Giant Mountain Wilderness Area
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Giant Mountain Wilderness Area
The Giant Mountain Wilderness Area, an Adirondack Park unit of New York's Forest Preserve, lies in Essex County, New York, in the towns of Elizabethtown and Keene. It is roughly bounded by NY 9N on the north, NY 73 on the west and south and US 9 on the east. It includes two bodies of water covering , of trails, and a single lean-to. Geography The Giant Mountain Wilderness Area topography is steep and rocky with a considerable number of vertical or near vertical cliffs. Repeated landslides have occurred on the west side of Giant, exposing bare rock. Numerous small brooks cascade from the upper slopes. The tops of the higher mountains are bare rock but aspen, white birch, balsam and spruce are slowly filling in the upper slopes. From the eastern boundary of Route 9 several miles south of Elizabethtown to the top of Giant Mountain represents a horizontal distance of about , with an elevation change of nearly , the greatest elevation change per horizontal mile over that distanc ...
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Adirondack Park
The Adirondack Park is a part of New York's Forest Preserve in northeastern New York, United States. The park was established in 1892 for “the free use of all the people for their health and pleasure”, and for watershed protection. The park's boundary roughly corresponds with the Adirondack Mountains. Unlike most state parks, about 52 percent of the land is privately owned inholdings. State lands within the park are known as Forest Preserve. Land use on public and private lands in the park is regulated by the Adirondack Park Agency. This area contains 102 towns and villages, as well as numerous farms, businesses and an active timber-harvesting industry. The year-round population is 132,000, with 200,000 seasonal residents. The inclusion of human communities makes the park one of the great experiments in conservation in the industrialized world. The Forest Preserve was designated a National Historic Landmark in 1963. The park's include more than 10,000 lakes, 30,000 miles ...
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Lean-to
A lean-to is a type of simple structure originally added to an existing building with the rafters "leaning" against another wall. Free-standing lean-to structures are generally used as shelters. One traditional type of lean-to is known by its Finnish name . Lean-to buildings A lean-to is originally defined as a building in which the rafters lean against another building or wall, a penthouse. These structures frequently have skillion roofs and as such are sometimes referred to as "skillions". A lean-to shelter is a free-standing structure with only three walls and a single-pitched roof. The open side is commonly oriented away from the prevailing winds and rains. Often it is a rough structure made of logs or unfinished wood and used as a camping shelter. A lean-to addition is a shed with a sloping roof and three walls that abuts the wall of another structure. This form of lean-to is generally provisional; it is an appendix to an existing building constructed to fulfill a new need ...
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List Of Wilderness Areas In The Adirondack Park
The Adirondack Park is a part of New York's Forest Preserve in northeastern New York, United States. The park was established in 1892 for “the free use of all the people for their health and pleasure”, and for watershed protection. The park's boundary roughly corresponds with the Adirondack Mountains. Unlike most state parks, about 52 percent of the land is privately owned inholdings. State lands within the park are known as Forest Preserve. Land use on public and private lands in the park is regulated by the Adirondack Park Agency. This area contains 102 towns and villages, as well as numerous farms, businesses and an active timber-harvesting industry. The year-round population is 132,000, with 200,000 seasonal residents. The inclusion of human communities makes the park one of the great experiments in conservation in the industrialized world. The Forest Preserve was designated a National Historic Landmark in 1963. The park's include more than 10,000 lakes, 30,000 miles o ...
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Roaring Brook Falls (New York)
Roaring Brook Falls is a waterfall in the southwestern hills of Cheshire, Connecticut in the Northeastern United States. Formed as the eponymous Roaring Brook descends a wooded cliffside on West Mountain, the waterfall is an 80-foot horsetail and ranks as one of the tallest in the state. History and conservation Recovered arrowheads suggest that Algonquian Native Americans frequented the vicinity of Roaring Brook Falls prior to the arrival of settlers from the Connecticut Colony. Beginning as early as the 17th century, the surrounding landscape was clear-cut for agriculture and the falls were harnessed to power a stream-side mill. By the late 1800s, Roaring Brook Falls had become something of a local landmark with visitors from the nearby city of New Haven touring the area and enjoying the scenery. The property encompassing the waterfall was still privately owned in 1974 when concerned locals discovered that it might be sold for development. Significant efforts were launch ...
