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Quechee Gorge
The Quechee Gorge is located in Quechee, Vermont along U.S. Route 4. The gorge is 165 feet deep and is the deepest gorge in Vermont. It serves as a popular tourist attraction in Quechee State Park and can be viewed from the U.S. Route 4 bridge and from trails on both sides of the gorge. Many people from around New England flock to the gorge for the views. The Ottauquechee River flows through the bottom of the gorge and is a popular whitewater kayak run. Geology The gorge was carved approximately 13,000 years ago as the Laurentide Ice Sheet retreated across the region. The carving is thought to be a result of rapid downcutting of the Ottauquechee River after the drainage of glacial Lake Hitchcock Lake Hitchcock was a glacial lake that formed approximately 15,000 years ago in the late Pleistocene epoch. After the Laurentide Ice Sheet retreated, glacial ice melt accumulated at the terminal moraine and blocked up the Connecticut River, cre .... The gorge cuts through bedrock o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quechee Gorge, Vermont
Quechee is a census-designated place and one of five unincorporated villages in the town of Hartford, Windsor County, Vermont, United States. As of the 2010 census, the population of the CDP was 656. It is the site of Quechee Gorge on the Ottauquechee River and is also the home to the Quechee Lakes planned community, initiated in the late 1960s, which also brought to the community the small Quechee Lakes Ski Area in the 1970s. Quechee was known for a picturesque covered bridge at the site of the old Quechee mill, which now houses the Simon Pearce glass-blowing facility and restaurant. The bridge was severely damaged by flooding caused by Hurricane Irene in 2011. The bridge has since been rebuilt. Quechee has a small branch post office with zip code 05059. The region was historically inhabited by tribes of the Abenaki people; evidence exists of an ancient Abenaki village at the site of Quechee, in addition to more recent Abenaki settlements and activity throughout Hartford. G ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quechee, Vermont
Quechee is a census-designated place and one of five unincorporated villages in the town of Hartford, Windsor County, Vermont, United States. As of the 2010 census, the population of the CDP was 656. It is the site of Quechee Gorge on the Ottauquechee River and is also the home to the Quechee Lakes planned community, initiated in the late 1960s, which also brought to the community the small Quechee Lakes Ski Area in the 1970s. Quechee was known for a picturesque covered bridge at the site of the old Quechee mill, which now houses the Simon Pearce glass-blowing facility and restaurant. The bridge was severely damaged by flooding caused by Hurricane Irene in 2011. The bridge has since been rebuilt. Quechee has a small branch post office with zip code 05059. The region was historically inhabited by tribes of the Abenaki people; evidence exists of an ancient Abenaki village at the site of Quechee, in addition to more recent Abenaki settlements and activity throughout Hartford. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quechee State Park
The Quechee State Park is located on US Route 4 in Quechee, Vermont. The park land is owned by the US Army Corps of Engineers and leased from by the State of Vermont. The park contains the Quechee Gorge, a popular Vermont tourist stop. The land was originally the site of the Dewey wool mill which ceased operation in 1952 and relocated to Enfield, New Hampshire. Shortly after the closing of the Mill the US Army Corps of Engineers acquired the property as part of its regional flood control plan. A hydroelectric dam sits at the north end of the gorge. Activities include camping, hiking, swimming, river fishing, picnicking, wildlife watching and winter sports. Camping facilities include 45 tent/trailer sites and 7 lean-to sites, two bathrooms with showers and a sanitary dump station. There is also a large field and play area, a picnic area next to Quechee Gorge with a pit toilet and a hiking trail along the gorge. See also *List of Vermont state parks This is a list of state parks ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quechee Gorge Bridge
