Southwest Hunter Mountain
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Southwest Hunter Mountain
Southwest Hunter Mountain (Leavitt Peak) is a subpeak of Hunter Mountain, located in Greene County, New York. It is considered one of the Catskills' High Peaks in its own right, because of its separation from the main summit, and its topographic prominence. Hunter Mountain is named after John Hunter, who also gave his name to the town of Hunter. Southwest Hunter is part of the Devil's Path range of the Catskill Mountains. SW Hunter is flanked to the northeast by the main summit of Hunter, and to the west faces West Kill Mountain across Diamond Notch. It is considered a bushwhack, as there are no official trails leading to its summit, in the midst of a dense montane boreal forest of red spruce and balsam fir. Attempts to climb from Diamond Notch, the closest approach of a maintained trail, have led to the creation of a maze of herd paths on the level area west of the mountain's summit, none of which leads to it and many of which dead-end. Hikers have instead been following t ...
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Key Col
In topography, prominence (also referred to as autonomous height, relative height, and shoulder drop in US English, and drop or relative height in British English) measures the height of a mountain or hill's summit relative to the lowest contour line encircling it but containing no higher summit within it. It is a measure of the independence of a summit. A peak's ''key col'' (the highest col surrounding the peak) is a unique point on this contour line and the ''parent peak'' is some higher mountain, selected according to various criteria. Definitions The prominence of a peak may be defined as the least drop in height necessary in order to get from the summit to any higher terrain. This can be calculated for a given peak in the following way: for every path connecting the peak to higher terrain, find the lowest point on the path; the ''key col'' (or ''key saddle'', or ''linking col'', or ''link'') is defined as the highest of these points, along all connecting paths; the prom ...
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Desire Path
A desire path (often referred to as a desire line in transportation planning), also known as a game trail, social trail, fishermen trail, herd path, cow path, elephant path, goat track, pig trail, use trail and bootleg trail, is an unplanned small trail created as a consequence of mechanical erosion caused by human or animal traffic. The path usually represents the shortest or the most easily navigated route between an origin and destination, and the width and severity of its surface erosion are often indicators of the traffic level it receives. Desire paths typically emerge as convenient shortcuts where more deliberately constructed paths take a longer or more circuitous route, have gaps, or are non-existent. Once someone has already treaded out a path through the natural vegetation, subsequent traffics tend to follow that visibly existing route (as it is more convenient than carving out a new path by oneself), and the repeated trampling will further erode away both the remaini ...
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Catskill Park
The Catskill Park is in the Catskill Mountains in New York in the United States. It consists of of land inside a Blue Line in four counties: Delaware, Greene, Sullivan, and Ulster. As of 2005, or 41 percent of the land within, is owned by the state as part of the Forest Preserve; it is managed by the Department of Environmental Conservation (DEC). Another 5% is owned by New York City to protect four of the city's reservoirs in the region that lie partially within the park and their respective watersheds. There are bobcats, minks and fishers in the preserve, and coyotes are often heard. There are some 400 black bears living in the region. The state operates numerous campgrounds and there are over of multi-use trails. Hunting is permitted, in season, in much of the park. It has approximately 50,000 permanent residents, bolstered somewhat by second-home ownership on weekends and in the summer, and attracts about half a million visitors every year. The park is governed by ...
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Hunter Mountain Wild Forest
Hunting is the human activity, human practice of seeking, pursuing, capturing, or killing wildlife or feral animals. The most common reasons for humans to hunt are to harvest food (i.e. meat) and useful animal products (fur/hide (skin), hide, bone/tusks, horn (anatomy), horn/antler, etc.), for recreation/taxidermy (see trophy hunting), to remove predators dangerous to humans or domestic animals (e.g. wolf hunting), to pest control, eliminate pest (organism), pests and nuisance animals that damage crops/livestock/poultry or zoonosis, spread diseases (see varmint hunting, varminting), for trade/tourism (see safari), or for conservation biology, ecological conservation against overpopulation and invasive species. Recreationally hunted species are generally referred to as the ''game (food), game'', and are usually mammals and birds. A person participating in a hunt is a hunter or (less commonly) huntsman; a natural area used for hunting is called a game reserve; an experienced hun ...
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Esopus Creek
Esopus Creek is a tributary of the Hudson River that drains the east-central Catskill Mountains in the U.S. state of New York. From its source at Winnisook Lake on the slopes of Slide Mountain, the Catskills' highest peak, it flows across Ulster County to the Hudson at Saugerties. Many tributaries extend its watershed into neighboring Greene County and a small portion of Delaware County. Midway along its length, it is impounded at Olive Bridge to create Ashokan Reservoir, the first of several built in the Catskills as part of New York City's water supply system. Its own flow is supplemented above the reservoir by the Shandaken Tunnel, which carries water from the city's Schoharie Reservoir into the creek. The creek, originally known by the Native Americans in the area as ''Atkarkaton'' or ''Atkankarten'' and by Dutch settlers as the "Esopus Kill", takes its name from the Esopus tribe of the Lenape, who were living around the lower Esopus when the Dutch first explored ...
