Slide Mountain Wilderness Area
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Slide Mountain Wilderness Area
The Slide Mountain Wilderness Area is, at , the largest tract of state-owned Forest Preserve in New York's Catskill Park, and the largest area under any kind of wilderness area protection between the Adirondacks and the southern Appalachians. It is located in the towns of Shandaken, Denning and Olive in Ulster County. Location Within those three towns, the Slide Wilderness might be better described as contained within the lands bounded on the north roughly by Esopus Creek and Route 28, the east by Ulster County Route 42 (known in different towns as Sundown Road or Peekamoose Road) almost to the shores of Ashokan Reservoir, the west by Ulster County Route 47, and on the south by Sugarloaf Road and Red Hill Road. The area's wilderness character is buffered not only by restrictive local zoning and conservation of neighboring private lands but also by bordering on two other large state-owned tracts, the Big Indian- Beaver Kill Wilderness Area to the west and the Sundown Wild ...
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Ulster County, New York
Ulster County is a county in the U.S. state of New York. It is situated along the Hudson River. As of the 2020 census, the population was 181,851. The county seat is Kingston. The county is named after the Irish province of Ulster. History Founding and formation When part of the New Netherland colony, Dutch traders first called the area of present-day Ulster County "Esopus", a name borrowed for convenience from a locality on the opposite side of the Hudson. The local Lenape indigenous people called themselves Waranawanka, but soon came to be known to the Dutch as the "Esopus Indians" because they were encountered around the settlement known as Esopus. In 1652, Thomas Chambers, a freeholder from the Manor of Rensselaerswyck, purchased land at Esopus. He and several others actually settled and began farming by June, 1653. The settlements grew into the village of Wiltwijck, which the English later named Kingston. In 1683, the Duke of York created 12 counties in his province, ...
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Beaver Kill
The Beaver Kill, sometimes written as the Beaverkill or Beaverkill River, is a tributary of the East Branch Delaware River, a main tributary of the Delaware River, approximately long, in the U.S. state of New York (state), New York. The Kill (body of water), kill drains a Baldigo, Barry; ; United States Geological Survey; 1999, p. 7. area of the Catskill Mountains and has long been celebrated as one of the most famous trout streams in the United States. Its preservation helped establish many of the basic conservation principles of rivers in the United States. The river has been popular as a trout stream since the early 19th century, when it became one of the first resort destinations in the United States. The subsequent depletion of the brook trout population by the 1850s led to an early conservation movement to preserve the river, including the introduction of hatcheries for brown trout. Its popularity as a trout stream arises in part from the many cold springs and deep pools in ...
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Delaware River
The Delaware River is a major river in the Mid-Atlantic (United States), Mid-Atlantic region of the United States. From the meeting of its branches in Hancock (village), New York, Hancock, New York, the river flows for along the borders of New York (state), New York, Pennsylvania, New Jersey, and Delaware, before emptying into Delaware Bay. It is the longest free-flowing river in the Eastern United States. The river has been recognized by the National Wildlife Federation as one of the country's Great Waters. The river's drainage basin, watershed drains an area of and provides drinking water for 17 million people. The river has two branches that rise in the Catskill Mountains of New York: the West Branch Delaware River, West Branch at Mount Jefferson (New York), Mount Jefferson in Jefferson, New York, Jefferson, Schoharie County, New York, Schoharie County, and the East Branch Delaware River, East Branch at Grand Gorge, New York, Grand Gorge, Delaware County, New York, ...
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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 Pidwirny & S ...
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Neversink River
The Neversink River (also called Neversink Creek in its upper course) is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed April 1, 2011 tributary of the Delaware River in southeastern New York (state), New York in the United States. The name of the river comes from the corruption of an Algonquin language, Algonquian language phrase meaning "mad river." The Neversink River is considered by many to be the birthplace of American dry fly fishing.Askins, Justin. ''The Legendary Neversink: A Treasury of the Best Writing About One of America's Great Trout Rivers'', Skyhorse Publishing, 2007, page xv Course The Neversink's main flow begins just south of the border between present-day Ulster County, New York, Ulster and Sullivan County, New York, Sullivan County (United States), counties, where the east and west branches of the river join near the hamlet (place), hamlet of Claryville, New York, Claryville. Both branches begin o ...
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Stream
A stream is a continuous body of water, body of surface water Current (stream), flowing within the stream bed, bed and bank (geography), banks of a channel (geography), channel. Depending on its location or certain characteristics, a stream may be referred to by a variety of local or regional names. Long large streams are usually called rivers, while smaller, less voluminous and more intermittent river, intermittent streams are known as streamlets, brooks or creeks. The flow of a stream is controlled by three inputs – surface runoff (from precipitation or meltwater), daylighting (streams), daylighted subterranean river, subterranean water, and surfaced groundwater (Spring (hydrology), spring water). The surface and subterranean water are highly variable between periods of rainfall. Groundwater, on the other hand, has a relatively constant input and is controlled more by long-term patterns of precipitation. The stream encompasses surface, subsurface and groundwater fluxes th ...
