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Lake Neepaulin
Lake Neepaulin is a small man-made freshwater lake located in Wantage Township in Sussex County, New Jersey in the United States.United States Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map. Retrieved July 20, 2015. See also: United States Geological Survey, ''Hamburg, NJ Quadrangle USGS 1:24 Topographic Map 41074B5''. Located in the watershed of Papakating Creek, a tributary of the Wallkill River, the lake was created in the 1950s by damming an unnamed mountain stream as the feature of a private residential development. The stream, now known as Neepaulakating Creek, did not receive a name until 2002.Friends of Lake Neepaulin, Nathaniel Sajdak, Jennifer E. Runyon (USGS), United States Board of Geographic NamesCase Brief: Neepaulakating Creek(2002). Retrieved July 20, 2015. Description Lake Neepaulin is a man-made lake created from the damming of Neepaulakating Creek, a small mountain stream that was not named until 2002. The creek' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neepaulakating Creek
Neepaulakating Creek is a 2.4-mile long (3.8 km) tributary of Papakating Creek in Wantage Township in Sussex County, New Jersey in the United States.United States Geological Survey, Geographic Names Information SystemFeature Detail Report for: Neepaulakating Creek Retrieved June 26, 2015.United States Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map Retrieved June 26, 2015. Note: The upper elevation of its headwaters is approximately 640 feet above mean sea level derived from a reading of the USGS NHD topographic map. The NHD information provides the elevation the mouth at 395 feet above mean sea level. See also: United States Geological Survey, ''Hamburg, NJ Quadrangle USGS 1:24 Topographic Map 41074B5'' and ''Branchville, NJ Quadrangle USGS 1:24 Topographic Map 41074B4''. It is one of three streams feeding the Papakating Creek, a major contributor to the Wallkill River. Although the stream was dammed in the 1950s to create Lak ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wantage Township, New Jersey
Wantage Township is a township in Sussex County, New Jersey, United States. As of the 2010 United States Census, its population was 11,358, reflecting an increase of 971 (+9.3%) from the 10,387 counted in the 2000 Census, which had in turn increased by 900 (+9.5%) from the 9,487 counted in the 1990 Census. Wantage Township was formed as a precinct on May 30, 1754, from portions of Newton Township. It was incorporated as a township on February 21, 1798, as part of the state's initial group of 104 townships. Boundary exchanges were made with Frankford Township in both 1826 and 1834. Portions of the township were taken on October 14, 1891 to form the Borough of Deckertown (renamed Sussex borough in 1902).Snyder, John P''The Story of New Jersey's Civil Boundaries: 1606-1968'' Bureau of Geology and Topography; Trenton, New Jersey; 1969. p. 233. Accessed October 25, 2012. The township was named for Wantage, England. Geography According to the United States Census Bureau, the t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kittatinny Valley
The Kittatinny Valley is a section of the Great Appalachian Valley in Sussex and Warren counties in northwestern New Jersey that is bounded on the northwest by Kittatinny Mountain, and in the southeast by the New Jersey Highlands region. The valley is roughly long, with a breadth of . Geology and geography The Kittatinny Valley is in northern New Jersey. The western side of the valley goes from the New York state line, east of High Point, and runs southwest along the base of the eastern slope of Kittatinny Mountains to the terminal moraine created by the Wisconsin Glacier just north of Columbia on the New Jersey border with Pennsylvania. This is slightly south of the Delaware Water Gap. The eastern side of the valley trends northeast along Highlands of the Jenny Jump Mountains, then along the base of Allamuchy Mountains to Andover where it follows the western edge of the Pimple Hills to the Hamburg Mountains. The eastern edge of the valley follows the western base of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Papakating Creek Watershed
Papakating Creek is a tributary of the Wallkill River located in Frankford and Wantage townships in Sussex County, New Jersey in the United States. The creek rises in a small swamp located beneath the eastern face of Kittatinny Mountain in Frankford and its waters join the Wallkill to the east of Sussex borough. Papakating Creek and its three major tributaries drain the northern portion of New Jersey's Kittatinny Valley a fertile valley underlain by shale and limestone of the Ordovician Martinsburg Formation and soils deposited by retreating glaciers in the last ice age. The region which the Papakating Creek and its tributaries drain is largely rural farmland and forests with a few low-density residential communities. The New Jersey Department of Environmental Protection reports that phosphorus and fecal coliform from agricultural or residential runoff as well as arsenic from agricultural pesticide applications or regional mineralogy impair the creek. Within the waters ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reservoirs In New Jersey
A reservoir (; from French ''réservoir'' ) is an enlarged lake behind a dam. Such a dam may be either artificial, built to store fresh water or it may be a natural formation. Reservoirs can be created in a number of ways, including controlling a watercourse that drains an existing body of water, interrupting a watercourse to form an embayment within it, through excavation, or building any number of retaining walls or levees. In other contexts, "reservoirs" may refer to storage spaces for various fluids; they may hold liquids or gasses, including hydrocarbons. ''Tank reservoirs'' store these in ground-level, elevated, or buried tanks. Tank reservoirs for water are also called cisterns. Most underground reservoirs are used to store liquids, principally either water or petroleum. Types Dammed valleys Dammed reservoirs are artificial lakes created and controlled by a dam constructed across a valley, and rely on the natural topography to provide most of the basin of the re ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Goose
A goose (plural, : geese) is a bird of any of several waterfowl species in the family (biology), family Anatidae. This group comprises the genera ''Anser (bird), Anser'' (the grey geese and white geese) and ''Branta'' (the black geese). Some other birds, mostly related to the shelducks, have "goose" as part of their names. More distantly related members of the family Anatidae are swans, most of which are larger than true geese, and ducks, which are smaller. The term "goose" may refer to either a male or female bird, but when paired with "gander", refers specifically to a female one (the latter referring to a male). Young birds before fledging are called goslings. The List of collective nouns, collective noun for a group of geese on the ground is a gaggle; when in flight, they are called a skein, a team, or a wedge; when flying close together, they are called a plump. Etymology The word "goose" is a direct descendant of,''*ghans-''. In Germanic languages, the root gave Old E ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fertilizer
