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The Dry Fork is a 39.1-mile-long (62.9 km) [2] 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 quality of the surface water resources of the New River has been studied in recent years by both the State of West Virginia and New River Gorge Park Resource Management staff. Data from these studies suggest the presence of metals, organic contaminants and influx of raw sewage are common in many tributaries of the New River.
The Coal River is a tributary of the Kanawha River in southern West Virginia. It is formed near the community of Alum Creek by the confluence of the Big and Little Coal Rivers, and flows generally northward through western Kanawha County, past the community of Upper Falls and into the Kanawha River at St. Albans.
The Kanawha River (/ k ə ˈ n ɔː ə / kə-NAW-ə) is a tributary of the Ohio River, approximately 97 mi (156 km) long, in the U.S. state of West Virginia.The largest inland waterway in West Virginia, its watershed has been a significant industrial region of the state since early in the 19th century.
A USGS stream gauge on the creek near Richwood recorded a mean annual discharge of 233.6 cu ft/s (6.61 m 3 /s) during water years 1945-2019. The highest annual mean discharge during the period was 318 cu ft/s (9.0 m 3 /s) in water year 1979, and the lowest was 126.2 cu ft/s (3.57 m 3 /s) in water year 1999.
Geologic Map of West Virginia. West Virginia's geologic history stretches back into the Precambrian, and includes several periods of mountain building and erosion. At times, much of what is now West Virginia was covered by swamps, marshlands, and shallow seas, accounting for the wide variety of sedimentary rocks found in the state, as well as its wealth of coal and natural gas deposits.
High flow areas of Deckers Creek. Deckers Creek is a 24.6-mile-long (39.6 km) [1] tributary of the Monongahela River that runs through north-central West Virginia.It begins west of Arthurdale and flows southeast, then north, then northwest towards Morgantown, where it empties into the Monongahela River. [2]
The environment of West Virginia encompasses terrain and ecosystems ranging from plateaus to mountains. Most of West Virginia lies within the Appalachian mixed mesophytic forests ecoregion , while the higher elevations along the eastern border and in the panhandle lie within the Appalachian-Blue Ridge forests .