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Rocky Mountain (New York)
Rocky Mountain is a mountain located in Ulster County, New York. The mountain is part of the Catskill Mountains. Rocky Mountain is flanked to the west by Lone Mountain, and to the northeast by Balsam Cap. The south and east sides of Rocky Mountain drain into the headwaters of Rondout Creek, thence into the Hudson River, and into New York Bay. The northeast and northwest sides of Rocky Mtn. drain into the East Branch of the Neversink River, the Delaware River, and into Delaware Bay. Rocky Mountain is one of the 35 peaks in the Catskills greater than 3,500 feet elevation, and is a required ascent for membership in the Catskill Mountain 3500 Club. The ascent involvebushwhackingas there is no trail to the summit. Rocky Mountain is within the Slide Mountain Wilderness of New York's Catskill State Park. See also * List of mountains in New York There are three major mountain ranges in New York: the Adirondack Mountains, the Catskill Mountains, and part of the Appalachian ...
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Slide Mountain (New York)
Slide Mountain is the highest peak in the Catskill Mountains of the U.S. state of New York. It is located in the town of Shandaken in Ulster County. While the contour line on topographic maps is generally accepted as its height, the exact elevation of the summit has never been officially determined by the U.S. Coast and Geodetic Survey, and many informal surveys suggest the mountain may actually top 4,200 feet (1,280 m) above sea level. While it was not identified as the range's highest peak until the late 19th century, it has played a prominent role in Catskill history. Renowned naturalist John Burroughs wrote memorably of his climbs up Slide, and it helped get the Catskills added to New York's Forest Preserve. Bicknell's thrush was first identified on its summit. Geography Like most other Catskill peaks, Slide's summit is gentle and rounded, taking the form of a narrow ridge that rises to a wider bump on its eastern end. From there the mountain slopes down steeply to the c ...
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Catskill Mountains
The Catskill Mountains, also known as the Catskills, are a physiographic province of the larger Appalachian Mountains, located in southeastern New York. As a cultural and geographic region, the Catskills are generally defined as those areas close to or within the borders of the Catskill Park, a forest preserve protected from many forms of development under New York state law. Geologically, the Catskills are a mature dissected plateau, a flat region subsequently uplifted and eroded into sharp relief by watercourses. The Catskills form the northeastern end of the Allegheny Plateau (also known as the Appalachian Plateau). The Catskills were named by early Dutch settlers. They are well known in American society as the setting for films and works of art, including many 19th-century Hudson River School paintings, as well as for being a favored destination for vacationers from New York City in the mid-20th century. The region's many large resorts gave many young stand-up comedian ...
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Catskill High Peaks
The Catskill High Peaks are all of the mountains in New York's Catskill Mountains above in elevation whose summits are separated either by ''or'' a vertical drop of at least between it and the next nearest separate summit. By usual standards, these mountains are rather low and rounded, and mostly covered by vegetation. Unlike the Adirondack High Peaks, those in the Catskills are more evenly distributed around the eastern half of the range instead of being confined to one small area. All except Bearpen and Vly lie within the Catskill Park Blue Line. The 3500s The elevation was chosen in the early 1950s when Dan Smiley, a descendant of the founders of Mohonk Mountain House and his fellow birders were trying to find the elusive Bicknell's thrush, which prefers to nest and breed in the boreal forests that predominate above that elevation in the Catskills. They drew up a list nearly identical to the one below and published it in a naturalists' journal. A decade later hikers ...
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Leather
Leather is a strong, flexible and durable material obtained from the tanning, or chemical treatment, of animal skins and hides to prevent decay. The most common leathers come from cattle, sheep, goats, equine animals, buffalo, pigs and hogs, and aquatic animals such as seals and alligators. Leather can be used to make a variety of items, including clothing, footwear, handbags, furniture, tools and sports equipment, and lasts for decades. Leather making has been practiced for more than 7,000 years and the leading producers of leather today are China and India. Animal rights groups claim that modern commercial leather making and the consumption of its products is unethically killing animals. According to the life-cycle assessment (LCA) report for the United Nations Industrial Development Organization, 99% of the raw hides and skins used in the production of leather derive from animals raised for meat and/or dairy production. Critics of tanneries claim that they engage in uns ...
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Hemlock Bark
Tanbark is the bark of certain species of trees, traditionally used for tanning hides into leather. The words "tannin", "tanning", "tan," and " tawny" are derived from the Medieval Latin ''tannare'', "to convert into leather." Bark mills are horse- or oxen-driven or water-powered edge mills and were used in earlier times to shred the tanbark to derive tannins for the leather industry. A "barker" was a person who stripped bark from trees to supply bark mills. Tanbark around the world In Europe, oak is a common source of tanbark. Quercitannic acid is the chief constituent found in oak barks. The bark is taken from young branches and twigs in oak coppices and can be up to 4 mm thick; it is grayish-brown on the outside and brownish-red on the inner surface. In some areas of the United States, such as northern California, "mulch" is often called tanbark, even by manufacturers and distributors. In these areas, the word "mulch" may refer to peat moss or to very fine tanbark. I ...
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