Watershed-Based Plans

The Cacapon River, located in the Appalachian Mountains of West Virginia's Eastern Panhandle region, is an 81.0-mile-long shallow river known for its fishing, boating, wildlife, hunting, and wilderness scenery. As part of the Potomac River watershed, it is an American Heritage 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 Elk River is a tributary of the Kanawha River, 172 miles (277 km) long, in central West Virginia in the United States. Via the Kanawha and Ohio rivers, it is part of the watershed of the Mississippi River. The Elk 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.

The Gauley River is a 105-mile-long (169 km) river in West Virginia. It merges with the New River to form the Kanawha River, a tributary of the Ohio River. The river features numerous recreational whitewater areas, including those in Gauley River National Recreation Area downstream of the Summersville Dam. The Gauley rises in the Monongahela National Forest on Gauley Mountain in Pocahontas County as three streams, the North, Middle, and South Forks, each of which flows across the southern extremity of Randolph County; they converge in Webster County. The river then flows generally west-southwestwardly through Webster, Nicholas and Fayette counties, past the towns of Camden-on-Gauley and Summersville, to the town of Gauley Bridge, where it joins the New River to form the Kanawha River. Via the Kanawha and Ohio rivers, it is part of the Mississippi River watershed.

The Guyandotte River is a tributary of the Ohio River, approximately 166 mi long, in southwestern West Virginia in the United States. It was named after the French term for the Wendat Native Americans. Via the Ohio River, it is part of the Mississippi River watershed. The Guyandotte River is formed in southwestern Raleigh County by the confluence of three streams, Winding Gulf, Stonecoal Creek, and the Devils Fork. The Guyandotte flows initially west-northwestwardly into Wyoming and Mingo counties. It turns briefly northward in Mingo County and enters Logan County, where it turns north-northwestwardly for the remainder of its highly meandering course through Logan, Lincoln and Cabell counties. It enters the Ohio River from the south at Huntington, about 5 mi east of the city's downtown.

Potts Creek and Sweet Spring Creek watersheds are tributaries of the James River in West Virginia. The West Virginia portion of the James River watershed lies entirely within Monroe County and encompasses approximately 71square miles. These two creeks are at the headwaters of the James River watershed. The remainder of the James River watershed is located in the state of Virginia and drains into the Chesapeake Bay.

The Monongahela River, often referred to locally as the Mon, is a 130-mile-long river on the Allegheny Plateau in north-central West Virginia and 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.

The South Branch Potomac River has its headwaters in northwestern Highland County, Virginia near Hightown along the eastern edge of the Allegheny Front. After a river distance of 139 miles, the mouth of the South Branch lies east of Green Spring in Hampshire County, West Virginia where it meets the North Branch Potomac River to form the Potomac.

Tug Fork

The Tug Fork is a tributary of the Big Sandy River, 159 miles long, in southwestern West Virginia, southwestern Virginia, and eastern Kentucky in the United States. Via the Big Sandy and Ohio rivers, it is part of the watershed of the Mississippi River. The Tug Fork rises in the Appalachian Mountains of extreme southwestern West Virginia, in southern McDowell County, near the Virginia state line. It flows in a meandering course through the mountains generally northwest, past Welch. Approximately 20 miles northwest of Welch, it briefly forms approximately 4 miles of the state line between West Virginia (northeast) and Virginia (southwest). For the remainder of its course it forms part of the boundary between West Virginia (east) and Kentucky (west), flowing northwest past Williamson, West Virginia. It joins the Levisa Fork at Louisa, Kentucky to form the Big Sandy.

The West Fork River is a principal tributary of the Monongahela River, 103-mile long, in north-central West Virginia, United States. Via the Monongahela and Ohio Rivers, it is part of the watershed of the Mississippi River, draining an area of 881 square miles on the unglaciated portion of the Allegheny Plateau.