The West Branch Lackawanna River (also known as Ball Creek ) is a tributary of the Lackawanna River in Susquehanna County, Pennsylvania , in the United States. It is approximately 9.5 miles (15.3 km) long and flows through Ararat Township , Herrick Township , and Union Dale . The watershed of the river has an area of 16.8 square miles (44 km). The river is not designated as an impaired stream and it has a high level of water quality . Lakes and wetlands in the river's watershed include Ball Lake, Fiddle Lake, Hathaway Lake, Lake Romobe, Lewis Lake, Lowe Lake, and Sink Hole Swamp. The river is also dammed by at least two dams: the Romobe Lake Dam and the Hathaway Pond Dam.
84-454: The West Branch Lackawanna River is a second-order stream. Its watershed is narrow and largely undeveloped. The Delaware and Hudson Railway historically followed the river for some distance and a number of bridges have also been constructed over it. The river is designated as a Coldwater Fishery and a Migratory Fishery. Both brook trout and brown trout inhabit it and the river was historically stocked with trout as well. Recreational opportunities in
168-402: A fuse plug . If present, the fuse plug is designed to wash out in case of a large flood, greater than the discharge capacity of the spillway gates. Although many months may be needed for construction crews to restore the fuse plug and channel after such an operation, the total damage and cost to repair is less than if the main water-retaining structures had been overtopped. The fuse plug concept
252-711: 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
336-537: A "significant" hazard. A 1921 book described the topography in the watershed of the West Branch Lackawanna River as "rough and mountainous". The watershed contains a narrow valley bordered by steep hills. Ponds, lakes, and swamps occur throughout the watershed, which has been affected by glaciation . The channel of the West Branch Lackawanna River is sinuous and flows through rock formations consisting of sandstone and shale . The watershed of
420-554: A 1999 stream survey. Additionally, there was no trash along its banks . The streambanks are stable in most reaches, but there is slight erosion in a few places. There is a concrete spillway at the outflow of Hathaway Lake. The Romobe Lake Dam is located on the river. As of 1980, it is in poor condition. Additionally, the Hathaway Pond Dam is located 3,000 feet (910 m) downriver of the Romobe Lake Dam and has been labelled
504-443: A baffle of concrete blocks but usually have a "flip lip" and/or dissipator basin, which creates a hydraulic jump , protecting the toe of the dam from erosion. Stepped channels and spillways have been used for over 3,000 years. Despite being superseded by more modern engineering techniques such as hydraulic jumps in the mid twentieth century, since around 1985 interest in stepped spillways and chutes has been renewed, partly due to
588-463: A few dams lack overflow spillways and rely entirely on bottom outlets. The two main types of spillways are controlled and uncontrolled. A controlled spillway has mechanical structures or gates to regulate the rate of flow. This design allows nearly the full height of the dam to be used for water storage year-round, and flood waters can be released as required by opening one or more gates. An uncontrolled spillway, in contrast, does not have gates; when
672-402: 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
756-576: A north-south direction. It is in the extreme northeast of the Lackawanna River watershed and mainly occupies Herrick Township and Ararat Township. A smaller part of the watershed is in Union Dale and an even smaller part is in Clifford Township . The watershed of the West Branch Lackawanna River is largely undeveloped, with farms, small communities, and residential areas. Dairy farms occur within
840-565: A plunge pool, or two ski jumps can direct their water discharges to collide with one another. Third, a stilling basin at the terminus of a spillway serves to further dissipate energy and prevent erosion. They are usually filled with a relatively shallow depth of water and sometimes lined with concrete. A number of velocity-reducing components can be incorporated into their design to include chute blocks, baffle blocks, wing walls, surface boils, or end sills. Spillway gates may operate suddenly without warning, under remote control. Trespassers within
924-1248: 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
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#17328517030941008-540: 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
1092-403: A protective barrier to coastal shoreline. Mangroves stabilize the coastal zone from the interior and will migrate with the shoreline to remain adjacent to the boundary of the water. The main conservation benefit these systems have against storms and storm surges is the ability to reduce the speed and height of waves and floodwaters. Spillway A spillway is a structure used to provide
1176-423: A roughly southerly direction for a few miles, crossing Pennsylvania Route 374 and entering Union Dale. In Union Dale, the river continues to flow south, receiving Fiddle Lake Creek, its only named tributary, from the right after several tenths of a mile. A few tenths of a mile further downstream, it enters Stillwater Lake and reaches its confluence with the Lackawanna River. The West Branch Lackawanna River joins
1260-419: A spillway to regulate downstream flow—by releasing water in a controlled manner before the reservoir is full, operators can prevent an unacceptably large release later. Other uses of the term "spillway" include bypasses of dams and outlets of channels used during high water, and outlet channels carved through natural dams such as moraines . Water normally flows over a spillway only during flood periods, when
1344-422: 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
