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Dolly Sods
The Dolly Sods Wilderness – originally simply Dolly Sods – is a U.S. Wilderness Area in the Allegheny Mountains of eastern West Virginia, US, and is part of the Monongahela National Forest (MNF) of the U.S. Forest Service (USFS). Dolly Sods is a rocky, high-altitude plateau with sweeping vistas and lifeforms normally found much farther north in Canada. To the north, the distinctive landscape of "the Sods" is characterized by stunted ("flagged") trees, wind-carved boulders, heath barrens, grassy meadows created in the last century by logging and fires, and sphagnum bogs that are much older. To the south, a dense cove forest occupies the branched canyon excavated by the North Fork of Red Creek. The name derives from an 18th-century German homesteading family – the Dahles – and a local term for an open mountaintop meadow – a "sods". Geography Topography Dolly Sods is the highest plateau east of the Mississippi River with altitudes ranging from 2,644 ft. (806 m) ...
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Monongahela National Forest
The Monongahela National Forest is a national forest located in the Allegheny Mountains of eastern West Virginia, USA. It protects over of federally managed land within a proclamation boundary that includes much of the Potomac Highlands Region and portions of 10 counties. The Monongahela National Forest includes some major landform features such as the Allegheny Front and the western portion of the Ridge-and-valley Appalachians. Within the forest boundaries lie some of the highest mountain peaks in the state, including the highest, Spruce Knob (4,863 ft). Spruce Knob is also the highest point in the Allegheny Mountains. Approximately 75 tree species are found in the forest. Almost all of the trees are a second growth forest, grown back after the land was heavily cutover around the start of the 20th century. Species for which the forest is important include red spruce (''Picea rubens''), balsam fir (''Abies balsamea''), and mountain ash (''Sorbus americana''). The Monong ...
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Roaring Plains West Wilderness
The Roaring Plains West Wilderness is a U.S. Wilderness Area in the Allegheny Mountains of eastern West Virginia, USA. It is part of the Monongahela National Forest and includes Mount Porte Crayon, the sixth highest point in the state. Known as "Roaring Plains West" to the advocates of a much larger area (15,138 acres) of proposed wilderness preservation, the RPW consists of set aside by the Wild Monongahela Act, which was made law on 30 March 2009. (There are also areas known as "Roaring Plains North" and "Roaring Plains East" not included in the WMA.) Along with neighboring Flatrock Plains, these areas comprise the highest plateau in the eastern United States. Geography The Roaring Plains and Flatrock Plains areas include portions of Randolph and Pendleton Counties. These high-elevation plateaux, which encompass the highest sphagnum bogs in West Virginia, consist of vast expanses of rocky, tree-studded plains surrounded by rock outcrops and cliffs offering impressive views ...
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West Virginia Highlands Conservancy
West or Occident is one of the four cardinal directions or points of the compass. It is the opposite direction from east and is the direction in which the Sun sets on the Earth. Etymology The word "west" is a Germanic word passed into some Romance languages (''ouest'' in French, ''oest'' in Catalan, ''ovest'' in Italian, ''oeste'' in Spanish and Portuguese). As in other languages, the word formation stems from the fact that west is the direction of the setting sun in the evening: 'west' derives from the Indo-European root ''*wes'' reduced from ''*wes-pero'' 'evening, night', cognate with Ancient Greek ἕσπερος hesperos 'evening; evening star; western' and Latin vesper 'evening; west'. Examples of the same formation in other languages include Latin occidens 'west' from occidō 'to go down, to set' and Hebrew מַעֲרָב maarav 'west' from עֶרֶב erev 'evening'. Navigation To go west using a compass for navigation (in a place where magnetic north is the same dire ...
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Chesapeake Bay
The Chesapeake Bay ( ) is the largest estuary in the United States. The Bay is located in the Mid-Atlantic (United States), Mid-Atlantic region and is primarily separated from the Atlantic Ocean by the Delmarva Peninsula (including the parts: the Eastern Shore of Maryland / Eastern Shore of Virginia and the state of Delaware) with its mouth of the Bay at the south end located between Cape Henry and Cape Charles (headland), Cape Charles. With its northern portion in Maryland and the southern part in Virginia, the Chesapeake Bay is a very important feature for the ecology and economy of those two states, as well as others surrounding within its watershed. More than 150 major rivers and streams flow into the Bay's drainage basin, which covers parts of six states (New York, Pennsylvania, Delaware, Maryland, Virginia and West Virginia) and all of District of Columbia. The Bay is approximately long from its northern headwaters in the Susquehanna River to its outlet in the Atlantic Ocea ...
