel-Tracy, Quebec (northeast of Montreal). The Richelieu valley is not generally referred to as part of the Champlain Valley. The Champlain Lake Valley is the most heavily populated region in Vermont, broadly stretching eastward from the lake's shore to the base of the Green Mountains. The state's largest city, Burlington, is located on the lake, and the city's associated suburban communities encompass part of the central section of the valley. Beyond urbanized Chittenden County, however, the valley's landscape is primarily open pasture and row crops, making the Champlain Valley the most productive agricultural region of Vermont. The New York portion of the Champlain Valley includes the eastern portions of Clinton ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains 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 (topography), 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 Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, 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 Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Green Mountain Club
The Green Mountain Club is a non-profit membership organization dedicated to preserving and protecting Vermont's Long Trail. The Long Trail is the oldest long-distance hiking trail in America and stretches from the Massachusetts state line to the Canada–United States border, along the main ridge of the Green Mountains. History Conceived on March 11, 1910, by James P. Taylor who was at the time the Assistant Headmaster of the Vermont Academy in Windsor, Vermont. Taylor lobbied other Vermont residents who shared his dream of a mission to "make the Vermont mountains play a larger part in the life of the people by protecting and maintaining the Long Trail system and fostering, through education, the stewardship of Vermont's hiking trails and mountains". In 1910, work began on the construction of America's first long-distance hiking path known as the Long Trail. The club completed the Long Trail in 1930. Today With 10,000 members, the club remains responsible for the trail, and is r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Vermont Route 17
Vermont Route 17 (VT 17) is a state highway in western Vermont in the United States. The western terminus of the route is at the New York state line in Addison, where it connects to New York State Route 185 (NY 185) by way of the Lake Champlain Bridge. Its eastern terminus is at a junction with VT 100 in Waitsfield. VT 17 was initially much shorter than it is today, extending from the Champlain Bridge to Addison upon assignment. It was extended east through the Green Mountains to Waitsfield in 1965. Route description The routing of VT 17 varies greatly on opposite sides of the Bristol town center. West of Bristol, the route passes through generally level terrain and connects multiple communities. East of Bristol, VT 17 is more mountainous and more rural in nature. West of Bristol VT 17 begins at the New York state line over Lake Champlain, where it connects to NY 185 at the midpoint of the Lake Champlain Bridge. The route ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Vermont
Lake Vermont, also called Glacial Lake Vermont, was a temporary lake created by the retreating glaciers during the close of the last ice age. The lake once included land in the Canadian province of Quebec and the American states Vermont and New York. It was a geographical predecessor of Lake Champlain. Once the glacier retreated far enough north, it drained into Glacial Lake Candona, the geologic predecessor of the St. Lawrence River. At one time, Lake Vermont may have reached nearly as far south as to what is now Albany, New York. The surface of the lake was about above present day Lake Champlain, and was up to deep. The lake contained muddy water, and the sediment of Lake Vermont contains silt/clay varves, with silt being deposited during summer and clay during the less-energetic flow of winter. The Laurentide Ice Sheet retreated north of what is now Burlington, Vermont, about 13,500 years ago, marking the beginning of Lake Vermont. The ice damming the water at the north ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Champlain Thrust
The Champlain Thrust is a 200-mile long fault (geology), fault extending from southern Quebec, down through western Vermont in the Champlain Valley, and into eastern New York (state), New York in the Catskill Mountains, Catskills/Hudson Valley. This east dipping thrust fault transports Cambrian-Ordovician passive margin shelf rocks westward by about and places them on top of Middle Ordovician rocks. The Middle Ordovician accretion of the one or more island arcs terranes drove the initial thrusting during the Taconic Orogeny, though reactivation of the fault may have occurred during the middle Devonian Acadian Orogeny.Rolf Stanley, The Champlain thrust fault, Lone Rock Point, Burlington, Vermont., Geological Society of America Centennial Field Guide--Northeast Section, 1987 The Champlain Thrust marks the most westerly thrust of the Taconic Orogeny. Prominent exposures The thrust fault is exposed to the north of the city of Burlington, Vermont on the shores of Lake Champlain at Lo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Adirondack Mountains