A fertilizer (American English) or fertiliser (British English; see spelling differences) is any material of natural or synthetic origin that is applied to soil or to plant tissues to supply plant nutrients. Fertilizers may be distinct from liming materials or other non-nutrient soil amendments. Many sources of fertilizer exist, both natural and industrially produced. For most modern agricultural practices, fertilization focuses on three main macro nutrients: nitrogen (N), phosphorus (P), and potassium (K) with occasional addition of supplements like rock flour for micronutrients. Farmers apply these fertilizers in a variety of ways: through dry or pelletized or liquid application processes, using large agricultural equipment or hand-tool methods. Historically fertilization came from natural or organic sources: compost, animal manure, human manure, harvested minerals, crop rotations and byproducts of human-nature industries (i.e. fish processing waste, or bloodmeal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Phosphorus
Phosphorus is a chemical element with the symbol P and atomic number 15. Elemental phosphorus exists in two major forms, white phosphorus and red phosphorus, but because it is highly reactive, phosphorus is never found as a free element on Earth. It has a concentration in the Earth's crust of about one gram per kilogram (compare copper at about 0.06 grams). In minerals, phosphorus generally occurs as phosphate. Elemental phosphorus was first isolated as white phosphorus in 1669. White phosphorus emits a faint glow when exposed to oxygen – hence the name, taken from Greek mythology, meaning 'light-bearer' (Latin ), referring to the "Morning Star", the planet Venus. The term '' phosphorescence'', meaning glow after illumination, derives from this property of phosphorus, although the word has since been used for a different physical process that produces a glow. The glow of phosphorus is caused by oxidation of the white (but not red) phosphorus — a process now called chemi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clove Acres Lake
Clove Brook is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map, accessed October 3, 2011 tributary of Papakating Creek in Sussex County, New Jersey in the United States.Gertler, Edward. ''Garden State Canoeing'', Seneca Press, 2002. Clove Brook, previously known as ''Bastions Brook'', ''Clove Creek'', ''Clove River'', and ''Deep Clove River'', rises from north of Colesville and travels in a southeasterly direction, predominantly on the north side of State Route 23, down through the Clove Valley toward Sussex Borough. The brook enters the north end of Clove Acres Lake, passes over the dam, and proceeds through the center of the Borough of Sussex. Leaving the borough, the brook turns south and joins Papakating Creek just north of Lewisburg. The name Bastions Brook was noted as a part of the description of a parcel of land in a deed signed by Peter Decker in the eighteenth century. See also *List of rivers of New Jersey *West B ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
New Jersey Department Of Environmental Protection
The New Jersey Department of Environmental Protection (NJDEP) is a government agency in the U.S. state of New Jersey that is responsible for managing the state's natural resources and addressing issues related to pollution. NJDEP now has a staff of approximately 2,850. The department was created on April 22, 1970, America's first official Earth Day, making it the third state in the country to combine its environmental activities into a single, unified agency, with about 1,400 employees in five divisions, charged with responsibility for environmental protection and conservation efforts. Governor William T. Cahill appointed Richard J. Sullivan as the first commissioner. In December 2017, Catherine McCabe was nominated by New Jersey governor-elect Phil Murphy to serve as Commissioner of the New Jersey Department of Environmental Protection. Shawn M. LaTourette succeeded her in January 2021. Other former Commissioners have included Lisa P. Jackson and Bradley M. Campbell. Division ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Martinsburg Formation
The Ordovician Martinsburg Formation (Om) is a mapped bedrock unit in Pennsylvania, New Jersey, Maryland, Virginia, and West Virginia. It is named for the town of Martinsburg, West Virginia for which it was first described. It is the dominant rock formation of the Great Appalachian Valley in New Jersey (where it is called Kittatinny Valley and Pennsylvania (in the Lehigh Valley and Lebanon Valley). Description The Martinsburg is defined as a gray to dark gray, and infrequently tan and purple shale and slate. Local members of impure sandstone; thin, argillaceous limestone or phyllitic shale are present in the Cumberland Valley and the Lehigh Valley.Berg, T.M., Edmunds, W.E., Geyer, A.R. and others, compilers, (1980). Geologic Map of Pennsylvania: Pennsylvania Geologic Survey, Map 1, scale 1:250,000. The Martinsburg has three defined members in the Lehigh Valley: The Bushkill Member which is the basal slate unit. The Ramseyburg Member which is composed of alternating turbidite san ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Private Community
A private community is a residential community that can be an association or a proprietary organization. Associations can include condominiums, homeowner associations or cooperatives. Whereas governmental communities are financed with taxation, where taxes typically have little connection with benefits, private communities' benefits are financed by payments from its members. In a hotel, for example, the public goods such as elevators and security are paid for from room charges. One early American example was Lucas Place, created in 1851 in St. Louis, Missouri, the first of about 50 such private places unique to the city. Today, there are "60 million people who now live in roughly 300,000 private communities" in the United States. A noteworthy Canadian example, Arbutus Ridge Seaside Community for Active Adults in the Cowichan Valley on Vancouver Island was the first comprehensive retirement community built in Canada. It subsequently became the template and proving ground for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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