Mehoopany Creek is a tributary of the Susquehanna River in Sullivan and Wyoming counties, Pennsylvania , in the United States. It is approximately 26.8 miles (43.1 km) 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 123 square miles (320 km). Its major tributaries include Stony Brook and North Fork Mehoopany Creek.
58-814: Mehoopany Creek is designated as a high-quality coldwater fishery in Sullivan County. Its headwaters are listed in the Sullivan County Natural Areas Inventory. 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
116-711: A sink or a source of carbon, depending on the specific wetland. If they function as a carbon sink, they can help with climate change mitigation . However, wetlands can also be a significant source of methane emissions due to anaerobic decomposition of soaked detritus , and some are also emitters of nitrous oxide . Humans are disturbing and damaging wetlands in many ways, including oil and gas extraction , building infrastructure, overgrazing of livestock , overfishing , alteration of wetlands including dredging and draining, nutrient pollution , and water pollution . Wetlands are more threatened by environmental degradation than any other ecosystem on Earth, according to
174-402: A frequency and duration to support, and that under normal circumstances do support, a prevalence of vegetation typically adapted for life in saturated soil conditions. Wetlands generally included swamps, marshes, bogs, and similar areas.' For each of these definitions and others, regardless of the purpose, hydrology is emphasized (shallow waters, water-logged soils). The soil characteristics and
232-1259: A polar climate, wetland temperatures can be as low as −50 °C (−58 °F). Peatlands in arctic and subarctic regions insulate the permafrost , thus delaying or preventing its thawing during summer, as well as inducing its formation. The amount of precipitation a wetland receives varies widely according to its area. Wetlands in Wales , Scotland , and western Ireland typically receive about 1,500 mm (59 in) per year. In some places in Southeast Asia , where heavy rains occur, they can receive up to 10,000 mm (390 in). In some drier regions, wetlands exist where as little as 180 mm (7.1 in) precipitation occurs each year. Temporal variation: Surface flow may occur in some segments, with subsurface flow in other segments. Wetlands vary widely due to local and regional differences in topography , hydrology , vegetation , and other factors, including human involvement. Other important factors include fertility, natural disturbance, competition, herbivory , burial and salinity. When peat accumulates, bogs and fens arise. The most important factor producing wetlands
290-471: A population of 275; and Forkston, with a population of 210. Major roads in the watershed include Pennsylvania Route 87 . A gauging station was established on Mehoopany Creek in January 1914. Industries done in the watershed of Mehoopany Creek in the early 1900s included agriculture . The creek also provided water power for a number of mills . The Lehigh Valley Railroad also traversed the upper part of
348-540: A portion of the overall water cycle, which also includes atmospheric water (precipitation) and groundwater . Many wetlands are directly linked to groundwater and they can be a crucial regulator of both the quantity and quality of water found below the ground. Wetlands that have permeable substrates like limestone or occur in areas with highly variable and fluctuating water tables have especially important roles in groundwater replenishment or water recharge. Substrates that are porous allow water to filter down through
406-422: A strong influence on wetland water chemistry, particularly in coastal wetlands and in arid and semiarid regions with large precipitation deficits. Natural salinity is regulated by interactions between ground and surface water, which may be influenced by human activity. Carbon is the major nutrient cycled within wetlands. Most nutrients, such as sulfur , phosphorus , carbon , and nitrogen are found within
464-410: A unique kind of wetland where lush plant growth and slow decay of dead plants (under anoxic conditions) results in organic peat accumulating; bogs, fens, and mires are different names for peatlands. Variations of names for wetland systems: Some wetlands have localized names unique to a region such as the prairie potholes of North America's northern plain, pocosins , Carolina bays and baygalls of
