Cross Run
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Cross Run
Cross Run is a tributary of Catawissa Creek in Luzerne County, Pennsylvania, in the United States. It is approximately long and flows through Hazle Township. The stream is in the United States Geological Survey quadrangle of Conyngham. The stream has two reservoirs on it and has been used as a water supply for Hazleton since at least the late 1800s or early 1900s. Both of the stream's reservoirs have dams. The stream has one unnamed tributary. Cross Run and its unnamed tributary are considered by the Pennsylvania Department of Environmental Protection to be impaired for part of their lengths. Course Cross Run begins immediately east of Pismire Ridge in Hazle Township. The stream flows west-southwest for several hundred feet. It then turns south and after a few hundred feet enters a reservoir. At the southwestern corner of the reservoir, the stream passes through the Upper Mount Pleasant Dam and almost immediately turns southeast, entering a second reservoir after a few hundred f ...
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Susquehanna River
The Susquehanna River (; Lenape: Siskëwahane) is a major river located in the Mid-Atlantic region of the United States, overlapping between the lower Northeast and the Upland South. At long, it is the longest river on the East Coast of the United States. By watershed area, it is the 16th-largest river in the United States,Susquehanna River Trail
Pennsylvania Fish and Boat Commission, accessed March 25, 2010.
Susquehanna River
, Green Works Radio, accessed March 25, 2010.
and also the longest river in ...
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Ravine
A ravine is a landform that is narrower than a canyon and is often the product of streambank erosion.Definition of "ravine"
at
Ravines are typically classified as larger in scale than , although smaller than s. Ravines may also be called a cleuch, dell, ghout (),
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Rivers Of Luzerne 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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List Of Tributaries Of Catawissa Creek
Catawissa Creek is a long creek flowing into the Susquehanna River with 26 named tributaries, of which 19 are direct tributaries. The creek flows through Luzerne, Schuylkill, and Columbia counties in Pennsylvania. The two shortest tributaries are approximately long, while the longest is about in length. The tributaries include seventeen runs, six creeks, and three hollows (unnamed streams named after named valleys that they flow through). By length, the five largest tributaries of Catawissa Creek are Little Catawissa Creek, Tomhicken Creek, Scotch Run, Beaver Run, and Messers Run. By watershed area, the five largest tributaries are Tomhicken Creek, Little Catawissa Creek, Beaver Run, Scotch Run, and Messers Run. Various species of fish inhabit most of the tributaries of Catawissa Creek. The Pennsylvania Department of Environmental Protection considers eleven tributaries of the creek to be Coldwater Fisheries.Coldwater Fishery is an official designation that means that a s ...
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Hunkydory Creek
Hunkydory Creek is a tributary of Catawissa Creek in Schuylkill County and Luzerne County, in Pennsylvania, in the United States. It is approximately long and flows through Kline Township in Schuylkill County and Hazle Township in Luzerne County. The watershed of the creek has an area of . The creek is considered to be a Coldwater Fishery. It is likely that it is not inhabited by any species of fish. The main rock formations in the creek's watershed are the Mauch Chunk Formation, the Pottsville Formation, and the Llwellyn Formation and the main soils are the Udorthents Kill soil and the Hezleton soil. Course Hunkydory Creek begins at the Number Eight Reservoir in Kline Township, Schuylkill County. It flows north for several dozen feet before turning west-northwest for a few tenths of a mile. The creek then turns north and a few tenths of a mile further downstream, it exits Kline Township and Schuylkill County. Upon exiting Kline Township and Schuylkill County, Hunkydory Creek e ...
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Spies Run
Spies Run is a tributary of Catawissa Creek in Schuylkill County, Pennsylvania, in the United States. It is approximately long and flows through East Union Township. The stream has a pH that is fairly close to neutral. The stream is in the United States Geological Survey quadrangle of Conyngham. Trout naturally reproduce in it. Course Spies Run begins on a mountain in East Union Township, a few hundred feet from the border between East Union Township and Kline Township. It flows northwest in a narrow valley for several tenths of a mile. The stream then receives an unnamed tributary and turns north-northwest, entering a much broader valley. After a few tenths of a mile, it turns northwest and crosses a road. Within several hundred feet, the stream reaches its confluence with Catawissa Creek. Spies Run arrives at its confluence with Catawissa Creek upstream of the mouth of the creek. Hydrology Spies Run is described as a "clean stream" in the January 2013 Progress Report for the ...
