Stony Run (Little Catawissa Creek Tributary)
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Stony Run (Little Catawissa Creek Tributary)
Stony Run is a tributary of Little Catawissa Creek in Schuylkill County, Pennsylvania, in the United States. It is approximately long and flows through Union Township. The watershed of the stream has an area of . The stream is polluted and acidic. However, it is considered to be a coldwater fishery. The main rock formations in the stream's watershed are the Mauch Chunk Formation and the Pocono Formation. The main soils in the watershed are the Leck Kill soil and the Hazleton soil. No fish inhabit the stream. Course Stony Run begins on Little Mountain in Union Township. It flows east for several tenths of a mile before turning southeast for several hundred feet, leaving behind Catawissa Mountain and Little Mountain. The stream then turns northeast for a few tenths of a mile before turning east-northeast. Several tenths of a mile downstream, it crosses Ridge Road and turns east-southeast, almost immediately reaching its confluence with Little Catawissa Creek. Stony Run joins Littl ...
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Catawissa Creek
Catawissa Creek (colloquially known as The Cat) 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 east-central Pennsylvania in the United States. Its Drainage basin, watershed has an area of . The waters of Catawissa Creek are highly acidic, with a pH of 4.5, due to runoff from an abandoned mine in the creek's watershed. Catawissa Creek is smaller than the nearby Fishing Creek (North Branch Susquehanna River), Fishing Creek due to a lack of major tributaries. Catawissa Creek starts in Luzerne County, not far from Hazleton, Pennsylvania, Hazleton. It flows west and slightly south into Schuylkill County, Pennsylvania, Schuylkill County before flowing north into Columbia County, Pennsylvania, Columbia County and then west to the Susquehanna River, which it flows into at Catawissa, Pennsylvania, Catawissa. It parallels Catawissa Mountain for a significant portion of it ...
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Soil
Soil, also commonly referred to as earth or dirt, is a mixture of organic matter, minerals, gases, liquids, and organisms that together support life. Some scientific definitions distinguish ''dirt'' from ''soil'' by restricting the former term specifically to displaced soil. Soil consists of a solid phase of minerals and organic matter (the soil matrix), as well as a porous phase that holds gases (the soil atmosphere) and water (the soil solution). Accordingly, soil is a three-state system of solids, liquids, and gases. Soil is a product of several factors: the influence of climate, relief (elevation, orientation, and slope of terrain), organisms, and the soil's parent materials (original minerals) interacting over time. It continually undergoes development by way of numerous physical, chemical and biological processes, which include weathering with associated erosion. Given its complexity and strong internal connectedness, soil ecologists regard soil as an ecosystem. Most ...
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Rivers Of Schuylkill County, Pennsylvania
A river is a natural flowing watercourse, usually freshwater, flowing towards an ocean, sea, lake or another river. In some cases, a river flows into the ground and becomes dry at the end of its course without reaching another body of water. Small rivers can be referred to using names such as creek, brook, rivulet, and rill. There are no official definitions for the generic term river as applied to geographic features, although in some countries or communities a stream is defined by its size. Many names for small rivers are specific to geographic location; examples are "run" in some parts of the United States, "burn" in Scotland and northeast England, and "beck" in northern England. Sometimes a river is defined as being larger than a creek, but not always: the language is vague. Rivers are part of the water cycle. Water generally collects in a river from precipitation through a drainage basin from surface runoff and other sources such as groundwater recharge, springs, a ...
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Trexler Run
Trexler Run is a tributary of Little Catawissa Creek in Columbia County, Pennsylvania, Columbia and Schuylkill County, Pennsylvania, Schuylkill counties in Pennsylvania, in the United States. It is approximately long and flows through Roaring Creek Township in Columbia County and Union Township in Schuylkill County. The watershed of the stream has an area of . The stream is considered to be a High-Quality Coldwater Fishery and Class A Wild Trout Waters. The main rock formations in the stream's watershed are the Mauch Chunk Formation, the Pocono Formation, and the Pottsville Formation and the main soil is the Leck Kill soil. Both brook trout and brown trout inhabit the stream, as do several other species of fish. Course Trexler Run begins in a valley on Little Mountain in Roaring Creek Township, Pennsylvania, Roaring Creek Township, Columbia County. It flows south-southeast for several tenths of a mile, exiting Roaring Creek Township and Columbia County. Upon exiting Columbia Coun ...
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