The Adirondack Mountains (; a-də-RÄN-dak) form a massif in northeastern New York with boundaries that correspond roughly to those of Adirondack Park. They cover about 5,000 square miles (13,000 km2). The mountains form a roughly circular dome, about in diameter and about high. The current relief owes much to glaciation. There are more than 200 lakes around the mountains, including Lake George, Lake Placid, and Lake Tear of the Clouds, which is the source of the Hudson River. The Adirondack Region is also home to hundreds of mountain summits, with some reaching heights of or more. Etymology The word Adirondack is thought to come from the Mohawk word ''ha-de-ron-dah'' meaning "eaters of trees". The earliest written use of the name was in 1635 by Harmen Meyndertsz Van Den Bogaert in his Mohawk to Dutch glossary, found in his ''Journey into Mohawk Country''. He spelled it Adirondakx and said that it stood for Frenchmen, meaning the Algonquians who allied with the Fre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Champlain
, native_name_lang = , image = Champlainmap.svg , caption = Lake Champlain-River Richelieu watershed , image_bathymetry = , caption_bathymetry = , location = New York/Vermont in the United States; and Quebec in Canada , coords = , type = , inflow = Otter Creek, Winooski River, Missisquoi River, Poultney River, Lamoille River, Ausable River, Chazy River, Boquet River, Saranac River, La Chute River , outflow = Richelieu River , catchment = , basin_countries = Canada, United States , length = , width = , area = , depth = , max-depth = , volume = , residence_time = 3.3 years , shore = , elevation = , islands = 80 ( Grand Isle, North Hero, Isle La Motte, '' see list'') , cities = Burlington, Vermont; Plattsburgh, New York Lake Champlain ( ; french: Lac Champlain) is a natural freshwater lake in North America. It mostly lies between the US states of New York and Vermont, but also extends north into the Canadian province of Quebec. The New York portion of the Ch ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
The Nature Conservancy
The Nature Conservancy (TNC) is a global environmental organization headquartered in Arlington, Virginia. it works via affiliates or branches in 79 countries and territories, as well as across every state in the US. Founded in 1951, The Nature Conservancy has over one million members globally , and has protected more than of land in its history. , it is the largest environmental non-profit organization by assets and revenue in the Americas. History The Nature Conservancy developed out of a scholarly organization initially known as the Ecological Society of America (ESA). The ESA was founded in 1915, and later formed a Committee on Preservation of Natural Areas for Ecological Study, headed by Victor Shelford.Our History ". The Nature Conservancy. nature.org. Retrieved December 18, 2016. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountains Of Vermont
This is a list of mountains in the U.S. state of Vermont. List Gallery Mount Mansfield photos File:Jericho & Mt Mansfield aerial 2019-04-06.jpg, Aerial eastward view from Jericho File:Mt mansfield 06212004.JPG, Top of Mount Mansfield facing west File:1chin.jpg, Eastward view of "The Chin" File:Mount Mansfield, Vermont - panoramio (6).jpg, View from the northeast File:4chin.jpg, Top of Mount Mansfield facing south Killington Peak photos File:Killington 1.jpg, Top of Killington facing north File:Killington 3.jpg, Top of Killington facing west File:Killington 2.jpg, Top of Killington facing west Camel's Hump Mountain Photos File:CamelsHumpMt 20150724.jpg, Eastward view of Camel's Hump Mountain from South Burlington File:CamelsHumpVT2012.jpg, Westward view of the summit File:CamelsHumpFromWest 20151019.jpg, View from the northwest Woodbury Mountain Photos File:Buffalo from Hardwick Farms Rd 229.jpg, View of Woodbury from Hardwick Farms Road facing WSW File:Buffalo from Moun ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taconic Orogeny
The Taconic orogeny was a mountain building period that ended 440 million years ago and affected most of modern-day New England. A great mountain chain formed from eastern Canada down through what is now the Piedmont of the East coast of the United States. As the mountain chain eroded in the Silurian and Devonian periods, sediments from the mountain chain spread throughout the present-day Appalachians and midcontinental North America. New England and Canada Beginning in Cambrian time, about 550 million years ago, the Iapetus Ocean began to close. The weight of accumulating sediments, in addition to compressional forces in the crust, forced the eastern edge of the North American continent to fold gradually downward. In this manner, shallow-water carbonate deposition that had persisted on the continental shelf margin through Late Cambrian into Early Ordovician time, gave way to fine-grained clastic deposition and deeper water conditions during the Middle Ordovician. In this period ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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