522-587: A valley. It dips southeast, picking up the tributary Bellas Brook, and then flows in a northeasterly direction for several miles. Along the way, the creek passes Short Mountain and receives the tributary South Brook, along with numerous other tributaries. At Flat Top, it turns north for a few miles, receiving the tributary White Creek. The creek's valley becomes shallower and it receives the tributary North Fork Mehoopany Creek. It then turns northeast and enters Mehoopany Township . The creek meanders for several miles through this township before reaching its confluence with
580-515: A wetland is "an ecosystem that arises when inundation by water produces soils dominated by anaerobic and aerobic processes, which, in turn, forces the biota, particularly rooted plants, to adapt to flooding". Sometimes a precise legal definition of a wetland is required. The definition used for regulation by the United States government is: 'The term "wetlands" means those areas that are inundated or saturated by surface or ground water at
638-422: A wetland system includes its plants ( flora ) and animals ( fauna ) and microbes (bacteria, fungi). The most important factor is the wetland's duration of flooding. Other important factors include fertility and salinity of the water or soils. The chemistry of water flowing into wetlands depends on the source of water, the geological material that it flows through and the nutrients discharged from organic matter in
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#1732801326778696-403: A wetland) affects hydro-periods (temporal fluctuations in water levels) by controlling the water balance and water storage within a wetland. Landscape characteristics control wetland hydrology and water chemistry. The O 2 and CO 2 concentrations of water depend upon temperature , atmospheric pressure and mixing with the air (from winds or water flows). Water chemistry within wetlands
754-558: A whole. To replace these wetland ecosystem services , enormous amounts of money would need to be spent on water purification plants, dams, levees, and other hard infrastructure, and many of the services are impossible to replace. Floodplains and closed-depression wetlands can provide the functions of storage reservoirs and flood protection. The wetland system of floodplains is formed from major rivers downstream from their headwaters . "The floodplains of major rivers act as natural storage reservoirs, enabling excess water to spread out over
812-594: A wide area, which reduces its depth and speed. Wetlands close to the headwaters of streams and rivers can slow down rainwater runoff and spring snowmelt so that it does not run straight off the land into water courses. This can help prevent sudden, damaging floods downstream." Notable river systems that produce wide floodplains include the Nile River , the Niger river inland delta, the Zambezi River flood plain,
870-636: Is a township in Sullivan County , Pennsylvania , United States. The population was 626 at the 2020 census. The village of Lopez is located in the township. The Clemuel Ricketts Mansion was added to the National Register of Historic Places in 1983. According to the United States Census Bureau , the township has a total area of 59.2 square miles (153 km ), of which 58.25 square miles (150.9 km )
928-516: Is a distinct semi-aquatic ecosystem whose groundcovers are flooded or saturated in water , either permanently, for years or decades, or only seasonally. Flooding results in oxygen -poor ( anoxic ) processes taking place, especially in the soils . Wetlands form a transitional zone between waterbodies and dry lands , and are different from other terrestrial or aquatic ecosystems due to their vegetation 's roots having adapted to oxygen-poor waterlogged soils . They are considered among
986-440: Is determined by the pH , salinity , nutrients, conductivity , soil composition, hardness , and the sources of water. Water chemistry varies across landscapes and climatic regions. Wetlands are generally minerotrophic (waters contain dissolved materials from soils) with the exception of ombrotrophic bogs that are fed only by water from precipitation. Because bogs receive most of their water from precipitation and humidity from
1044-412: Is hydrology, or flooding . The duration of flooding or prolonged soil saturation by groundwater determines whether the resulting wetland has aquatic, marsh or swamp vegetation . Other important factors include soil fertility, natural disturbance, competition, herbivory , burial, and salinity. When peat from dead plants accumulates, bogs and fens develop. Wetland hydrology is associated with
1102-412: Is in three counties: Sullivan County, Wyoming County, and Bradford County . The watershed of Mehoopany Creek is forested. Lakes and swamps are present in its upper reaches. One lake in the watershed is Grant Lake, which has a surface area of 68.8 acres. There are a number of communities in the watershed of Mehoopany Creek. In 1921, the largest were Mehoopany, with a population of 648; Ricketts, with