1428-410: 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
1512-508: 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
1596-422: 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
1680-403: 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
1764-558: 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
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#17328517030941848-577: 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,
1932-509: Is 1190910. The river is also known as Ball Creek. This name appears on a United States Geological Survey map of Susquehanna County dating to 1944. However, in 1968, David G. Lappin of the United States Geological Survey was unable to verify the variant name. Several locals who were questioned had never heard the river being called "Ball Creek". The Newburg Turnpike, one of the earliest roads in its vicinity, historically crossed
2016-425: Is a reach where it has cloudy waters due to siltation caused by cows in the river. Two small pipes made of PVC discharge clear water into the river at road crossings. However, the source of these pipes is unknown. On November 10, 1950, the discharge of the West Branch Lackawanna River near Union Dale was measured to be 22.6 cubic feet per second. In the early 1900s, the average annual rate of precipitation in
2100-460: Is designed like an inverted bell , where water can enter around the entire perimeter. These uncontrolled spillways are also called morning glory (after the flower ), or glory hole spillways. In areas where the surface of the reservoir may freeze, this type of spillway is normally fitted with ice-breaking arrangements to prevent the spillway from becoming ice-bound. Some bell-mouth spillways are gate-controlled. The highest morning glory spillway in
2184-440: 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
2268-629: Is either freshwater , brackish or saltwater . The main types of wetland are defined based on 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
2352-412: 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
2436-517: Is not designated as an impaired stream. The water quality of the river was described as "good to excellent" in the Lackawanna River Watershed Conservation Plan. However, dairy farming in the watershed and fecal contaminants in some source ponds have caused some concern. In most reaches, the West Branch Lackawanna River has relatively clear waters. However, approximately 7.25 miles (11.67 km) upriver of its mouth, there
2520-443: Is set by dam safety guidelines, based on the size of the structure and the potential loss of human life or property downstream. The United States Army Corps of Engineers bases their requirements on the probable maximum flood (PMF) and the probable maximum precipitation (PMP). The PMP is the largest precipitation thought to be physically possible in the upstream watershed. Dams of lower hazard may be allowed to have an IDF less than
2604-451: 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
West Branch Lackawanna River - Misplaced Pages Continue
2688-604: Is used where building a spillway with the required capacity would be costly. A chute spillway is a common and basic design that transfers excess water from behind the dam down a smooth decline into the river below. These are usually designed following an ogee curve . Most often, they are lined on the bottom and sides with concrete to protect the dam and topography. They may have a controlling device and some are thinner and multiply-lined if space and funding are tight. In addition, they are not always intended to dissipate energy like stepped spillways. Chute spillways can be ingrained with
2772-545: 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
2856-492: 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
2940-666: 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
3024-466: The United States Army Corps of Engineers in 1960. Source ponds in the river's watershed include Ball Lake, Fiddle Lake, Hathaway Lake, Lake Romobe, Lewis Lake, Lowe Lake, and Sink Hole Swamp. The headwaters of the river are in small lakes and swamps upstream of Hathaway Lake. A swamp known as Pine Swamp is in the watershed. No debris was observed in the West Branch Lackawanna River during
3108-444: 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
3192-576: 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
3276-607: 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 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
3360-574: The Lackawanna River 40.32 miles (64.89 km) upriver of its mouth. The West Branch Lackawanna River has one named tributary, which is known as Fiddle Lake Creek. Fiddle Lake Creek joins the West Branch Lackawanna River 1.20 miles (1.93 km) upriver of its mouth. Its watershed has an area of 6.47 square miles (16.8 km). Other unnamed tributaries include "Unnamed trib 1", "Unnamed trib 2", and "Ball Lake Creek". Their lengths are 1.6 miles (2.6 km), 1.3 miles (2.1 km), and 1.9 miles (3.1 km), respectively. The West Branch Lackawanna River
3444-550: The Lackawanna River. The West Branch Lackawanna River has a small population of wild brook trout and brown trout . It has also been stocked , but this has ceased due to property conflicts. The Herrick Township Swamp, which is in the watershed of the West Branch Lackawanna River, is designated as an Important Bird Area by the Audubon Society . The Lake Romobe area, which is also in the river's watershed, holds this designation. There are some green algae growths on rocks in
West Branch Lackawanna River - Misplaced Pages Continue
3528-619: 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
3612-460: The PMF. As water passes over a spillway and down the chute, potential energy converts into increasing kinetic energy . Failure to dissipate the water's energy can lead to scouring and erosion at the dam's toe (base). This can cause spillway damage and undermine the dam's stability. To put this energy in perspective, the spillways at Tarbela Dam could, at full capacity, produce 40,000 MW; about 10 times
