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Conety Run
Conety Run (also known as Conety's Run) is a tributary of Little Nescopeck Creek in Luzerne County, Pennsylvania, in the United States. It is approximately long and flows through Fairview Township and Dennison Township. The watershed of the stream has an area of . The stream is designated as Class A Wild Trout Waters, but was historically stocked. It has an alkalinity concentration of 2 milligrams per liter, but is slightly acidic. The surficial geology in its vicinity mainly consists of alluvium, Wisconsinan Till, Wisconsinan Ice-Contact Stratified Drift, and bedrock consisting of sandstone and shale. Course Conety Run begins on Stony Cabin Ridge in Fairview Township. It flows west for a short distance before turning south-southwest for several tenths of a mile. It then passes through Fountain Lake and turns south for several tenths of a mile. The stream then enters Dennison Township and turns south-southeast. After more than a mile, it turns south-southwest and then south, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nescopeck Creek
Nescopeck Creek is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed August 8, 2011 tributary of the Susquehanna River in Luzerne County, Pennsylvania. The creek is in the Coal Region of Pennsylvania. The meaning of the creek's name is "deep black waters". The waters of Nescopeck Creek have difficulty ratings between Class I and Class III. However, during parts of the year, Nescopeck Creek is impossible to navigate due to rapids, flooding, and tight bends. Nescopeck Creek is home to a number of species of trout, although the waters are not always optimal for them. Nescopeck Creek's water is acidic, with a pH as low as 3.6 in some studies. Much of the land in the Nescopeck Creek's watershed is forest. Farmland is common in the lower portions of the Nescopeck Creek watershed and the Little Nescopeck Creek watershed, while coal mines are more common on Nescopeck Creek's tributaries Black Creek, Stony Creek, and Cranberry ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sea Level
Mean sea level (MSL, often shortened to sea level) is an average surface level of one or more among Earth's coastal bodies of water from which heights such as elevation may be measured. The global MSL is a type of vertical datuma standardised geodetic datumthat is used, for example, as a chart datum in cartography and marine navigation, or, in aviation, as the standard sea level at which atmospheric pressure is measured to calibrate altitude and, consequently, aircraft flight levels. A common and relatively straightforward mean sea-level standard is instead the midpoint between a mean low and mean high tide at a particular location. Sea levels can be affected by many factors and are known to have varied greatly over geological time scales. Current sea level rise is mainly caused by human-induced climate change. When temperatures rise, Glacier, mountain glaciers and the Ice sheet, polar ice caps melt, increasing the amount of water in water bodies. Because most of human settlem ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Central Railroad Of New Jersey
The Central Railroad of New Jersey, also known as the Jersey Central or Jersey Central Lines , was a Class I railroad with origins in the 1830s. It was absorbed into Conrail in April 1976 along with several other prominent bankrupt railroads of the Northeastern United States. History The earliest railroad ancestor of the CNJ was the Elizabethtown & Somerville Railroad, incorporated in 1831 and opened from Elizabethport to Elizabeth, New Jersey in 1836. Horses gave way to steam in 1839, and the railroad was extended west, reaching Somerville at the beginning of 1842. The Somerville & Easton Railroad was incorporated in 1847 and began building westward. In 1849 it purchased the Elizabethtown & Somerville and adopted a new name: Central Railroad Company of New Jersey. The line reached Phillipsburg, on the east bank of the Delaware River, in 1852. It was extended east across Newark Bay to Jersey City in 1864, and it gradually acquired branches to Flemington, Newark, Perth Am ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glen Summit Springs, Pennsylvania
Glen Summit Springs is a private community located in Northeastern Pennsylvania, United States, on the northern slope of the eastern end of Nescopeck Mountain, where it sweeps to the north to meet the southward bend of Penobscot Mountain. The area has long been known regionally for its mountain springs and is now protected by over of pristine, uncultivated forest made up of privately owned and conservation lands. The area was once the summer residence of many of the Wyoming Valley elite including the Kirbys, Welles, Hollenbacks, and Sterlings. The community is located in Fairview Township, Luzerne County, Pennsylvania, east of the census-designated place of Mountain Top. Early settlers One of the first settlers of Glen Summit Springs was John Conety. In the end of the 19th and the beginning of the 20th century, Conety owned approximately that included present-day Indian Springs and Glen Summit Springs. Conety had a log cabin on the property and kept a roadhouse for pa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geographic Names Information System
