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Mill Creek (Reilly Creek Tributary)
Mill Creek is a tributary of Reilly Creek in Luzerne County, Pennsylvania, in the United States. It is approximately long and flows through Dennison Township. The creek flows through a number of ponds, at least one of which has a dam. There are relatively few roads in the watershed of the creek and the significant majority of the watershed is forested land. The creek is named, but has not been assessed. Course Mill Creek begins in southeastern Dennison Township, not far from the community of White Haven. It flows north-northwest for a short distance before turning west-northwest for more than a mile, passing through a large pond and then a much smaller pond. The creek eventually turns abruptly north for a few tenths of a mile and then turns north-northwest, passing through Bryants Pond and meandering between Pine Mountain and Maple Ridge. A short distance further downstream, it reaches its confluence with Reilly Creek. Tributaries Mill Creek was no named tributaries. However, i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Creasy Creek
Creasy Creek is a tributary of Nescopeck Creek in Luzerne County, Pennsylvania, in the United States. It is approximately long and flows through Dennison Township. The watershed of the creek has an area of . The creek ranges from very slightly acidic to very slightly alkaline. It is considered to be a High-Quality Coldwater Fishery (although it was a Coldwater Fishery in the past) and Class A Wild Trout Waters. Creasy Creek has one named tributary and at least one unnamed tributary. Course Creasy Creek begins in a valley in eastern Dennison Township. It flows south for a short distance and almost immediately receives an unnamed tributary. It then turns south-southwest for two miles or so before turning west-southwest and then south-southwest. The creek then crosses Pennsylvania Route 437 and turns west, receiving the tributary Reilly Creek. After approximately a mile it turns southwest and after a few tenths of a mile reaches its confluence with Nescopeck Creek at Olympus Pond. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Catskill Formation
The Devonian Catskill Formation or the Catskill Clastic wedge is a unit of mostly terrestrial sedimentary rock found in Pennsylvania and New York. Minor marine layers exist in this thick rock unit (up to ). It is equivalent to the Hampshire Formation of Maryland, West Virginia, and Virginia. The Catskill is the largest bedrock unit of the Upper Devonian in northeast Pennsylvania and the Catskill region of New York, from which its name is derived. The Pocono Mountains of Pennsylvania are largely underlain by this unit as well. The rocks of the Catskill are predominantly red sandstone indicating a large scale terrestrial deposition during the Acadian orogeny. Many beds are cyclical in nature, preserving the record of a dynamic environment during its approximately 20 million years of deposition. Depositional environment During the Devonian period, the Catskill Delta was formed by a series of river deltas and otherwise marshy terrain. This terrain was sandwiched between the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Long Hollow (Oley Creek)
Long Hollow (historically known as Long Hollow Run) is a tributary of Catawissa Creek in Columbia County, Pennsylvania, in the United States. It is approximately long and flows through Roaring Creek Township and Beaver Township. The watershed of the stream has an area of . The stream has a neutral pH and is considered to be a coldwater fishery. The main rock formations in the stream's watershed are the Mauch Chunk Formation, the Spechty Kopf Formation, the Pocono Formation, and the Buddys Run Member of the Catskill Formation. Course Long Hollow begins on Catawissa Mountain in Roaring Creek Township. It flows east for a few tenths of a mile. The stream then enters Beaver Township. It continues east and after a sort distance, the stream receives an unnamed tributary. It then continues roughly east for considerably more than a mile in a deep valley. At the end of the valley, the stream reaches its confluence with Catawissa Creek. Long Hollow joins Catawissa Creek upstream of it ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Forest
A forest is an area of land dominated by trees. Hundreds of definitions of forest are used throughout the world, incorporating factors such as tree density, tree height, land use, legal standing, and ecological function. The United Nations' Food and Agriculture Organization (FAO) defines a forest as, "Land spanning more than 0.5 hectares with trees higher than 5 meters and a canopy cover of more than 10 percent, or trees able to reach these thresholds ''in situ''. It does not include land that is predominantly under agricultural or urban use." Using this definition, '' Global Forest Resources Assessment 2020'' (FRA 2020) found that forests covered , or approximately 31 percent of the world's land area in 2020. Forests are the predominant terrestrial ecosystem of Earth, and are found around the globe. More than half of the world's forests are found in only five countries (Brazil, Canada, China, Russia, and the United States). The largest share of forests (45 percent) are in th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Local Road
The road hierarchy categorizes roads according to their functions and capacities. While sources differ on the exact nomenclature, the basic hierarchy comprises freeways, arterials, collectors, and local roads. Generally, the functional hierarchy can more or less correspond to the hierarchy of roads by their owner or administrator. The related concept of access management aims to provide access to land development, while ensuring traffic flows freely and safely on surrounding roads. General classification Controlled-access highway At the top of the hierarchy in terms of traffic flow and speed are controlled-access highways; their defining characteristic is the ''control of access'' to and from the road, meaning that the road cannot be directly accessed from properties or other roads, but only from specific connector roads. This indirection, in conjunction with high speed limits and multiple lanes, allows these roads to support fast traffic flow with high volume, in both urb ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
State Route
A state highway, state road, or state route (and the equivalent provincial highway, provincial road, or provincial route) is usually a road that is either ''numbered'' or ''maintained'' by a sub-national state or province. A road numbered by a state or province falls below numbered national highways (Canada being a notable exception to this rule) in the hierarchy (route numbers are used to aid navigation, and may or may not indicate ownership or maintenance). Roads maintained by a state or province include both nationally numbered highways and un-numbered state highways. Depending on the state, "state highway" may be used for one meaning and "state road" or "state route" for the other. In some countries such as New Zealand, the word "state" is used in its sense of a sovereign state or country. By this meaning a state highway is a road maintained and numbered by the national government rather than local authorities. Countries Australia Australia's State Route system covers ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Drainage Basin
A drainage basin is an area of land where all flowing surface water converges to a single point, such as a river mouth, or flows into another body of water, such as a lake or ocean. A basin is separated from adjacent basins by a perimeter, the '' drainage divide'', made up of a succession of elevated features, such as ridges and hills. A basin may consist of smaller basins that merge at river confluences, forming a hierarchical pattern. Other terms for a drainage basin are catchment area, catchment basin, drainage area, river basin, water basin, and impluvium. In North America, they are commonly called a watershed, though in other English-speaking places, "watershed" is used only in its original sense, that of a drainage divide. In a closed drainage basin, or endorheic basin, the water converges to a single point inside the basin, known as a sink, which may be a permanent lake, a dry lake, or a point where surface water is lost underground. Drainage basins are similar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Susquehanna River Basin Commission
The Susquehanna River Basin Commission (SRBC) is a federal-interstate compact commission created by the Susquehanna River Basin Compact (Pub. L. 91-575) between three U.S states: (Pennsylvania, New York, and Maryland), and the federal government, and signed into law by President Richard Nixon on Christmas Eve 1970 to be effective 30 days later on January 23, 1971. The Compact In the late 1960s, a broad group of concerned citizens saw the need for a federal-interstate coordinating agency to lead the conservation, development, and administration of the Basin's resources that would preserve and enhance its value as a scenic and recreational asset for the people who live in the Basin. The need to coordinate these efforts, along with those of three states and the agencies of the federal government, led to the drafting of thSusquehanna River Basin Compact which was signed into law on December 24, 1970. The Compact, as adopted by the Congress of the United States, and the legislatures of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