3696-511: 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
3780-527: The Theta Land Company opened a section of the river to fishing by leasing them to the Pennsylvania Fish and Boat Commission for $ 1 per year. The drainage basin of the West Branch Lackawanna River is designated as a Coldwater Fishery and a Migratory Fishery. Wild trout naturally reproduce in the river from 6.70 miles (10.78 km) upriver of its mouth all the way downstream to its confluence with
3864-494: 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
3948-610: 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
4032-481: The West Branch Lackawanna River at Herrick, near where Pennsylvania Route 374 is today. In the 1800s, timbering operations came to affect lakes in the river's watershed. The area also was a host to sawmills and wood acid factories. The Delaware and Hudson Railway historically followed the West Branch Lackawanna River as far as Ararat . It left the watershed at Ararat Summit. Once the railroad arrived, industries such as dairying and ice harvesting began to occur in
4116-540: The West Branch Lackawanna River downstream of river mile 7.25. The algae possibly comes from agricultural runoff . The vegetation along the river was described in a 2002 report as "in good condition". It consisted of brush, forests, marshes/wetlands, natural fields, and pastures. An estimated 36 percent of the river had forests along its banks, 32 percent had brush, 13 percent had marshes, 10 percent had pastures, 6 percent had natural fields, and less than 2 percent had bare or compacted ground. A large hemlock forest surrounds
4200-512: The West Branch Lackawanna River has an area of 16.8 square miles (44 km). The mouth of the river is in the United States Geological Survey quadrangle of Forest City. However, its source is in the quadrangle of Thompson. The river also passes through the quadrangle of Orson. The West Branch Lackawanna River is a second-order stream. The river's watershed is relatively narrow in an east-west direction and relatively long in
4284-485: The West Branch Lackawanna River was built in 1958. It is 40.0 feet (12.2 m) long and is situated in Herrick Township. A three-span bridge of the same type was built over the river in 1961 in Union Dale and was repaired in 2010. This bridge is 202.1 feet (61.6 m) long and carries State Route 2040 / Skyline Drive. Volunteers carried out a stream survey of the West Branch Lackawanna River on May 1, 1999. In 2001,
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#17328517030944368-637: The West Branch Lackawanna River. These trails provide access for fishermen. However, much of the river's length is difficult to access due to dense vegetation and extensive posting. Pennsylvania State Game Lands Number 236 are located to the west of the West Branch Lackawanna River. These state game lands have an area of 2,009 acres (813 ha). Wetland A wetland 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
4452-476: The area. In the early 1900s, the major industries in the watershed of the West Branch Lackawanna River were mainly agriculture and ice harvesting . The river was also used as water power for some small mills at Uniondale. Around this time period, major communities in the watershed included Union Dale, Herrick Center, and Burnwood. Their populations were 355, 327, and 104, respectively. A prestressed box beam or girders bridge carrying Pennsylvania Route 374 over
4536-407: The capacity of its power plant. The energy can be dissipated by addressing one or more parts of a spillway's design. First, on the spillway surface itself by a series of steps along the spillway (see stepped spillway ). Second, at the base of a spillway, a flip bucket can create a hydraulic jump and deflect water upwards. A ski jump can direct water horizontally and eventually down into
4620-461: The controlled release of water downstream from a dam or levee , typically into the riverbed of the dammed river itself. In the United Kingdom, they may be known as overflow channels . Spillways ensure that water does not damage parts of the structure not designed to convey water. Spillways can include floodgates and fuse plugs to regulate water flow and reservoir level. Such features enable
4704-414: The difference in height between the intake and the outlet to create the pressure difference required to remove excess water. Siphons require priming to remove air in the bend for them to function, and most siphon spillways are designed to use water to automatically prime the siphon. One such design is the volute siphon, which employs volutes or fins on a funnel to form water into a vortex that draws air out of
4788-622: 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
4872-423: The flood is sometimes expressed as a return period . A 100-year recurrence interval is the flood magnitude expected to be exceeded on the average of once in 100 years. This parameter may be expressed as an exceedance frequency with a 1% chance of being exceeded in any given year. The volume of water expected during the design flood is obtained by hydrologic calculations of the upstream watershed. The return period
4956-494: 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
5040-464: 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
5124-462: 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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#17328517030945208-832: 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
5292-428: The reservoir has reached its capacity and water continues entering faster than it can be released. In contrast, an intake tower is a structure used to control water release on a routine basis for purposes such as water supply and hydroelectricity generation. A spillway is located at the top of the reservoir pool. Dams may also have bottom outlets with valves or gates which may be operated to release flood flow, and
