Windfall Run
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Windfall Run
Windfall Run is a tributary of Baker Run in Wyoming County, Pennsylvania, in the United States. It is approximately long and flows through Noxen Township. The watershed of the stream has an area of . The stream itself is classified as Class A Wild Trout Waters by the Pennsylvania Fish and Boat Commission. The surficial geology in its vicinity includes Wisconsinan Till and bedrock. Course Windfall Run begins in a wetland on a plateau in Noxen Township. It flows north-northeast for several tenths of a mile and enters a deep valley before turning east-southeast. The stream flows in this direction for more than a mile before reaching its confluence with Baker Run. Windfall Run joins Baker Run, which is itself only long, upstream of its mouth. Hydrology The concentration of alkalinity in Windfall Run is . Geography and geology The elevation near the mouth of Windfall Run is above sea level. The elevation near the source of the stream is between above sea level. The surficial ...
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Bowman Creek
Bowman Creek (also known as Bowmans Creek or Bowman's Creek) is a tributary of the Susquehanna River in Luzerne County and Wyoming County, in Pennsylvania, in the United States. It is approximately long and flows through Ross Township and Lake Township in Luzerne County and Noxen Township, Monroe Township, and Eaton Township in Wyoming County. The watershed of the creek has an area of . The creek is not designated as an impaired waterbody and its pH is close to neutral, although it has experienced some problems with acid rain. It has low concentrations of dissolved solids like calcium. The creek is relatively small in its upper reaches, but by Noxen, its width is . It is also relatively shallow in many reaches. Rock formations in the watershed include the Catskill Formation, the Huntley Mountain Formation, Burgoon Sandstone, the Mauch Chunk Formation, the Pottsville Group, and the Pocono Formation. Soil associations in the creek's watershed include the Wellsboro-Morris-Oquaga assoc ...
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Surficial Geology
Superficial deposits (or surficial deposits) refer to geological deposits typically of Quaternary age (less than 2.6 million years old). These geologically recent unconsolidated sediments may include stream channel and floodplain deposits, beach sands, talus gravels and glacial drift and moraine. All pre-Quaternary deposits are referred to as bedrock. Types and history There are several types of superficial deposit, including raised beaches and brickearth. These were formed in periods of climate change during the ice ages. The raised beaches were generally formed during periods of higher sea level, when ice sheets were at a minimum, and the sand and shingle deposits can be seen in many low cliffs. The brickearth is originally a wind-blown dust deposited under extremely cold, dry conditions but much has been re-deposited by flood water and mixed with flints. Superficial deposits were originally recorded only onshore and around the coast where they were laid down by various natu ...
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List Of Tributaries Of Bowman Creek
Bowman Creek is a long tributary of the Susquehanna River in Luzerne County and Wyoming County, in Pennsylvania, in the United States. It has 26 named tributaries, of which 21 are direct tributaries and 5 are sub-tributaries. These include nineteen runs, six creeks, and one hollow (a stream that does not have a name of its own, but takes the name of the valley through which it flows). By length, the tributaries range from the long Benson Hollow and Wolf Run to the long Leonard Creek and Beaver Run. By watershed area, they range from for Wolf Run and Sugar Run to for Roaring Run and Leonard Creek. The major tributaries of Bowman Creek include Sugar Hollow Creek, Marsh Creek, Leonard Creek, Roaring Run, and Beaver Run. Although the watershed of Bowman Creek largely consists of forested land, residential and commercial land infringes upon the floodplains of several tributaries: Marsh Creek, Leonard Creek, South Run, and Beaver Run. Bowman Creek's main stem is design ...
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List Of Rivers Of Pennsylvania
This is a list of streams and rivers in the U.S. state of Pennsylvania. By drainage basin This list is arranged by drainage basin, with respective tributaries indented under each larger stream's name. Delaware Bay Chesapeake Bay *''Elk River (MD)'' **Big Elk Creek **Little Elk Creek *''North East River (MD) **North East Creek *Gunpowder River Susquehanna River *Susquehanna River ** Deer Creek **Octoraro Creek *** West Branch Octoraro Creek **** Stewart Run *** East Branch Octoraro Creek **** Muddy Run ** Conowingo Creek ** Fishing Creek (Lancaster County) **Muddy Creek (Susquehanna River tributary) ***North Branch Muddy Creek *** South Branch Muddy Creek ** Tucquan Creek ** Otter Creek **Pequea Creek *** Big Beaver Creek ***Little Beaver Creek ** Conestoga River *** Little Conestoga Creek *** Mill Creek *** Lititz Run ***Cocalico Creek ****Hammer Creek **** Middle Creek **** Indian Run **** Little Cocalico Creek ***Muddy Creek (Conestoga River tributary) **** Little ...
