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Newport Creek
Newport Creek is a tributary of the Susquehanna River in Luzerne County, Pennsylvania, in the United States. It is in length. Named tributaries of the creek include South Branch Newport Creek. The entire watershed of Newport Creek is considered by the Pennsylvania Department of Environmental Protection to be impaired. Course Newport Creek begins in the community of Glen Lyon. It flows in an east-northeast direction into Luzerne County, not far from some strip mines. The creek parallels the Delaware and Hudson Railroad for some distance before turning north and then northeast to follow the railroad. The creek gets much closer to the strip mines at this point. It continues east, out of Newport Township and into the community of Nanticoke, where the tributary South Branch Newport Creek flows into Newport Creek. Newport Creek then flows through Nanticoke, passing a mountain known as Honey Pot. At this point, the creek turns north and reaches its confluence with the Susquehanna River ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Middle Branch Newport Creek
Middle Branch Newport Creek is a tributary of Newport Creek in Luzerne County, Pennsylvania, in the United States. It is approximately long and flows through Newport Township, Luzerne County, Pennsylvania, Newport Township. The creek is in the United States Geological Survey quadrangle of Nanticoke. It is considered to be impaired by abandoned mine drainage for . The creek was listed as an impaired stream in 2004. Course Middle Branch Newport Creek begins in Newport Township, on the border of Glen Lyon, Pennsylvania, Glen Lyon. It flows east for several hundred feet before turning north-northeast for a few tenths of a mile, crossing West Kirmar Ave/East Main Street. The creek then turns northeast again for some distance and passes near a number of small ponds before turning nearly due north for several hundred feet. At this point, it leaves the border of Glen Lyon and flows northeast before briefly turning northwest and reaching its confluence with Newport Creek. Hydrology A total ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
South Branch Newport Creek
South Branch Newport Creek is a tributary of Newport Creek in Luzerne County, Pennsylvania, in the United States. It is long. The entire watershed of the creek is considered by the Pennsylvania Department of Environmental Protection to be impaired. Mining has also been done in the watershed. Course South Branch Newport Creek begins in strip mines near the community of Wanamie in Newport Township. The headwaters are located north of Penobscot Mountain. The creek flows east for some distance before gradually turning north slightly west of the community of Alden. It then flows into the western part of Nanticoke, where it joins Newport Creek. Tributaries South Branch Newport Creek has one named tributary, which is known as Reservoir Creek. It also has an unnamed tributary. Hydrology At the headwaters of South Branch Newport Creek, the daily load of iron is . The concentration of iron at this location is 0.26 milligrams per liter. Downstream of UNTUnnamed tributary 28346, the dail ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glen Lyon, Pennsylvania
Glen Lyon is a census-designated place (CDP) in Newport Township, Luzerne County, Pennsylvania, United States. The population was 1,873 at the 2010 census. History The town of Glen Lyon was founded after anthracite coal mining began in Newport Township (ca. 1869). The colliery was operated by the Susquehanna Coal Company, a Pennsylvania Railroad property. The west side of the community was once called Morgantown; the east side was referred to as Williamstown. Later, the Glen Lyon Rail Station was established and the town was named after the terminus. Part of the east side, which was separated from the rest of the community by the railroad, became known as Canada. Roads and a streetcar line linked the town to Nanticoke and Wilkes-Barre. The streetcar line was replaced eventually by buses and automobiles as the main means of transport. A hill divided the community into two parts. Sixth Shaft was established on the hill. Coal hoisted from that mine was moved across a bridge to the bre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sediment
Sediment is a naturally occurring material that is broken down by processes of weathering and erosion, and is subsequently transported by the action of wind, water, or ice or by the force of gravity acting on the particles. For example, sand and silt can be carried in suspension in river water and on reaching the sea bed deposited by sedimentation; if buried, they may eventually become sandstone and siltstone (sedimentary rocks) through lithification. Sediments are most often transported by water (fluvial processes), but also wind (aeolian processes) and glaciers. Beach sands and river channel deposits are examples of fluvial transport and deposition, though sediment also often settles out of slow-moving or standing water in lakes and oceans. Desert sand dunes and loess are examples of aeolian transport and deposition. Glacial moraine deposits and till are ice-transported sediments. Classification Sediment can be classified based on its grain size, grain shape, and c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coal Seam
Coal mining is the process of extracting coal from the ground. Coal is valued for its energy content and since the 1880s has been widely used to generate electricity. Steel and cement industries use coal as a fuel for extraction of iron from iron ore and for cement production. In the United Kingdom and South Africa, a coal mine and its structures are a colliery, a coal mine is called a 'pit', and the above-ground structures are a 'pit head'. In Australia, "colliery" generally refers to an underground coal mine. Coal mining has had many developments in recent years, from the early days of men tunneling, digging and manually extracting the coal on carts to large open-cut and longwall mines. Mining at this scale requires the use of draglines, trucks, conveyors, hydraulic jacks and shearers. The coal mining industry has a long history of significant negative environmental impacts on local ecosystems, health impacts on local communities and workers, and contributes heavily to th ... [...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] |
