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Shepman Run
Shepman Run (also known as Shepmans Run) is a tributary of Little Muncy Creek in Lycoming County, Pennsylvania, in the United States. It is approximately long and flows through Moreland Township. The watershed of the stream has an area of . A covered bridge crosses the stream. Shepman Run is classified as a Coldwater Fishery and a Migratory Fishery. Course Shepman Run begins in a valley in Moreland Township. It flows east for a few tenths of a mile before turning south for several tenths of a mile. In this reach, the stream receives an unnamed tributary from the left and passes through a small pond. The stream then turns south-southwest for several tenths of a mile before reaching the end of its valley. Shortly afterwards, it turns east for a short distance before reaching its confluence with Little Muncy Creek. Shepman Run joins Little Muncy Creek upstream of its mouth. Tributaries Shepman Run has no named tributaries. However, it does have one unnamed tributary, which is l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Clarkstown, Pennsylvania
Lycoming County is a county in the Commonwealth of Pennsylvania. As of the 2020 census, the population was 114,188. Its county seat is Williamsport. Lycoming County comprises the Williamsport metropolitan statistical area. About northwest of Philadelphia and east-northeast of Pittsburgh, Lycoming is Pennsylvania's largest county by area. History Formation of the county Lycoming County was formed from Northumberland County on April 13, 1795. The county was larger than it is today. It took up most of the land that is now north central Pennsylvania. The following counties have been formed from land that was once part of Lycoming County: Armstrong, Bradford, Centre, Clearfield, Clinton, Indiana, Jefferson, McKean, Potter, Sullivan, Tioga, Venango, Warren, Forest, Elk and Cameron. Lycoming County was originally named Jefferson County in honor of Thomas Jefferson. This name proved to be unsatisfactory. The name change went through several steps. First a change to Lycomi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Mouth
A river mouth is where a river flows into a larger body of water, such as another river, a lake/reservoir, a bay/gulf, a sea, or an ocean. At the river mouth, sediments are often deposited due to the slowing of the current reducing the carrying capacity of the water. The water from a river can enter the receiving body in a variety of different ways. The motion of a river is influenced by the relative density of the river compared to the receiving water, the rotation of the earth, and any ambient motion in the receiving water, such as tides or seiches. If the river water has a higher density than the surface of the receiving water, the river water will plunge below the surface. The river water will then either form an underflow or an interflow within the lake. However, if the river water is lighter than the receiving water, as is typically the case when fresh river water flows into the sea, the river water will float along the surface of the receiving water as an overflow. Alon ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rivers Of Lycoming 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] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Laurel Run (Little Muncy Creek)
Laurel Run is a tributary of Little Muncy Creek in Columbia County and Lycoming County, in Pennsylvania, in the United States. It is approximately long and flows through Madison Township and Pine Township in Columbia County and Franklin Township and Moreland Township in Lycoming County. The watershed of the stream has an area of . It is classified as a Coldwater Fishery and a Migratory Fishery. A number of bridges have been constructed over the stream. Course Laurel Run begins in the Muncy Hills in Madison Township, Columbia County. It flows east-northeast for several tenths of a mile, heading through a small valley as it enters Pine Township, where it receives two unnamed tributaries from the right. The stream then gradually turns north-northwest for several tenths of a mile before entering Franklin Township, Lycoming County, where it receives one unnamed tributary from the left and one from the right. It then turns north for several tenths of a mile before receiving an unna ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cox Run
Cox Run is a tributary of Little Muncy Creek in Lycoming County, Pennsylvania, in the United States. It is approximately long and flows through Moreland Township, Wolf Township, and Muncy Creek Township. The watershed of the stream has an area of . Cox Run itself flows through a valley known as Neufer Hollow and is designated as a Coldwater Fishery. A streambank stabilization project along the stream was proposed in 2008. Course Cox Run begins in a valley to the east of Buck Hill in Moreland Township. It flows south for a few tenths of a mile before turning south-southwest, still flowing through its valley alongside Buck Hill. The stream then receives an unnamed tributary from the left before turning southwest for more than a mile. In this reach it flows between Buck Hill and Tommy Hill and receives another unnamed tributary from the left, passing through Wolf Township, and entering Muncy Creek Township. It eventually reaches the end of its valley and turns south-southwest, cro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lycoming College
Lycoming College is a Private college, private Liberal arts colleges in the United States, liberal arts college in Williamsport, Pennsylvania. Founded in 1812, Lycoming College is affiliated with the United Methodist Church but operates as an independent institution. Through its history, it has been an academy, seminary, junior college, and four-year college. History Lycoming College traces its roots to 1812 and the founding of the "Williamsport Academy for the Education of Youth in English and other languages, in the useful arts, science and literature". Eight spirited citizens secured the charter for the school and founded the academy to improve the educational opportunities of the community. Attendance was by subscription, although a state grant ensured that a number of underprivileged children would be taught free of charge. The academy was for boys but accepted girls in the 1830s. It was one of the early academics in Pennsylvania which placed it on the frontier of academy-b ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...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] |
Bridge
A bridge is a structure built to span a physical obstacle (such as a body of water, valley, road, or rail) without blocking the way underneath. It is constructed for the purpose of providing passage over the obstacle, which is usually something that is otherwise difficult or impossible to cross. There are many different designs of bridges, each serving a particular purpose and applicable to different situations. Designs of bridges vary depending on factors such as the function of the bridge, the nature of the terrain where the bridge is constructed and anchored, and the material used to make it, and the funds available to build it. The earliest bridges were likely made with fallen trees and stepping stones. The Neolithic people built boardwalk bridges across marshland. The Arkadiko Bridge (dating from the 13th century BC, in the Peloponnese) is one of the oldest arch bridges still in existence and use. Etymology The '' Oxford English Dictionary'' traces the origin of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
River Source
The headwaters of a river or stream is the farthest place in that river or stream from its estuary or downstream confluence with another river, as measured along the course of the river. It is also known as a river's source. Definition The United States Geological Survey (USGS) states that a river's "length may be considered to be the distance from the mouth to the most distant headwater source (irrespective of stream name), or from the mouth to the headwaters of the stream commonly known as the source stream". As an example of the second definition above, the USGS at times considers the Missouri River as a tributary of the Mississippi River. But it also follows the first definition above (along with virtually all other geographic authorities and publications) in using the combined Missouri—lower Mississippi length figure in lists of lengths of rivers around the world. Most rivers have numerous tributaries and change names often; it is customary to regard the longest ... [...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] |