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Rocky Peak Ridge
Rocky Peak Ridge is the twentieth highest peak in the High Peaks Region of the Adirondack Park of New York, United States. The name of the mountain is due to its geology, a rocky ridge to the east of the better known Giant Mountain. The long, bare ridge is unusual in the Adirondacks; it resulted from the last great forest fire A wildfire, forest fire, bushfire, wildland fire or rural fire is an unplanned, uncontrolled and unpredictable fire in an area of Combustibility and flammability, combustible vegetation. Depending on the type of vegetation present, a wildfire ... in the region, in 1913.Goodwin, Tony, ed., ''Adirondack Trails, High Peaks Region'', Lake George, New York: Adirondack Mountain Club, 2004. Ascents There are two trails leading to the top of the peak. One trail, leaving from the town of New Russia, is about a ten-mile round trip with a few, steep rock scrambles along the way. The more commonly used trail splits from the Giant Mountain Trail at about 0.1 ...
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Giant Mountain
Giant Mountain is the twelfth-highest peak in the High Peaks Region of the Adirondack Park, in New York, USA. The peak is also known as "Giant of the Valley," due to its stature looking over Keene Valley and St. Huberts to the west. The prominent rock slides on the mountain's steep western face and its location away from most other large peaks make it quite an imposing figure, leading to its name. Ascents On 2 June 1797, Charles Broadhead and his survey party made the first recorded ascent of Giant Mountain, recorded as Giant-of-the-Valley. They were surveying the boundaries of the Old Military Tract.The Old Military Tract was created on 5 May 1786 to award land to New York veterans of the U.S. Revolutionary War, as a substitute for the original proposal to award lands in central New York. The land was in Clinton, Essex, and Franklin counties. Broadhead's was the first recorded ascent of any of the 46 Adirondack High Peaks. Trails There are three main trails up Giant, one ...
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Chapel Pond
A chapel is a Christian place of prayer and worship that is usually relatively small. The term has several meanings. Firstly, smaller spaces inside a church that have their own altar are often called chapels; the Lady chapel is a common type of these. Secondly, a chapel is a place of worship, sometimes non-denominational, that is part of a building or complex with some other main purpose, such as a school, college, hospital, palace or large aristocratic house, castle, barracks, prison, funeral home, cemetery, airport, or a military or commercial ship. Thirdly, chapels are small places of worship, built as satellite sites by a church or monastery, for example in remote areas; these are often called a chapel of ease. A feature of all these types is that often no clergy were permanently resident or specifically attached to the chapel. Finally, for historical reasons, ''chapel'' is also often the term used by independent or nonconformist denominations for their places of worshi ...
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Lake Marie Louise
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ice ...
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Washbowl On Giant Mountain
A bowl is a typically round dish or container generally used for preparing, serving, or consuming food. The interior of a bowl is characteristically shaped like a spherical cap, with the edges and the bottom forming a seamless curve. This makes bowls especially suited for holding liquids and loose food, as the contents of the bowl are naturally concentrated in its center by the force of gravity. The exterior of a bowl is most often round but can be of any shape, including rectangular. The size of bowls varies from small bowls used to hold a single serving of food to large bowls, such as punch bowls or salad bowls, that are often used to hold or store more than one portion of food. There is some overlap between bowls, cups, and plates. Very small bowls, such as the tea bowl, are often called cups, while plates with especially deep wells are often called bowls. In many cultures bowls are the most common kind of vessel used for serving and eating food. Historically small bowls w ...
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Ausable River (New York)
The Ausable River (), also known as AuSable River and originally written as "Au Sable", runs in the U.S. state of New York, from the Adirondack Mountains and past the village of Lake Placid and Au Sable Forks to empty into Lake Champlain (at ). It has an East and West branch that join at Au Sable Forks. The river forms a partial boundary between Clinton County and Essex County. The Ausable River is known for its gorge, Ausable Chasm, located a few miles east of Keeseville. The Ausable River is long and drains a watershed of . It was originally named "Au Sable" (French for "sandy") by Samuel de Champlain when he first explored the region in 1609 because of its extensive sandy delta. West Branch Ausable River The West Branch of the Ausable arises from the conjunction of the MacIntyre, South Meadow and Marcy Brooks, east of Mount Jo near the Adirondak Loj; it then runs northeast to Au Sable Forks (), and is fed by Lake Placid and the Chubb River along the ...
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New York State Route 73
New York State Route 73 (NY 73) is a state highway located entirely within Essex County, New York, in the United States. The highway begins at an intersection with NY 86 in the village of Lake Placid and ends at a junction with U.S. Route 9 (US 9) north of the hamlet of Underwood in the extreme southwestern corner of the town of Elizabethtown. NY 73 meanders through a mountainous region of Adirondack Park and passes by several named peaks, including Porter Mountain and Lower Wolfjaw Mountain. Along the way, the route has a short concurrency with NY 9N in the town of Keene. In the early 19th century, Lake Placid and Keene were connected by the North West Bay Road, an east–west highway linking Hopkinton to Westport. The highway was initially a crude, impassable road; however, it was significantly improved by the state of New York in the mid-1810s. A highway linking Keene to Underwood was constructed by 1846; at Underwood, the road connect ...
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