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Brook Trout
The brook trout (''Salvelinus fontinalis'') is a species of freshwater fish in the char genus ''Salvelinus'' of the salmon family Salmonidae. It is native to Eastern North America in the United States and Canada, but has been introduced elsewhere in North America, as well as to Iceland, Europe, and Asia. In parts of its range, it is also known as the eastern brook trout, speckled trout, brook charr, squaretail, brookie or mud trout, among others. A potamodromous population in Lake Superior, as well as an anadromous population in Maine, is known as coaster trout or, simply, as coasters. The brook trout is the state fish of nine U.S. states: Michigan, New Hampshire, New Jersey, New York, North Carolina, Pennsylvania, Vermont, Virginia, and West Virginia, and the Provincial Fish of Nova Scotia in Canada. Systematics and taxonomy The brook trout was first scientifically described as ''Salmo fontinalis'' by the naturalist Samuel Latham Mitchill in 1814. The specific epithet "''fontina ...
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Trout
Trout are species of freshwater fish belonging to the genera '' Oncorhynchus'', ''Salmo'' and ''Salvelinus'', all of the subfamily Salmoninae of the family Salmonidae. The word ''trout'' is also used as part of the name of some non-salmonid fish such as ''Cynoscion nebulosus'', the spotted seatrout or speckled trout. Trout are closely related to salmon and char (or charr): species termed salmon and char occur in the same genera as do fish called trout (''Oncorhynchus'' – Pacific salmon and trout, ''Salmo'' – Atlantic salmon and various trout, ''Salvelinus'' – char and trout). Lake trout and most other trout live in freshwater lakes and rivers exclusively, while there are others, such as the steelhead, a form of the coastal rainbow trout, that can spend two or three years at sea before returning to fresh water to spawn (a habit more typical of salmon). Arctic char and brook trout are part of the char genus. Trout are an important food source for humans and wildlife, ...
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Pennsylvania State Game Lands Number 57
Pennsylvania (; (Pennsylvania Dutch: )), officially the Commonwealth of Pennsylvania, is a state spanning the Mid-Atlantic, Northeastern, Appalachian, and Great Lakes regions of the United States. It borders Delaware to its southeast, Maryland to its south, West Virginia to its southwest, Ohio to its west, Lake Erie and the Canadian province of Ontario to its northwest, New York to its north, and the Delaware River and New Jersey to its east. Pennsylvania is the fifth-most populous state in the nation with over 13 million residents as of 2020. It is the 33rd-largest state by area and ranks ninth among all states in population density. The southeastern Delaware Valley metropolitan area comprises and surrounds Philadelphia, the state's largest and nation's sixth most populous city. Another 2.37 million reside in Greater Pittsburgh in the southwest, centered around Pittsburgh, the state's second-largest and Western Pennsylvania's largest city. The state's subsequent five m ...
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Public Property
Public property is property that is dedicated to public use. The term may be used either to describe the use to which the property is put, or to describe the character of its ownership (owned collectively by the population of a state). This is in contrast to private property, owned by an individual person or artificial entities that represent the financial interests of persons, such as corporations. State ownership, also called public ownership, government ownership or state property, are property interests that are vested in the state, rather than an individual or communities. Differences from private property In a paper by Armen A. Alchian, he explored what distinguishes public property from private property, concluding that a unique difference lies in the limitations put on its alienability. That is, a crucial feature of public property lies in the inability of their owners to sell or grant them to others. According to Alchian, private property is that which can be transferr ...
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Quadrangle (geography)
A "quadrangle" is a topographic map produced by the United States Geological Survey (USGS) covering the United States. The maps are usually named after local physiographic features. The shorthand "quad" is also used, especially with the name of the map; for example, "the Ranger Creek, Texas quad". From approximately 1947-1992, the USGS produced the 7.5 minute series, with each map covering an area one-quarter of the older 15-minute quad series, which it replaced. A 7.5 minute quadrangle map covers an area of . Both map series were produced via photogrammetric analysis of aerial photography using stereoplotters supplemented by field surveys. These maps employ the 1927 North American Datum (NAD27); conversion or a change in settings is necessary when using a GPS which by default employ the WGS84 geodetic datum. Beginning in 2009, the USGS made available digital versions of 7.5 minute quadrangle maps based on GIS data that use the NAD83 datum, which is typically within one meter of ...
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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 ...
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Shale
Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4) and tiny fragments (silt-sized particles) of other minerals, especially quartz and calcite.Blatt, Harvey and Robert J. Tracy (1996) ''Petrology: Igneous, Sedimentary and Metamorphic'', 2nd ed., Freeman, pp. 281–292 Shale is characterized by its tendency to split into thin layers ( laminae) less than one centimeter in thickness. This property is called '' fissility''. Shale is the most common sedimentary rock. The term ''shale'' is sometimes applied more broadly, as essentially a synonym for mudrock, rather than in the more narrow sense of clay-rich fissile mudrock. Texture Shale typically exhibits varying degrees of fissility. Because of the parallel orientation of clay mineral flakes in shale, it breaks into thin layers, often splintery and usually parallel to the otherwise indistinguishable beddin ...
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Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ...
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