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The Elk River is a tributary of
the Kanawha River, 172 miles long, in central West Virginia. Via
the Kanawha and Ohio Rivers, it is part of the watershed of the Mississippi
River.
Course
The Elk is the longest river in West
Virginia which flows entirely within the state's boundaries.
It is formed in the Allegheny
Mountains in Pocahontas County by the confluence of two
short streams, the Big Spring Fork and the Old Field Fork,
which join near the community of Slatyfork. It flows above ground for
several miles before it sinks into a network of caverns and flows
underground for more than five miles. The old riverbed of solid rock,
however, remains above ground in this section known as "The
Dries."
It follows a generally westward
course across the unglaciated Allegheny Plateau, through Randolph,
Webster, Braxton, Clay, and Kanawha Counties,
past the towns of Webster Springs, Sutton, Gassaway,
Clay, Clendenin, and Elkview before joining the Kanawha
River at Charleston.
At Sutton, a U.S. Army
Corps of Engineers dam causes the Elk to form Sutton Lake.
The Elk's largest tributaries are the
Holly River and the Birch River, both of which join it
in Braxton County.
The upper portion of the river, above
Sutton Lake, is a popular coldwater trout stream. Below Sutton
Lake, it is a high-gradient warmwater fishery well-known for its
muskellunge, walleye and smallmouth bass fishing.
Variant
names
According to the Geographic Names
Information System, the Elk River has also been known
historically as:
- Pe-quo-ni
- Pe-quo-ni-cepe
- Pequoni
- Tis-chil-waugh
- Tiskelewah
- Tiskelwah
- To-que-man
- To-qui-min-cepe
References
- Columbia Gazetteer of North
America entry
- DeLorme (1997). West Virginia
Atlas & Gazetteer. Yarmouth, Maine: DeLorme. ISBN
0-89933-246-3.
- GNIS entry
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