The Quechee Gorge Bridge is a historic bridge, carrying U.S. Route 4 (US 4) across Quechee Gorge, near the Quechee village of Hartford, Vermont. Built in 1911, it is Vermont's oldest surviving steel arch bridge. It was listed on the National Register of Historic Places in 1990. Description and history The Quechee Gorge Bridge is located on US 4, roughly midway between Woodstock and White River Junction, Vermont. It is set high above the Ottauquechee River near the southern end of Quechee Gorge, a major local tourist attraction that is part of Quechee State Park. It is a three-span steel deck truss structure, long, wide, and high carrying two lanes of traffic (one in each direction) and sidewalks on both sides. Its main span is a parabolic spandrel-braced Pratt truss, forming a span of . The arch is mounted on concrete footings, which are located near the stone abutments of the previous bridge. The bridge structure is built out of a series of panels and other stee ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ottauquechee River
The Ottauquechee River (pronounced ''AWT-ah-KWEE-chee'') is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed April 1, 2011 river in eastern Vermont in the United States. It is a tributary of the Connecticut River, which flows to Long Island Sound. The Ottauquechee rises in the Green Mountains in eastern Rutland County in the town of Killington, and flows generally eastwardly into Windsor County, where it passes through or along the boundaries of the towns of Bridgewater, Woodstock, Pomfret, Hartford and Hartland; and the villages of Woodstock and Quechee. It joins the Connecticut River in the town of Hartland, about 4 miles (6 km) south-southwest of White River Junction.DeLorme (1996). ''Vermont Atlas & Gazetteer''. Yarmouth, Maine: DeLorme. A headwaters tributary known as the North Branch Ottauquechee River flows southeastwardly through the towns of Killington and Bridgewater. Quechee State Park is located al ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Laurentide Ice Sheet
The Laurentide Ice Sheet was a massive sheet of ice that covered millions of square miles, including most of Canada and a large portion of the Northern United States, multiple times during the Quaternary glacial epochs, from 2.58 million years ago to the present. The last advance covered most of northern North America between c. 95,000 and c. 20,000 years before the present day and, among other geomorphological effects, gouged out the five Great Lakes and the hosts of smaller lakes of the Canadian Shield. These lakes extend from the eastern Northwest Territories, through most of northern Canada, and the upper Midwestern United States (Minnesota, Wisconsin, and Michigan) to the Finger Lakes, through Lake Champlain and Lake George areas of New York, across the northern Appalachians into and through all of New England and Nova Scotia. At times, the ice sheet's southern margin included the present-day sites of coastal towns of the Northeastern United States, and cities such as Bos ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Hitchcock
Lake Hitchcock was a glacial lake that formed approximately 15,000 years ago in the late Pleistocene epoch. After the Laurentide Ice Sheet retreated, glacial ice melt accumulated at the terminal moraine and blocked up the Connecticut River, creating the long, narrow lake. The lake existed for approximately 3,000 years, after which a combination of erosion and continuing geological changes likely caused it to drain. At its longest, Lake Hitchcock stretched from the moraine dam at present-day Rocky Hill, Connecticut, to St. Johnsbury, Vermont (about ). Although the rift valley through which the river flows above Rocky Hill actually continues south to New Haven, on Long Island Sound, the obstructing moraine at Rocky Hill diverted the river southeast to its present mouth at Old Saybrook. Lake Hitchcock is an important part of the geology of Connecticut. It experienced annual layering of sediments, or varves: silt and sand in the summertime (due to glacial meltwater) and clay in the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canyons And Gorges Of Vermont
A canyon (from ; archaic British English spelling: ''cañon''), or gorge, is a deep cleft between escarpments or cliffs resulting from weathering and the erosive activity of a river over geologic time scales. Rivers have a natural tendency to cut through underlying surfaces, eventually wearing away rock layers as sediments are removed downstream. A river bed will gradually reach a baseline elevation, which is the same elevation as the body of water into which the river drains. The processes of weathering and erosion will form canyons when the river's headwaters and estuary are at significantly different elevations, particularly through regions where softer rock layers are intermingled with harder layers more resistant to weathering. A canyon may also refer to a rift between two mountain peaks, such as those in ranges including the Rocky Mountains, the Alps, the Himalayas or the Andes. Usually, a river or stream carves out such splits between mountains. Examples of mountain-type c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Windsor County, Vermont
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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