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Total Maximum Daily Load
A total maximum daily load (TMDL) is a regulatory term in the U.S. Clean Water Act, describing a plan for restoring impaired waters that identifies the maximum amount of a pollutant that a body of water can receive while still meeting water quality standards. State and federal agency responsibilities The Clean Water Act requires that state environmental agencies complete TMDLs for impaired waters and that the United States Environmental Protection Agency (EPA) review and approve / disapprove those TMDLs. Because both state and federal governments are involved in completing TMDLs, the TMDL program is an example of cooperative federalism. If a state doesn't take action to develop TMDLs, or if EPA disapproves state-developed TMDLs, the EPA is responsible for issuing TMDLs. EPA published regulations in 1992 establishing TMDL procedures. Application of TMDLs has broadened significantly in the last decade to include many watershed-scale efforts, including the Chesapeake Bay TMDL. TMDLs ...
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Geographic Names Information System
The Geographic Names Information System (GNIS) is a database of name and locative information about more than two million physical and cultural features throughout the United States and its territories, Antarctica, and the associated states of the Marshall Islands, Federated States of Micronesia, and Palau. It is a type of gazetteer. It was developed by the United States Geological Survey (USGS) in cooperation with the United States Board on Geographic Names (BGN) to promote the standardization of feature names. Data were collected in two phases. Although a third phase was considered, which would have handled name changes where local usages differed from maps, it was never begun. The database is part of a system that includes topographic map names and bibliographic references. The names of books and historic maps that confirm the feature or place name are cited. Variant names, alternatives to official federal names for a feature, are also recorded. Each feature receives a per ...
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Drilled Well
Drilling is a cutting process where a drill bit is spun to cut a hole of circular cross-section in solid materials. The drill bit is usually a rotary cutting tool, often multi-point. The bit is pressed against the work-piece and rotated at rates from hundreds to thousands of revolutions per minute. This forces the cutting edge against the work-piece, cutting off chips (swarf) from the hole as it is drilled. In rock drilling, the hole is usually not made through a circular cutting motion, though the bit is usually rotated. Instead, the hole is usually made by hammering a drill bit into the hole with quickly repeated short movements. The hammering action can be performed from outside the hole ( top-hammer drill) or within the hole (down-the-hole drill, DTH). Drills used for horizontal drilling are called drifter drills. In rare cases, specially-shaped bits are used to cut holes of non-circular cross-section; a square cross-section is possible. Process Drilled holes are chara ...
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Water Well
A well is an excavation or structure created in the ground by digging, driving, or drilling to access liquid resources, usually water. The oldest and most common kind of well is a water well, to access groundwater in underground aquifers. The well water is drawn up by a pump, or using containers, such as buckets or large water bags that are raised mechanically or by hand. Water can also be injected back into the aquifer through the well. Wells were first constructed at least eight thousand years ago and historically vary in construction from a simple scoop in the sediment of a dry watercourse to the qanats of Iran, and the stepwells and sakiehs of India. Placing a lining in the well shaft helps create stability, and linings of wood or wickerwork date back at least as far as the Iron Age. Wells have traditionally been sunk by hand digging, as is still the case in rural areas of the developing world. These wells are inexpensive and low-tech as they use mostly manual labour, ...
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Water Supply
Water supply is the provision of water by public utilities, commercial organisations, community endeavors or by individuals, usually via a system of pumps and pipes. Public water supply systems are crucial to properly functioning societies. These systems are what supply drinking water to populations around the globe. Aspects of service quality include continuity of supply, water quality and water pressure. The institutional responsibility for water supply is arranged differently in different countries and regions (urban versus rural). It usually includes issues surrounding policy and regulation, service provision and standardization. The cost of supplying water consists, to a very large extent, of fixed costs (capital costs and personnel costs) and only to a small extent of variable costs that depend on the amount of water consumed (mainly energy and chemicals). Almost all service providers in the world charge tariffs to recover part of their costs. Water supply is a separate ...
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Dreck Creek
Yiddish words used in the English language include both words that have been assimilated into Englishused by both Yiddish and English speakersand many that have not. An English sentence that uses either may be described by some as Yinglish (or Hebronics), though a secondary sense of the term ''Yinglish'' describes the distinctive way certain Jews in English-speaking countries add many Yiddish words into their conversation, beyond general Yiddish words and phrases used by English speakers. In this meaning, Yinglish is not the same as Yeshivish, which is spoken by many Orthodox Jews, though the two share many parallels. Yiddish Many of these words have not been assimilated into English and are unlikely to be understood by English speakers who do not have substantial Yiddish knowledge. Leo Rosten's book ''The Joys of Yiddish'' explains these words (and many more) in detail. With the exceptions of ''blintz'', ''kosher'' (used in English slang), and ''shmo'', none of the other words ...
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