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Stony Clove Notch
Stony Clove Notch is a narrow pass, roughly 2,220 feet (677 m) in elevation located in the Town of Hunter in Greene County, New York, deep in the Catskill Mountains. It is traversed by New York State Route 214, although in the past the Ulster and Delaware Railroad went through it as well. The notch divides Hunter and Plateau mountains. There is just enough room for the road, and the steep, soaring slopes of both mountains are some of the Catskills' most striking scenery, with landslides and rocky cliffs visible. It sits at one end of the range of mountains known as the Devil's Path, and early visitors found it a terrifying place to visit. Today it is a popular destination not only for tourists in the region but for outdoor recreationists as well. One of the Catskills' major hiking trails crosses the road near the notch, and ice climbers and snowboarders have lately been attracted to the cliffs and slopes in winter. History Natural origins Stony Clove Notch was created ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Notch Lake
Notch Lake is an artificial lake in Edgewood, New York, in the Town of Hunter in the Catskill Mountains. It is located near the Stony Clove Notch, and is located near the edge of the Devil's Tombstone Campsite, bordering New York State Route 214. There is also a parking lot near the shore. It is the beginning of the Stony Clove Creek. One thing unusual about it is that it is one of the few places in the Catskills where there is a patch of Boreal Forest Taiga (; rus, тайга́, p=tɐjˈɡa; relates to Mongolic and Turkic languages), generally referred to in North America as a boreal forest or snow forest, is a biome characterized by coniferous forests consisting mostly of pines, spruc ... growing below 3,000 feet above sea level. A fire occurred near the northern shore in the 1990s. Camping is not allowed at the day-use area next to the parking lot and Pond, however, camping is allowed a short walk South along Route 214 at the Devil's Tombstone Campground. Refer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stony Clove And Catskill Mountain Railroad
The Ulster and Delaware Railroad (U&D) was a railroad located in the state of New York. It was often advertised as "The Only All-Rail Route to the Catskill Mountains." At its greatest extent, the U&D extended from Kingston Point on the Hudson River through the Catskill Mountains to its western terminus at Oneonta, passing through the counties of Ulster, Delaware, Schoharie and Otsego. History Rondout and Oswego Railroad During the early 19th century, waterways formed the principal transportation network in New York. An important point on this network was Rondout. Located at the confluence of Rondout Creek and the Hudson River, in 1828 it became the eastern terminus of the Delaware and Hudson Canal. Here, cargo and passengers were transferred from canal boats to the larger vessels navigating the Hudson. By the end of the Civil War, railroads were pre-empting waterways as the preferred method of transportation. Thomas Cornell, founder of the Cornell Steamboat Company and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tanning (leather)
Tanning is the process of treating Skinning, skins and Hide (skin), hides of animals to produce leather. A tannery is the place where the skins are processed. Tanning hide into leather involves a process which permanently alters the protein structure of skin, making it more durable and less susceptible to decomposition and coloring. Before tanning, the skins are dehaired, degreased, desalted and soaked in water over a period of six hours to two days. Historically this process was considered a noxious or "odoriferous trade" and relegated to the outskirts of town. Historically, tanning used tannin, an acidic chemical compound from which the tanning process draws its name, derived from the bark of certain trees. An alternative method, developed in the 1800s, is chrome tanning, where chromium salts are used instead of natural tannins. History The English word for tanning is from medieval Latin , derivative of (oak bark), from French (tanbark), from old-Cornish (red oak). ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
West Kill Mountain
West Kill Mountain, or Westkill Mountain, is located in Greene County, New York. The mountain is named after the West Kill stream which flows along its northern side, and is part of the Devil's Path range of the Catskill Mountains. To the east, West Kill Mountain faces Southwest Hunter Mountain across Diamond Notch; to the west, West Kill faces North Dome across Mink Hollow. West Kill Mountain stands within the watershed of the Hudson River, which drains into New York Bay. The north slopes drain into the West Kill, thence into Schoharie Creek, the Mohawk River, and the Hudson River. The southeast slopes of the mountain drain into Hollow Tree Brook, thence into Stony Clove Creek, Esopus Creek, and the Hudson River. The southwest slopes of West Kill Mountain drain into the Broadstreet Hollow stream, thence into Esopus Creek. West Kill Mountain is contained within the Westkill Mountain Wilderness Area of New York's Catskill State Park. See also * List of mountains in N ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Diamond Notch