The Geographic Names Information System (GNIS) is a database of name and locative information about more than two million physical and cultural features throughout the United States and its territories, Antarctica, and the associated states of the Marshall Islands, Federated States of Micronesia, and Palau. It is a type of gazetteer. It was developed by the United States Geological Survey (USGS) in cooperation with the United States Board on Geographic Names (BGN) to promote the standardization of feature names. Data were collected in two phases. Although a third phase was considered, which would have handled name changes where local usages differed from maps, it was never begun. The database is part of a system that includes topographic map names and bibliographic references. The names of books and historic maps that confirm the feature or place name are cited. Variant names, alternatives to official federal names for a feature, are also recorded. Each feature receives a per ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Times Leader
The ''Times Leader'' is a privately owned newspaper in Wilkes-Barre, Pennsylvania. Founding Founded in 1879, it was locally owned until being purchased by Capital Cities in 1978. Early history On November 27, 1907, the ''Wilkes-Barre Times'' printed a notice that it and the ''Wilkes-Barre Leader'', both afternoon dailies, would merge, creating The ''Times Leader'' with the first newspaper to be dated Monday December 2, 1907. The ''Times Leader'', in the heart of coal country, was subject to a very bitter strike that began October 6, 1978. Over 200 union employees walked off the job in defiance of what they viewed as union busting tactics by the ''Times Leaders new corporate owner, Capital Cities. The four striking newspaper unions began to publish the ''Citizens' Voice'' as a strike paper. Eventually the four unions were decertified. The ''Voice'' continued publication. This in turn prompted competition and created the unusual environment where Wilkes-Barre, with its popula ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Forest
A forest is an area of land dominated by trees. Hundreds of definitions of forest are used throughout the world, incorporating factors such as tree density, tree height, land use, legal standing, and ecological function. The United Nations' Food and Agriculture Organization (FAO) defines a forest as, "Land spanning more than 0.5 hectares with trees higher than 5 meters and a canopy cover of more than 10 percent, or trees able to reach these thresholds ''in situ''. It does not include land that is predominantly under agricultural or urban use." Using this definition, '' Global Forest Resources Assessment 2020'' (FRA 2020) found that forests covered , or approximately 31 percent of the world's land area in 2020. Forests are the predominant terrestrial ecosystem of Earth, and are found around the globe. More than half of the world's forests are found in only five countries (Brazil, Canada, China, Russia, and the United States). The largest share of forests (45 percent) are in th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
United States Geological Survey
The United States Geological Survey (USGS), formerly simply known as the Geological Survey, is a scientific agency of the United States government. The scientists of the USGS study the landscape of the United States, its natural resources, and the natural hazards that threaten it. The organization's work spans the disciplines of biology, geography, geology, and hydrology. The USGS is a fact-finding research organization with no regulatory responsibility. The agency was founded on March 3, 1879. The USGS is a bureau of the United States Department of the Interior; it is that department's sole scientific agency. The USGS employs approximately 8,670 people and is headquartered in Reston, Virginia. The USGS also has major offices near Lakewood, Colorado, at the Denver Federal Center, and Menlo Park, California. The current motto of the USGS, in use since August 1997, is "science for a changing world". The agency's previous slogan, adopted on the occasion of its hundredt ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Till
image:Geschiebemergel.JPG, Closeup of glacial till. Note that the larger grains (pebbles and gravel) in the till are completely surrounded by the matrix of finer material (silt and sand), and this characteristic, known as ''matrix support'', is diagnostic of till. image:Glacial till exposed in roadcut-750px.jpg, Glacial till with tufts of grass Till or glacial till is unsorted glacier, glacial sediment. Till is derived from the erosion and entrainment of material by the moving ice of a glacier. It is deposited some distance down-ice to form terminal, lateral, medial and ground moraines. Till is classified into primary deposits, laid down directly by glaciers, and secondary deposits, reworked by fluvial transport and other processes. Description Till is a form of '' glacial drift'', which is rock material transported by a glacier and deposited directly from the ice or from running water emerging from the ice. It is distinguished from other forms of drift in that it is depos ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers ( laminae) less than one centimeter in thickness. This property is called '' fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the more narrow sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable beddin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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