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Stony Clove Creek
Stony Clove Creek is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed October 3, 2011 creek in the Catskill Mountains in New York. It is a tributary of Esopus Creek, which in turn is a tributary of the Hudson River. It joins the Esopus in the village of Phoenicia, and has two smaller tributaries up north of Phoenicia. Description The Stony Clove starts near the Stony Clove Notch in Edgewood in Greene County. It originates at Notch Lake, near the Devil's Tombstone Campsite, and flows through the small villages of Edgewood and Lanesville, entering Ulster County at Chichester. History Early maps and deeds indicate that the Stony Clove flowed into the Warner Bushkill, or alternatively named, the Barber Bushkill, before flowing into the Esopus. Later cartographers have changed the nomenclature of the streams so that the Barber Bushkill or Warner Bushkill flows into the Stony Clove. It was formed about 10,000 years ago, d ...
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Mohawk River
The Mohawk River is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed October 3, 2011 river in the U.S. state of New York. It is the largest tributary of the Hudson River. The Mohawk flows into the Hudson in Cohoes, New York, a few miles north of the city of Albany.Mohawk River
, The Columbia Gazetteer of North America
The river is named for the of the Iroquois Confederacy. It is a major waterway in north-central New York. The largest tributary, the Schoharie Creek, accounts fo ...
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Schoharie Creek
Schoharie Creek is a river in New York that flows north from the foot of Indian Head Mountain in the Catskills through the Schoharie Valley to the Mohawk River. It is twice impounded north of Prattsville to create New York City's Schoharie Reservoir and the Blenheim-Gilboa Power Project. During the American Revolutionary War, Iroquois Indian attacks against the cluster of farms in the valley of the Cobleskill Creek tributary was the site of the Cobleskill Massacre (May 1778), virtually depopulating settlements in the southern Mohawk valley. News of this and two other mixed Tory-Indian guerrilla attacks led to an appropriation of funds for the Sullivan Expedition dispatched by General Washington in 1779 to break the threat of Indian raids. The Erie Canal crossed over the creek by an aqueduct at Schoharie Crossing State Historic Site. Two notable bridge collapses have occurred on Schoharie Creek. In 1987, two spans of the New York State Thruway collapsed. On August 28, 20 ...
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West Kill
The West Kill, an tributary of Schoharie Creek, flows through the town of Lexington, New York, United States, from its source on Hunter Mountain, the second-highest peak of the Catskill Mountains. Ultimately its waters reach the Hudson River via the Mohawk. Since it drains into the Schoharie upstream of Schoharie Reservoir, it is part of the New York City water supply system. It lends its name to both a mountain to its south and a small town midway along its length. The West Kill's watershed accounts for 10 percent of the reservoir's basin. It has the highest elevations and steepest slopes of any of the Schoharie's subwatersheds, with runoff from seven of the 35 Catskill High Peaks draining into the stream. Due to limited development and extensive land protection in the stream's watershed, its water is relatively clean, supporting a habitat for both wild and stocked trout; historically it has drawn fly fishers and other anglers. However, the West Kill has contributed to t ...
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Headwaters
The headwaters of a river or stream is the farthest place in that river or stream from its estuary or downstream confluence with another river, as measured along the course of the river. It is also known as a river's source. Definition The United States Geological Survey (USGS) states that a river's "length may be considered to be the distance from the mouth to the most distant headwater source (irrespective of stream name), or from the mouth to the headwaters of the stream commonly known as the source stream". As an example of the second definition above, the USGS at times considers the Missouri River as a tributary of the Mississippi River. But it also follows the first definition above (along with virtually all other geographic authorities and publications) in using the combined Missouri—lower Mississippi length figure in lists of lengths of rivers around the world. Most rivers have numerous tributaries and change names often; it is customary to regard the longest t ...
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New York Bay
New York Bay is the large tidal body of water in the New York–New Jersey Harbor Estuary where the Hudson River, Raritan River, and Arthur Kill empty into the Atlantic Ocean between Sandy Hook and Rockaway Point. Geography New York Bay is usually divided into two major components, which are connected by the Narrows. They are Upper New York Bay and Lower New York Bay. The term New York Harbor usually refers to Upper New York Bay and the surrounding Port of New York and New Jersey, but sometimes is taken to be a synonym for New York Bay. Upper New York Bay includes several islands. Liberty Island is the location of the Statue of Liberty. Nearby Ellis Island is known as a former immigration station. Governors Island is a former military base, now a park and historic site. Robbins Reef Light is also in the upper bay. Lower New York Bay includes Hoffman Island and nearby Swinburne Island. Both are artificial islands that are closed to the public. History Commissioned by King Fr ...
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Hudson River
The Hudson River is a river that flows from north to south primarily through eastern New York. It originates in the Adirondack Mountains of Upstate New York and flows southward through the Hudson Valley to the New York Harbor between New York City and Jersey City, eventually draining into the Atlantic Ocean at Lower New York Bay. The river serves as a political boundary between the states of New Jersey and New York at its southern end. Farther north, it marks local boundaries between several New York counties. The lower half of the river is a tidal estuary, deeper than the body of water into which it flows, occupying the Hudson Fjord, an inlet which formed during the most recent period of North American glaciation, estimated at 26,000 to 13,300 years ago. Even as far north as the city of Troy, the flow of the river changes direction with the tides. The Hudson River runs through the Munsee, Lenape, Mohican, Mohawk, and Haudenosaunee homelands. Prior to European ...
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