1160-515: Is land and 0.95 square miles (2.5 km ) (1.63%) is water. Colley Township is bordered by Bradford County to the north, Wyoming and Luzerne Counties to the east, Davidson Township to the southwest, and Laporte and Cherry Townships to the west. Colley Township is home to the Clemuel Ricketts Mansion on Ganoga Lake , listed on the National Register of Historic Places , and part of Ricketts Glen State Park . At
1218-573: Is suitable for intermediate and novice canoers . The creek is easier to canoe on in its lower reaches than in its upper reaches and the scenery on the creek is described as "good". The American Whitewater Association's difficulty ranking of the creek ranges from I to III during normal flow conditions. Mehoopany Creek flows through Pennsylvania State Game Lands in many places. 41°34′26″N 76°03′31″W / 41.5739°N 76.0587°W / 41.5739; -76.0587 Colley Township, Sullivan County, Pennsylvania Colley Township
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#17328013267781276-451: Is the only place in the world where both crocodiles and alligators coexist. The saltwater crocodile inhabits estuaries and mangroves. Snapping turtles also inhabit wetlands. Birds , particularly waterfowl and waders use wetlands extensively. Mammals of wetlands include numerous small and medium-sized species such as voles , bats , muskrats and platypus in addition to large herbivorous and apex predator species such as
1334-545: Is usually saturated with water". More precisely, wetlands are areas where "water covers the soil , or is present either at or near the surface of the soil all year or for varying periods of time during the year, including during the growing season". A patch of land that develops pools of water after a rain storm would not necessarily be considered a "wetland", even though the land is wet. Wetlands have unique characteristics: they are generally distinguished from other water bodies or landforms based on their water level and on
1392-433: The 2010 census there were 694 people, 214 households, and 116 families living in the township. The population density was 11.9 people per square mile (4.65/km ). There were 640 housing units at an average density of 11/sq mi (4.3/km ). The racial makeup of the township was 76.7% White, 21.6% African American, 0.4% Native American, 1.2% Asian, and 0.1% from two or more races. Hispanic or Latino of any race were 5.8%. Of
1450-505: The Millennium Ecosystem Assessment from 2005. Methods exist for assessing wetland ecological health . These methods have contributed to wetland conservation by raising public awareness of the functions that wetlands can provide. Since 1971, work under an international treaty seeks to identify and protect " wetlands of international importance ." A simplified definition of wetland is "an area of land that
1508-688: The Pantanal in South America, and the Sundarbans in the Ganges - Brahmaputra delta. Wetlands contribute many ecosystem services that benefit people. These include for example water purification , stabilization of shorelines, storm protection and flood control . In addition, wetlands also process and condense carbon (in processes called carbon fixation and sequestration ), and other nutrients and water pollutants . Wetlands can act as
1566-444: The atmosphere , their water usually has low mineral ionic composition. In contrast, wetlands fed by groundwater or tides have a higher concentration of dissolved nutrients and minerals. Fen peatlands receive water both from precipitation and ground water in varying amounts so their water chemistry ranges from acidic with low levels of dissolved minerals to alkaline with high accumulation of calcium and magnesium . Salinity has
1624-576: The beavers , coypu , swamp rabbit , Florida panther , jaguar , and moose . Wetlands attract many mammals due to abundant seeds, berries, and other vegetation as food for herbivores, as well as abundant populations of invertebrates, small reptiles and amphibians as prey for predators. Invertebrates of wetlands include aquatic insects such as dragonflies , aquatic bugs and beetles , midges, mosquitos , crustaceans such as crabs, crayfish, shrimps, microcrustaceans, mollusks like clams, mussels, snails and worms. Invertebrates comprise more than half of
1682-512: The 179 households 14.0% had children under the age of 18 living with them, 44.1% were married couples living together, 5.0% had a female householder with no husband present, and 46.4% were non-families. 38.5% of households were one person and 23.5% were one person aged 65 or older. The average household size was 2.03 and the average family size was 2.69. The age distribution was 28.9% under the age of 18, 26.3% from 18 to 24, 11.6% from 25 to 44, 13.8% from 45 to 64, and 19.5% 65 or older. The median age