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Potomac River
The Potomac River () drains the Mid-Atlantic United States, flowing from the Potomac Highlands into Chesapeake Bay. It is long,U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map. Retrieved August 15, 2011 with a drainage area of 14,700 square miles (38,000 km2), and is the fourth-largest river along the East Coast of the United States and the 21st-largest in the United States. Over 5 million people live within its watershed. The river forms part of the borders between Maryland and Washington, D.C. on the left descending bank and between West Virginia and Virginia on the right descending bank. Except for a small portion of its headwaters in West Virginia, the North Branch Potomac River is considered part of Maryland to the low-water mark on the opposite bank. The South Branch Potomac River lies completely within the state of West Virginia except for its headwaters, which lie in Virginia. Course The Potomac River runs ...
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Headwaters
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 t ...
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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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Ohio River
The Ohio River is a long river in the United States. It is located at the boundary of the Midwestern and Southern United States, flowing southwesterly from western Pennsylvania to its mouth on the Mississippi River at the southern tip of Illinois. It is the third largest river by discharge volume in the United States and the largest tributary by volume of the north-south flowing Mississippi River that divides the eastern from western United States. It is also the 6th oldest river on the North American continent. The river flows through or along the border of six states, and its drainage basin includes parts of 14 states. Through its largest tributary, the Tennessee River, the basin includes several states of the southeastern U.S. It is the source of drinking water for five million people. The lower Ohio River just below Louisville is obstructed by rapids known as the Falls of the Ohio where the elevation falls in restricting larger commercial navigation, although in the 18th ...
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Monongahela River
The Monongahela River ( , )—often referred to locally as the Mon ()—is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed August 15, 2011 river on the Allegheny Plateau in North Central West Virginia, north-central West Virginia and Greater Pittsburgh, Southwestern Pennsylvania. The river flows from the confluence of its west and east forks in north-central West Virginia northeasterly into southwestern Pennsylvania, then northerly to Pittsburgh and its confluence with the Allegheny River to form the Ohio River. The river's entire length is navigable via a series of locks and dams. Etymology The Unami language, Unami word ''Monongahela'' means "falling banks", in reference to the geological instability of the river's banks. Moravian Church, Moravian missionary David Zeisberger (1721–1808) gave this account of the naming: "In the Lenape language, Indian tongue the name of this river was ''Mechmenawungihilla'' (alter ...
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Cheat River
The Cheat River is a U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map , accessed August 15, 2011 tributary of the Monongahela River in eastern West Virginia and southwestern Pennsylvania in the United States. Via the Ohio River, the Cheat and Monongahela are part of the Mississippi River watershed. Owing to the ruggedness of the surrounding Allegheny Mountains, the Cheat remains largely remote with few settlements or developments along its banks. Its headwaters are in the Cheat-Potomac Ranger District of the Monongahela National Forest. Geography The Cheat is formed at Parsons, West Virginia, by the confluence of Shavers Fork and Black Fork. Black Fork is fed by the Blackwater River and by the Dry, Glady, and Laurel Forks — these are traditionally referred to as the five Forks of Cheat. (The "High Falls of Cheat" 5 feet/4.6 m highis a few miles upstream of Bemis on Shavers Fork.) From Parsons the Cheat River flows generally ...
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Black Fork (Cheat River)
The Black Fork is a principal tributary of the Cheat River in the Allegheny Mountains of eastern West Virginia, USA. It is a short stream, about four miles (6 km) in length,''The American Rivers Outstanding Rivers List'', Second Edition, May 1991. Compiled and edited by Matthew H. Huntington and John D. Echeverria. Washington, DC: American Rivers, Inc. formed by the confluence of two other streams not far above its mouth.DeLorme (1997). ''West Virginia Atlas & Gazetteer''. Yarmouth, Maine: DeLorme. . It was traditionally considered one of the five Forks of Cheat. Geography Via the Cheat, Monongahela and Ohio Rivers, it is part of the watershed of the Mississippi River, draining an area of 500 square miles (1,295 km²). The Black Fork flows for its entire length in Tucker County. It is formed at the town of Hendricks by the confluence of the Dry Fork and the Blackwater River, and flows generally northwestwardly through Hambleton to Parsons, where it joins the S ...
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Dry Fork River
The Dry Fork is a tributary of the Black Fork of the Cheat River in the Allegheny Mountains of eastern West Virginia, USA. Via the Black Fork, the Cheat, and the Monongahela and Ohio rivers, it is part of the watershed of the Mississippi River. The Dry Fork flows for much of its length in the Monongahela National Forest and drains mostly rural and forested areas.DeLorme (1997). ''West Virginia Atlas & Gazetteer''. Yarmouth, Maine: DeLorme. . It was traditionally considered one of the five Forks of Cheat. Name According to the Geographic Names Information System, Dry Fork has also been known historically as Dry Run. The stream's name derives from the occurrence of underground passages through which portions of the stream flow, leaving a dry streambed on the surface at times during the year. (See Sinks of Gandy) Geography Course The Dry Fork rises between Rich Mountain and Little Middle Mountain in eastern Randolph County and initially flows north-northeastwardly, past th ...
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