Stony Brook (Mehoopany Creek)
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Stony Brook (Mehoopany Creek)
Stony Brook is a tributary of Mehoopany Creek in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through North Branch township and Forkston Township. The brook has a tributary known as Red Brook. Logging was done in the upper reaches of the watershed of Stony Brook in the early 1900s. Course Stony Brook begins in North Branch Township. It enters a valley and flows southeast for approximately two miles (three kilometers) before turning south and entering Forkston Township. Shortly afterwards, the brook receives the tributary Red Brook and turns east. Further downstream, it bends south and then southwest before it reaches its confluence with Mehoopany Creek. Stony Brook joins Mehoopany Creek upstream of its mouth. Tributaries Stony Brook has a tributary known as Red Brook, which has a watershed of . Geography and geology The elevation near the mouth of Stony Brook is above sea level. The elevation of the source of the brook is between . T ...
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Mehoopany Creek
Mehoopany Creek is a tributary of the Susquehanna River in Sullivan and Wyoming counties, Pennsylvania, in the United States. It is approximately long. In Sullivan County the creek flows through Colley Township and in Wyoming County it flows through Forkston Township and Mehoopany Township. The stream's watershed has an area of . Its major tributaries include Stony Brook and North Fork Mehoopany Creek. Mehoopany Creek is designated as a high-quality coldwater fishery in Sullivan County. Its headwaters are listed in the Sullivan County Natural Areas Inventory. Course Mehoopany Creek begins in Splashdam Pond in Colley Township, just west of the eastern border of Sullivan County. The creek flows north and then east. It leaves Sullivan County approximately a mile from its headwaters. Upon leaving Sullivan County, Mehoopany Creek enters Forkstown Township, Wyoming County. In this township, it flows roughly east, entering a valley. It dips southeast, picking up the tributary Bellas ...
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Wyoming County, Pennsylvania
Wyoming County is a county in the Commonwealth of Pennsylvania. It is part of Northeastern Pennsylvania. As of the 2020 census, the population was 26,069. Its county seat is Tunkhannock. It was created in 1842 from part of Luzerne County. Wyoming County is included in the Scranton—Wilkes-Barre—Hazleton, PA Metropolitan Statistical Area. Geography According to the U.S. Census Bureau, the county has a total area of , of which is land and (1.9%) is water. The county is intersected by the North Branch of the Susquehanna River, and drained by Tunkhannock, Mehoopany, and other large creeks. The land surface is generally hilly or mountainous, Mehoopany, Tunkhannock, Knob, and Bowman's mountains occupying a portion. The soil is fertile. Timber, coal, and iron are very abundant. Climate The county has a humid continental climate which is warm-summer (''Dfb'') except along the river starting below Falls where it is hot-summer (''Dfa''). Average monthly temperatures in Tunkhann ...
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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 ...
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Red Brook (Stony Brook)
Red Brook is a tributary of Stony Brook in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Forkston Township. The watershed of the stream has an area of . The stream has been named one of the best places for hiking in Wyoming County and features waterfalls, cascades, cliffs, and boulders. Its headwaters are in Coalbed Swamp, a combined boreal conifer swamp and shrub swamp. Course Red Brook begins on Dutch Mountain in Coalbed Swamp, in Forkston Township. It flows northeast for a short distance before turning east-southeast and entering a valley. After several tenths of a mile, the stream turns east-northeast for several tenths of a mile. It then reaches its confluence with Stony Brook. Red Brook joins Stony Brook upstream of its mouth. Geography and geology The elevation near the mouth of Red Brook is above sea level. The elevation near the stream's source is above sea level. Geographical features along Red Brook include two la ...
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North Branch Township, Wyoming County, Pennsylvania
North Branch Township is a township in Wyoming County, Pennsylvania, Wyoming County, Pennsylvania. The population was 236 at the United States Census 2020, 2020 census. Geography According to the United States Census Bureau, U.S. Census Bureau, the township has a total area of 22.5 square miles (58.2 km2): 22.3 square miles (57.9 km2) is land; 0.1 square miles (0.3 km2, or 0.53%) is water. Demographics As of the census of 2010, there were 206 people, 93 households, and 56 families residing in the township. The population density was 9.2 people per square mile (3.6/km2). There were 129 housing units at an average density of 5.8/sq mi (2.3/km2). The racial makeup of the township was 96.6% White (U.S. Census), White, 0.5% Native American (U.S. Census), Native American, 1% Asian (U.S. Census), Asian and 1.9% from two or more races. Hispanic (U.S. Census), Hispanic or Latino (U.S. Census), Latino of any race were 3.9% of the population. There w ...