1740-471: The 214 households 12.6% had children under the age of 18 living with them, 45.3% were married couples living together, 5.6% had a female householder with no husband present, and 45.8% were non-families. 40.2% of households were one person and 22.4% were one person aged 65 or older. The average household size was 1.94 and the average family size was 2.57. The age distribution was 16.9% under the age of 18, 65.7% from 18 to 64, and 17.4% 65 or older. The median age
1798-568: The Hollywood Film, Pajama Party. At the 2000 census there were 647 people, 179 households, and 95 families living in the township. The population density was 11.2 people per square mile (4.3/km ). There were 542 housing units at an average density of 9.3/sq mi (3.6/km ). The racial makeup of the township was 70.48% White, 20.87% African American, 0.93% Native American, 0.15% Asian, 4.17% from other races, and 3.40% from two or more races. Hispanic or Latino of any race were 7.57%. Of
Mehoopany Creek - Misplaced Pages Continue
1856-639: The Okavango River inland delta, the Kafue River flood plain, the Lake Bangweulu flood plain (Africa), Mississippi River (US), Amazon River (South America), Yangtze River (China), Danube River (Central Europe) and Murray-Darling River (Australia). Groundwater replenishment can be achieved for example by marsh , swamp , and subterranean karst and cave hydrological systems. The surface water visibly seen in wetlands only represents
1914-522: The Southeastern US, mallines of Argentina, Mediterranean seasonal ponds of Europe and California, turloughs of Ireland, billabongs of Australia, among many others. Wetlands are found throughout the world in different climates. Temperatures vary greatly depending on the location of the wetland. Many of the world's wetlands are in the temperate zones , midway between the North or South Poles and
1972-700: The Susquehanna River near the community of North Mehoopany. Mehoopany Creek joins the Susquehanna River 231.52 miles (372.60 km) upstream of its mouth. Tributaries of Mehoopany Creek include Stony Brook , North Fork Mehoopany Creek, and numerous others. North Fork Mehoopany Creek joins Mehoopany Creek 6.26 miles (10.07 km) upstream of its mouth and its watershed has an area of 40.00 square miles (103.6 km). Stony Brook joins Mehoopany Creek 12.20 miles (19.63 km) upstream of its mouth. The watershed of this brook has an area of 6.87 square miles (17.8 km). The average rate of precipitation in
2030-502: The US, the best known classifications are the Cowardin classification system and the hydrogeomorphic (HGM) classification system. The Cowardin system includes five main types of wetlands: marine (ocean-associated), estuarine (mixed ocean- and river-associated), riverine (within river channels), lacustrine (lake-associated) and palustrine (inland nontidal habitats). Peatlands are
2088-610: The United States' commercial fish and shellfish stocks depend solely on estuaries to survive. Amphibians such as frogs and salamanders need both terrestrial and aquatic habitats in which to reproduce and feed. Because amphibians often inhabit depressional wetlands like prairie potholes and Carolina bays, the connectivity among these isolated wetlands is an important control of regional populations. While tadpoles feed on algae, adult frogs forage on insects. Frogs are sometimes used as an indicator of ecosystem health because their thin skin permits absorption of nutrients and toxins from
2146-534: The dominant plants and the source of the water. For example, marshes are wetlands dominated by emergent herbaceous vegetation such as reeds , cattails and sedges . Swamps are dominated by woody vegetation such as trees and shrubs (although reed swamps in Europe are dominated by reeds, not trees). Mangrove forest are wetlands with mangroves , halophytic woody plants that have evolved to tolerate salty water . Examples of wetlands classified by
2204-634: The equator. In these zones, summers are warm and winters are cold, but temperatures are not extreme. In subtropical zone wetlands, such as along the Gulf of Mexico , average temperatures might be 11 °C (52 °F). Wetlands in the tropics are subjected to much higher temperatures for a large portion of the year. Temperatures for wetlands on the Arabian Peninsula can exceed 50 °C (122 °F) and these habitats would therefore be subject to rapid evaporation. In northeastern Siberia , which has