Diamond Notch is a wind gap located between West Kill Mountain and Southwest Hunter Mountain in the Catskills of New York. The south side of Diamond Notch drains through Diamond Notch Hollow via Hollow Tree Brook to Stony Clove Creek, thence to Esopus Creek and the Hudson River. Water from the north side also reaches the Hudson, but via a longer route—first the West Kill, then Schoharie Creek to the Mohawk Mohawk may refer to: Related to Native Americans *Mohawk people, an indigenous people of North America (Canada and New York) *Mohawk language, the language spoken by the Mohawk people *Mohawk hairstyle, from a hairstyle once thought to have been t ..., the Hudson's largest tributary. References {{Gaps of the Appalachian Mountains Mountain passes of New York (state) Climbing areas of the United States Catskills Landforms of Greene County, New York Wind gaps of New York (state) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alf Evers
Alf Evers (February 2, 1905 – December 29, 2004) was an American historian who lived in Ulster County, New York for much of his life and wrote lengthy, definitive histories of the Catskills and Woodstock, serving the latter as town historian. At the time of his death his history of Kingston was nearly complete and awaited publication. Biography Evers was born in the Bronx neighborhood of Williamsbridge and lived there till the age of nine, when his parents moved to a farm near Tillson. He developed a passion for history from the many stories of the farmhands, the work of British naturalist Gilbert White and collecting Native American arrowheads with one of his high school teachers in New Paltz. He attended Hamilton College and, after graduation, returned to the city and the Art Students League, where he met his wife, illustrator Helen Baker. They eventually settled in Litchfield, Connecticut, where they wrote and illustrated 50 children's books together, most telling fa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Charles Lanman
Charles Lanman (June 14, 1819 - March 4, 1895) was an American author, government official, artist, librarian, and explorer. Biography Charles Lanman was born in Monroe, Michigan, on June 14, 1819, the son of Charles James Lanman, and the grandson of United States Senator James Lanman. Lanman's early life included newspaper work as editor of the Monroe Gazette in 1845, associate editor of the Cincinnati Chronicle in 1846, and member of the editorial staff of the New York Express in 1847. He spent ten years, from 1835 to 1845, studying with Hudson River School artists in New York City, where he met many artists, including Washington Irving. Lanman studied art under Asher B. Durand and at 28 became an elected associate of the National Academy of Design in 1846. Lanman's career included service as librarian for the U.S. War Department (1849-1850), private secretary to Senator Daniel Webster (1850-1853), librarian and the head of the returns office in the U.S. Interior Depar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
File (formation)
A file is a military term for a number of troops drawn up in line ahead, i.e. one behind the other in a column. The number of files is the measure of the width of a column of troops in several ranks one behind the other.McNab, p. 55.Schwartz, p. 9 Usage Files are useful when troops don't know where the enemy is, since there are overlapping fields of fire from each soldier, and cover from a possible flanking attack. Files are at a disadvantage when there are heavy weapons nearby, supported by infantry, especially machine guns and tanks. Ancient Greek use A file of men in the Greek phalanx was called a lochos A ''lochos'', plural ''lochoi'' ( el, λόχος ''lokhos'', pl. ''lokhoi''), is a tactical sub unit of Classical Greece and of the modern Greek army. The term derived from the ancient Greek for ambush and the men carrying out the ambush, but in p ... () and usually ranged from eight to sixteen men.''Royal military panorama'', p. 149. References Bibliography * * Dup ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Erosion
Erosion is the action of surface processes (such as water flow or wind) that removes soil, rock, or dissolved material from one location on the Earth's crust, and then transports it to another location where it is deposited. Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as ''physical'' or ''mechanical'' erosion; this contrasts with ''chemical'' erosion, where soil or rock material is removed from an area by dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres. Agents of erosion include rainfall; bedrock wear in rivers; coastal erosion by the sea and waves; glacial plucking, abrasion, and scour; areal flooding; wind abrasion; groundwater processes; and mass movement processes in steep landscapes like landslides and debris flows. The rates at which such processes act control how fast a surface is eroded. Typically, physical erosion procee ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