5376-411: The reservoir is controlled by the mechanical gates. In this case, the dam is not designed to function with water flowing over the top if it, either due to the materials used for its construction or conditions directly downstream. If inflow to the reservoir exceeds the gate's capacity, an artificial channel called an auxiliary or emergency spillway will convey water. Often, that is intentionally blocked by
5460-456: The river downstream. One parameter of spillway design is the largest flood it is designed to handle. The structures must safely withstand the appropriate spillway design flood (SDF), sometimes called the inflow design flood (IDF). The magnitude of the SDF may be set by dam safety guidelines, based on the size of the structure and the potential loss of human life or property downstream. The magnitude of
5544-423: The river for 1.5 miles (2.4 km). The D&H Rail Trail passes through the watershed of the West Branch Lackawanna River. In the early 2000s, the Lackawanna River Watershed Conservation Plan recommended further improvement of this rail trail . However, it is mostly used by locals. The main stem of the river has been described as a "pristine cold-water fisher[y]". There are some trails going to and alongside
5628-429: 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
5712-537: 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
5796-412: 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
5880-515: 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 ,
5964-425: The southern end of that lake, the river flows southeast for more than a mile before turning south-southeast. After several tenths of a mile, it turns south and then south-southwest. It then flows west-southwest for a short distance before turning south-southeast and entering Herrick Township. The river passes through a wetland and continues meandering south-southeast as its valley becomes narrower. It eventually turns in
6048-406: 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
6132-414: The spillway are at high risk of drowning. Spillways are usually fenced and equipped with locked gates to prevent casual trespassing within the structure. Warning signs, sirens, and other measures may be in place to warn users of the downstream area of sudden release of water. Operating protocols may require "cracking" a gate to release a small amount of water to warn persons downstream. The sudden closure of
6216-709: 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
6300-490: 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
6384-457: 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
6468-424: The system. The priming happens automatically when the water level rises above the inlets. The ogee crest over-tops a dam, a side channel wraps around the topography of a dam, and a labyrinth uses a zig-zag design to increase the sill length for a thinner design and increased discharge. A drop inlet resembles an intake for a hydroelectric power plant, and transfers water from behind the dam directly through tunnels to
6552-440: 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
6636-474: The use of new construction materials (e.g. roller-compacted concrete , gabions ) and design techniques (e.g. embankment overtopping protection). The steps produce considerable energy dissipation along the chute and reduce the size of the required downstream energy dissipation basin. Research is still active on the topic, with newer developments on embankment dam overflow protection systems, converging spillways and small weir design. A bell-mouth spillway
6720-474: The water rises above the lip or crest of the spillway, it begins to be released from the reservoir. The rate of discharge is controlled only by the height of water above the reservoir's spillway. The fraction of storage volume in the reservoir above the spillway crest can only be used for the temporary storage of floodwater; it cannot be used as water supply storage because it sits higher than the dam can retain it. In an intermediate type, normal level regulation of
6804-582: The watershed and there is a large farm near the headwaters. The watershed is a "sensitive stream" and thus has less than 10 percent impervious cover. A wetland complex of regional significance exists in the watershed of the West Branch Lackawanna River. The West Branch Lackawanna River was entered into the Geographic Names Information System on August 2, 1979. Its identifier in the Geographic Names Information System
6888-534: The watershed include the D&H Trail and Pennsylvania State Game Lands Number 236. The West Branch Lackawanna River begins in a wetland in Ararat Township. It flows north for a few tenths of a mile before entering Sinkhole Swamp . From this point, it turns east and enters Fomobe Lake . From the southeastern part of this lake, the river flows south-southeast for a few tenths of a mile and enters Hathaway Lake . From
6972-402: The watershed of the West Branch Lackawanna River was 35 to 40 inches (89 to 102 cm). The elevation near the mouth of the West Branch Lackawanna River is 1,575 feet (480 m) above sea level . The elevation of the river's source is between 2,000 and 2,020 feet (610 and 620 m) above sea level. The mouth of the West Branch Lackawanna River is at Stillwater Dam, which was built by
7056-669: The world is at Hungry Horse Dam in Montana, U.S., and is controlled by a 64-by-12-foot (19.5 by 3.7 m) ring gate. The bell-mouth spillway in Covão dos Conchos reservoir in Portugal is constructed to look like a natural formation. The largest bell-mouth spillway is in Geehi Dam , in New South Wales, Australia, measuring 105 ft (32 m) in diameter at the lake's surface. A siphon uses
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