2262-504: The following areas: According to the Ramsar Convention: The economic worth of the ecosystem services provided to society by intact, naturally functioning wetlands is frequently much greater than the perceived benefits of converting them to 'more valuable' intensive land use – particularly as the profits from unsustainable use often go to relatively few individuals or corporations, rather than being shared by society as
2320-468: The interface between truly terrestrial ecosystems and aquatic systems, making them inherently different from each other, yet highly dependent on both." In environmental decision-making, there are subsets of definitions that are agreed upon to make regulatory and policy decisions. Under the Ramsar international wetland conservation treaty , wetlands are defined as follows: An ecological definition of
2378-462: The known animal species in wetlands, and are considered the primary food web link between plants and higher animals (such as fish and birds). Depending on a wetland's geographic and topographic location, the functions it performs can support multiple ecosystem services , values, or benefits. United Nations Millennium Ecosystem Assessment and Ramsar Convention described wetlands as a whole to be of biosphere significance and societal importance in
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2436-438: The most biologically diverse of all ecosystems, serving as habitats to a wide range of aquatic and semi-aquatic plants and animals , with often improved water quality due to plant removal of excess nutrients such as nitrates and phosphorus . Wetlands exist on every continent , except Antarctica . The water in wetlands is either freshwater , brackish or saltwater . The main types of wetland are defined based on
2494-837: The plants and animals controlled by the wetland hydrology are often additional components of the definitions. Wetlands can be tidal (inundated by tides) or non-tidal. The water in wetlands is either freshwater , brackish , saline , or alkaline . There are four main kinds of wetlands – marsh , swamp , bog , and fen (bogs and fens being types of peatlands or mires ). Some experts also recognize wet meadows and aquatic ecosystems as additional wetland types. Sub-types include mangrove forests , carrs , pocosins , floodplains , peatlands, vernal pools , sinks , and many others. The following three groups are used within Australia to classify wetland by type: Marine and coastal zone wetlands, inland wetlands and human-made wetlands. In
2552-429: The soil and underlying rock into aquifers which are the source of much of the world's drinking water . Wetlands can also act as recharge areas when the surrounding water table is low and as a discharge zone when it is high. Mangroves , coral reefs , salt marsh can help with shoreline stabilization and storm protection. Tidal and inter-tidal wetland systems protect and stabilize coastal zones. Coral reefs provide
2610-537: The soil of wetlands. Anaerobic and aerobic respiration in the soil influences the nutrient cycling of carbon, hydrogen, oxygen, and nitrogen, and the solubility of phosphorus thus contributing to the chemical variations in its water. Wetlands with low pH and saline conductivity may reflect the presence of acid sulfates and wetlands with average salinity levels can be heavily influenced by calcium or magnesium. Biogeochemical processes in wetlands are determined by soils with low redox potential. The life forms of
2668-412: The soils and plants at higher elevations. Plants and animals may vary within a wetland seasonally or in response to flood regimes. There are four main groups of hydrophytes that are found in wetland systems throughout the world. Submerged wetland vegetation can grow in saline and fresh-water conditions. Some species have underwater flowers, while others have long stems to allow the flowers to reach
2726-530: The sources of water include tidal wetlands , where the water source is ocean tides ); estuaries , water source is mixed tidal and river waters; floodplains , water source is excess water from overflowed rivers or lakes; and bogs and vernal ponds , water source is rainfall or meltwater . The world's largest wetlands include the Amazon River basin , the West Siberian Plain ,
2784-406: The spatial and temporal dispersion, flow, and physio-chemical attributes of surface and ground waters. Sources of hydrological flows into wetlands are predominantly precipitation , surface water (saltwater or freshwater), and groundwater. Water flows out of wetlands by evapotranspiration , surface flows and tides , and subsurface water outflow. Hydrodynamics (the movement of water through and from