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Forkston Township, Wyoming County, Pennsylvania
Forkston Township is a township in Wyoming County, Pennsylvania, United States. The population was 305 at the 2020 census. Geography According to the United States Census Bureau, the township has a total area of , of which is land and 0.2 square miles (0.5 km, or 0.28%) is water. Demographics At the census of 2010, 397 people (in 170 households and 108 families) resided in the Township. The population density was 5.6 people per square mile (2.2/km). The Township held 294 housing units, an average density of 4.2/sq mi (1.6/km). The racial makeup of the township was 98% White, 1% American Indian, 0.25% Asian, 0.25% from other races, and 0.5% from two or more races; Hispanic or Latino persons of any race comprised 0.5% of the population. Of the 170 households, 22.4% had children under the age of 18 living with them, 54.7% were married couples living together, 4.7% had a female householder with no husband present, and 36.5% were non-families. Single persons c ...
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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 ...
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Conglomerate (geology)
Conglomerate () is a clastic sedimentary rock that is composed of a substantial fraction of rounded to subangular gravel-size clasts. A conglomerate typically contains a matrix of finer-grained sediments, such as sand, silt, or clay, which fills the interstices between the clasts. The clasts and matrix are typically cemented by calcium carbonate, iron oxide, silica, or hardened clay. Conglomerates form by the consolidation and lithification of gravel. They can be found in sedimentary rock sequences of all ages but probably make up less than 1 percent by weight of all sedimentary rocks. In terms of origin and depositional mechanisms, they are closely related to sandstones and exhibit many of the same types of sedimentary structures, e.g., tabular and trough cross-bedding and graded bedding.Boggs, S. (2006) ''Principles of Sedimentology and Stratigraphy.'', 2nd ed. Prentice Hall, New York. 662 pp. Friedman, G.M. (2003) ''Classification of sediments and sedimentary rocks.'' In G ...
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Coal
Coal is a combustible black or brownish-black sedimentary rock, formed as rock strata called coal seams. Coal is mostly carbon with variable amounts of other elements, chiefly hydrogen, sulfur, oxygen, and nitrogen. Coal is formed when dead plant matter decays into peat and is converted into coal by the heat and pressure of deep burial over millions of years. Vast deposits of coal originate in former wetlands called coal forests that covered much of the Earth's tropical land areas during the late Carboniferous ( Pennsylvanian) and Permian times. Many significant coal deposits are younger than this and originate from the Mesozoic and Cenozoic eras. Coal is used primarily as a fuel. While coal has been known and used for thousands of years, its usage was limited until the Industrial Revolution. With the invention of the steam engine, coal consumption increased. In 2020, coal supplied about a quarter of the world's primary energy and over a third of its electricity. Some iron ...
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Spruce
A spruce is a tree of the genus ''Picea'' (), a genus of about 35 species of coniferous evergreen trees in the family Pinaceae, found in the northern temperate and boreal (taiga) regions of the Earth. ''Picea'' is the sole genus in the subfamily Piceoideae. Spruces are large trees, from about 20 to 60 m (about 60–200 ft) tall when mature, and have whorled branches and conical form. They can be distinguished from other members of the pine family by their needles (leaves), which are four-sided and attached singly to small persistent peg-like structures (pulvini or sterigmata) on the branches, and by their cones (without any protruding bracts), which hang downwards after they are pollinated. The needles are shed when 4–10 years old, leaving the branches rough with the retained pegs. In other similar genera, the branches are fairly smooth. Spruce are used as food plants by the larvae of some Lepidoptera (moth and butterfly) species, such as the eastern spruce budwo ...
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Trout
Trout are species of freshwater fish belonging to the genera '' Oncorhynchus'', ''Salmo'' and ''Salvelinus'', all of the subfamily Salmoninae of the family Salmonidae. The word ''trout'' is also used as part of the name of some non-salmonid fish such as ''Cynoscion nebulosus'', the spotted seatrout or speckled trout. Trout are closely related to salmon and char (or charr): species termed salmon and char occur in the same genera as do fish called trout (''Oncorhynchus'' – Pacific salmon and trout, ''Salmo'' – Atlantic salmon and various trout, ''Salvelinus'' – char and trout). Lake trout and most other trout live in freshwater lakes and rivers exclusively, while there are others, such as the steelhead, a form of the coastal rainbow trout, that can spend two or three years at sea before returning to fresh water to spawn (a habit more typical of salmon). Arctic char and brook trout are part of the char genus. Trout are an important food source for humans and wildlife, ...
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Henry Lott Brook
Henry Lott Brook is a tributary of Mehoopany Creek in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Forkston Township. The watershed of the stream has an area of . The stream is not designated as an impaired waterbody and it is classified as a High-Quality Coldwater Fishery. It is one of five large tributaries of Mehoopany Creek to cut through the Mehoopany Creek- Bowman Creek watershed divide. Course Henry Lott Brook begins on South Mountain in Forkston Township. It flows in a roughly northerly direction for several tenths of a mile, entering a valley. The stream then turns north-northwest for more than a mile before turning north and reaching the end of its valley. It then reaches its confluence with Mehoopany Creek. Henry Lott Brook joins Mehoopany Creek upstream of its mouth. Geography, geology, and hydrology The elevation near the mouth of Henry Lott Brook is above sea level. The elevation near the stream's source is a ...
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