Sedimentary Rock
Sedimentary rocks are types of rock that are formed by the accumulation or deposition of mineral or organic particles at Earth's surface, followed by cementation. Sedimentation is the collective name for processes that cause these particles to settle in place. The particles that form a sedimentary rock are called sediment, and may be composed of geological detritus (minerals) or biological detritus (organic matter). The geological detritus originated from weathering and erosion of existing rocks, or from the solidification of molten lava blobs erupted by volcanoes. The geological detritus is transported to the place of deposition by water, wind, ice or mass movement, which are called agents of denudation. Biological detritus was formed by bodies and parts (mainly shells) of dead aquatic organisms, as well as their fecal mass, suspended in water and slowly piling up on the floor of water bodies (marine snow). Sedimentation may also occur as dissolved minerals precipitate from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Interbedding
In geology, interbedding occurs when beds (layers of rock) of a particular lithology lie between or alternate with beds of a different lithology. For example, sedimentary rocks may be interbedded if there were sea level variations in their sedimentary depositional environment. Intercalation is a special case of interbedding where a layer is variably inserted into an already existing sequence; or where two separate depositional environments in close spatial proximity migrate alternately across the contact. While interbedding has layers that are horizontally flat (or aligned with the angle of the entire stratum), intercalated rock on the other hand has slanted layers that streak through each other (even when it aligns with the stratum). For example intercalated conglomerate and sandstone looks like ripples of different material networked through each other somewhat off the horizontal, as the beds are deposited in a gradient. This is likely due to differing fluvial conditions and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pleistocene
The Pleistocene ( , often referred to as the ''Ice age'') is the geological Epoch (geology), epoch that lasted from about 2,580,000 to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was finally confirmed in 2009 by the International Union of Geological Sciences, the cutoff of the Pleistocene and the preceding Pliocene was regarded as being 1.806 million years Before Present (BP). Publications from earlier years may use either definition of the period. The end of the Pleistocene corresponds with the end of the last glacial period and also with the end of the Paleolithic age used in archaeology. The name is a combination of Ancient Greek grc, label=none, πλεῖστος, pleīstos, most and grc, label=none, καινός, kainós (latinized as ), 'new'. At the end of the preceding Pliocene, the previously isolated North and South American continents were joined by the Isthmus of Panama, causing Great American Interchang ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glaciofluvial Deposits
Glaciofluvial deposits or Glacio-fluvial sediments consist of boulders, gravel, sand, silt and clay from ice sheets or glaciers. They are transported, sorted and deposited by streams of water. The deposits are formed beside, below or downstream from the ice. They include kames, kame terraces and eskers formed in ice contact and outwash fans and outwash plains below the ice margin. Typically the outwash sediment is carried by fast and turbulent fluvio-glacial meltwater streams, but occasionally it is carried by catastrophic outburst floods. Larger elements such as boulders and gravel are deposited nearer to the ice margin, while finer elements are carried farther, sometimes into lakes or the ocean. The sediments are sorted by fluvial processes. They differ from glacial till, which is moved and deposited by the ice of the glacier, and is unsorted. Ice-contact deposits A subglacial megaflood may cut cavities into the base of the ice. As the flood dies down, sediment is deposited ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coal Region
The Coal Region is a region of Northeastern Pennsylvania. It is known for being home to the largest known deposits of anthracite, anthracite coal in the world with an estimated reserve of seven billion short tons. The region is typically defined as comprising five Pennsylvania counties, Carbon County, Pennsylvania, Carbon County, Lackawanna County, Pennsylvania, Lackawanna County, Luzerne County, Pennsylvania, Luzerne County, Northumberland County, Pennsylvania, Northumberland County, and Schuylkill County, Pennsylvania, Schuylkill County. It is home to 910,716 people as of the 2010 census. The Coal Region is bordered by Berks County, Pennsylvania, Berks, Lehigh County, Pennsylvania, Lehigh, and Northampton County, Pennsylvania, Northampton Counties (including the Lehigh Valley) to its south; Columbia County, Pennsylvania, Columbia and Dauphin County, Pennsylvania, Dauphin Counties to its west; Wyoming County, Pennsylvania, Wyoming County to its north; and Warren County, New Je ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Little Wilkes-Barre Mountain
Little is a synonym for small size and may refer to: Arts and entertainment * ''Little'' (album), 1990 debut album of Vic Chesnutt * ''Little'' (film), 2019 American comedy film *The Littles, a series of children's novels by American author John Peterson ** ''The Littles'' (TV series), an American animated series based on the novels Places *Little, Kentucky, United States *Little, West Virginia, United States Other uses *Clan Little, a Scottish clan *Little (surname), an English surname *Little (automobile), an American automobile manufactured from 1912 to 1915 *Little, Brown and Company, an American publishing company * USS ''Little'', multiple United States Navy ships See also * * *Little Mountain (other) *Little River (other) Little River may refer to several places: Australia Streams New South Wales *Little River (Dubbo), source in the Dubbo region, a tributary of the Macquarie River * Little River (Oberon), source in the Oberon Shire, a tributary of Cox ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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