2842-719: The surface of the water. When trees and shrubs comprise much of the plant cover in saturated soils, those areas in most cases are called swamps . The upland boundary of swamps is determined partly by water levels. This can be affected by dams Some swamps can be dominated by a single species, such as silver maple swamps around the Great Lakes . Others, like those of the Amazon basin , have large numbers of different tree species. Other examples include cypress ( Taxodium ) and mangrove swamps. Many species of fish are highly dependent on wetland ecosystems. Seventy-five percent of
2900-496: The surface. Submerged species provide a food source for native fauna, habitat for invertebrates, and also possess filtration capabilities. Examples include seagrasses and eelgrass . Floating water plants or floating vegetation are usually small, like those in the Lemnoideae subfamily (duckweeds). Emergent vegetation like the cattails ( Typha spp.), sedges ( Carex spp.) and arrow arum ( Peltandra virginica ) rise above
2958-464: The surrounding environment resulting in increased extinction rates in unfavorable and polluted environmental conditions. Reptiles such as snakes , lizards , turtles , alligators and crocodiles are common in wetlands of some regions. In freshwater wetlands of the Southeastern US, alligators are common and a freshwater species of crocodile occurs in South Florida. The Florida Everglades
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#17328013267783016-474: The two highest priority sites in the [Sullivan] county" according to their listing in the Sullivan County Natural Areas Inventory. These headwaters are a wetland complex, which contains several rare plant species. However, the wetlands are mostly dominated by blueberry plants. The headwaters of Mehoopany Creek are home to three plant species that are rare or endangered in Pennsylvania. Mehoopany Creek
3074-440: The types of plants that live within them. Specifically, wetlands are characterized as having a water table that stands at or near the land surface for a long enough period each year to support aquatic plants . A more concise definition is a community composed of hydric soil and hydrophytes . Wetlands have also been described as ecotones , providing a transition between dry land and water bodies. Wetlands exist "...at
3132-420: The watershed in this period. Logging has been done near the headwaters of the creek. Mehoopany Creek and its drainage basin is designated as a high-quality coldwater fishery in Sullivan County. A total of 9.8 miles (15.8 km) of the creek are stocked with fish. However, native trout are also present in the watershed, especially in the tributary Stony Brook. The headwaters of Mehoopany Creek are "one of
3190-529: The watershed of Mehoopany Creek is described as "rough and hilly" in a 1921 book. The watershed has numerous steep hills, with heights from 900 to 1,000 feet (270 to 300 m). The creek's channel is sinuous . The creek has alluvial floodplains in its lower reaches. Mehoopany Creek flows through rock formations of shale and sandstone . Mehoopany Creek has "dangerously situated strainers" and major rapids in places. The watershed of Mehoopany Creek has an area of 123 square miles (320 km). The watershed
3248-439: The watershed of Mehoopany Creek ranges from 35 to 45 inches (89 to 114 cm) per year. Mehoopany Creek is acidic in early spring. The elevation near the mouth of Mehoopany Creek is 604 feet (184 m) above sea level . The elevation of the creek's source is between 2,040 feet (620 m) and 2,080 feet (630 m). Its elevation decreases at a rate of 88 feet (27 m) per mile in its upper reaches. The topography of
3306-623: Was 22 years. For every 100 females, there were 158.8 males. For every 100 females age 18 and over, there were 144.7 males. The median household income was $ 23,542 and the median family income was $ 33,333. Males had a median income of $ 28,036 versus $ 20,417 for females. The per capita income for the township was $ 10,979. About 3.0% of families and 45.6% of the population were below the poverty line , including none of those under age 18 and 17.9% of those age 65 or over. 41°31′30″N 76°14′44″W / 41.52500°N 76.24556°W / 41.52500; -76.24556 Wetland A wetland
3364-489: Was 25.3 years. The median household income was $ 30,096 and the median family income was $ 35,208. Males had a median income of $ 23,750 versus $ 40,250 for females. The per capita income for the township was $ 14,243. About 19.5% of families and 31.5% of the population were below the poverty line , including 20.2% of those under age 18 and 30.1% of those age 65 or over. Pajamas made in the Lopez Factories were used in
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