Balsam Lake Mountain
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Balsam Lake Mountain
Balsam Lake Mountain is one of the Catskill Mountains, located in the Town of Hardenburgh, New York, United States. It is the westernmost of the range's 35 High Peaks. Its exact height has not been determined, but the highest contour line on topographic maps, , is usually given as its elevation. Located within the Balsam Lake Mountain Wild Forest management unit of the Catskill Park Forest Preserve, in the late 19th century its summit became the site of the first fire lookout tower in the state, operated by members of a nearby sportsmen's club. It was later taken over by the state's conservation agencies, which built several improved towers on the site, one of which remains, along with its accessory buildings and has been listed on the National Register of Historic Places, although it has not been used for fire detection since 1988. The summit is also the site of a rare sphagnum bog that has been affected by acid rain since a mid-20th century windstorm blew down many of 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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Sphagnum
''Sphagnum'' is a genus of approximately 380 accepted species of mosses, commonly known as sphagnum moss, peat moss, also bog moss and quacker moss (although that term is also sometimes used for peat). Accumulations of ''Sphagnum'' can store water, since both living and dead plants can hold large quantities of water inside their cells; plants may hold 16 to 26 times as much water as their dry weight, depending on the species.Bold, H. C. 1967. Morphology of Plants. second ed. Harper and Row, New York. p. 225-229. The empty cells help retain water in drier conditions. As sphagnum moss grows, it can slowly spread into drier conditions, forming larger mires, both raised bogs and blanket bogs. Thus, sphagnum can influence the composition of such habitats, with some describing sphagnum as 'habitat manipulators'. These peat accumulations then provide habitat for a wide array of peatland plants, including sedges and Calcifuges, ericaceous shrubs, as well as orchids and carnivorous plant ...
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Drainage Basin
A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the '' drainage divide'', made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide. In a closed drainage basin, or endorheic basin, the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, a dry lake, or a point where surface water is lost underground. Drainage basins are similar ...
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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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Balsam Lake Mountain Map
Balsam is the resinous exudate (or sap) which forms on certain kinds of trees and shrubs. Balsam (from Latin balsamum "gum of the balsam tree", ultimately from Semitic, Aramaic ''busma'', Arabic ''balsam'' and Hebrew ''basam'', "spice", "perfume") owes its name to the biblical Balm of Gilead. Chemistry Balsam is a solution of plant-specific resins in plant-specific solvents ( essential oils). Such resins can include resin acids, esters, or alcohols. The exudate is a mobile to highly viscous liquid and often contains crystallized resin particles. Over time and as a result of other influences the exudate loses its liquidizing components or gets chemically converted into a solid material (i.e. by autoxidation). Some authors require balsams to contain benzoic or cinnamic acid or their esters. Plant resins are sometimes classified according to other plant constituents in the mixture, for example as: * pure resins (guaiac, hashish), * gum-resins (containing gums/ polysacchar ...
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Graham Mountain (New York)
Graham Mountain is the seventh highest of the Catskill High Peaks and the highest privately owned mountain in the range. It is located in the town of Hardenburgh, New York, United States. Its summit is unique in the Catskills for its pygmy hardwood forest cover and absence of evergreen boreal species that normally dominate at that elevation in the range, despite the presence of balsam fir on the slopes below the summit. In the early 1960s a relay station was built there for Instructional Television, a predecessor to today's Public Broadcasting Service. The relay station was abandoned after a few years and its ruins can be seen from the slopes and summits of neighboring peaks. Graham is within the Catskill Park. Only part of it is in the state-owned Forest Preserve; the summit and the most common access route are owned by descendants of railroad magnate Jay Gould, a native of the region, who closed the peak to the public indefinitely in January 2021. Prior to then, a success ...
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Woodpecker Ridge
Woodpecker Ridge is a ridge located in the Catskill Mountains of New York southwest of Pine Hill. Mill Brook Ridge Mill Brook Ridge is a mountain A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited ... is located north of Woodpecker Ridge. References Mountains of Ulster County, New York Mountains of New York (state) {{UlsterCountyNY-geo-stub ...
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Mill Brook Ridge
Mill Brook Ridge is a mountain A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually highe ... located in the Catskill Mountains of New York south of Arkville. Mill Brook Ridge is located north of Woodpecker Ridge. References Mountains of Ulster County, New York Mountains of New York (state) {{UlsterCountyNY-geo-stub ...
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Mountain Pass
A mountain pass is a navigable route through a mountain range or over a ridge. Since many of the world's mountain ranges have presented formidable barriers to travel, passes have played a key role in trade, war, and both Human migration, human and animal migration throughout history. At lower elevations it may be called a hill pass. A mountain pass is typically formed between two volcanic peaks or created by erosion from water or wind. Overview Mountain passes make use of a gap (landform), gap, saddle (landform), saddle, col or notch (landform), notch. A topographic saddle is analogous to the mathematical concept of a saddle surface, with a saddle point marking the highest point between two valleys and the lowest point along a ridge. On a topographic map, passes are characterized by contour lines with an hourglass shape, which indicates a low spot between two higher points. In the high mountains, a difference of between the summit and the mountain is defined as a mountain pas ...
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Fleischmanns, New York
Fleischmanns is a village in Delaware County, New York, United States. The population was 351 at the 2010 census. The Village of Fleischmanns is within the town of Middletown and is named after Charles Louis Fleischmann, a Hungarian manufacturer. History Early settlers of this area came from Germany, England, the Netherlands and Ireland. To reach this mountainous place, they traveled by horse and wagon (and later by stagecoach) over rough, dusty roads in summer and rutted, snowy paths in winter. Eventually, the road was resurfaced with planks from Kingston to Pine Hill with the cost of maintenance covered by tollgates along the way. Still, it was a difficult journey until the Ulster and Delaware Railroad reached the village from Rondout and Kingston on May 23, 1870. Fleischmanns was initially named Griffin Corners in honor of Matthew Griffin, a prominent lawyer (he was admitted to the bar in 1851) and businessman (he owned a store and later a hotel). He also helped to sec ...
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Doubletop Mountain (New York)
Doubletop Mountain is a mountain located in Ulster County, New York. The mountain is part of the Catskill Mountains. Doubletop Mountain is flanked to the northwest by Graham Mountain, to the east by Big Indian Mountain, and to the southwest by the Beaver Kill Range. Doubletop Mountain stands within the watershed of the Delaware River, which drains into Delaware Bay. The northeast side of Doubletop Mountain drains into the headwaters of Dry Brook, thence into the East Branch of the Delaware River. The northwest end of Doubletop Mountain drains into Flatiron Brook, thence into Dry Brook. The southwest side of Doubletop drains into the headwaters of Beaver Kill, thence into the East Branch of the Delaware River. The south end of Doubletop drains into High Falls Brook, thence into the West Branch of the Neversink River, and the Delaware River. The southeast slopes of Doubletop drain into Pigeon Brook, thence into Biscuit Brook, and the West Branch of the Neversink. Dou ...
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Barkaboom Mountain
Barkaboom Mountain is a mountain located in the Catskill Mountains of New York southwest of Margaretville. Touchmenot Mountain Touchmenot Mountain is a mountain located in the Catskill Mountains of New York southwest of Margaretville. Cross Mountain is located northeast of Touchmenot Mountain and Barkaboom Mountain Barkaboom Mountain is a mountain located in the ... is located southwest of Barkaboom Mountain and Cross Mountain is located northeast. References Mountains of Delaware County, New York Mountains of New York (state) {{DelawareCountyNY-geo-stub ...
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