Guyandotte River

About

Guyandotte River, West Virginia — 1861 Salt Boom, 1980 R.D. Bailey Lake, Raleigh Logan. The Guyandotte carries a class I-III rating and a workable flow window of 575 to 1,750 CFS, measured at USGS gauge 03203600, which reports a mean discharge of 1,157 CFS. The river drains 1,670 square miles of the unglaciated Allegheny Plateau, winding north and west through Raleigh, Wyoming, Mingo, Logan, and Cabell Counties before reaching the Ohio River at Huntington. This is old, folded country, and the river reflects it.

Long before surveyors arrived, the Guyandotte flowed through the ancestral territory of the Shawnee, the Mingo, the Cherokee, the Seneca, the Wyandot, the Delaware, the Muncie, the Ottawa, and the Mohican. The river served as a primary travel corridor, hunting ground, and gathering place. A framework of cession treaties — the 1744 Treaty of Lancaster, the 1768 Treaty of Fort Stanwix, the 1770-1795 Treaty of Greenville, the 1817 Treaty of Fort Meigs, and the 1866 Treaty with the Seneca, Shawnee, and Quapaw — reshaped who governed these valleys. The Eastern Band of Cherokee Indians, the Absentee-Shawnee Tribe, the Eastern Shawnee Tribe, the Shawnee Tribe, and the Delaware Tribe maintain cultural connections to the watershed today.

The river's defining early chapter is the 1857-1861 salt boom, when extensive dams were built to power salt furnaces. According to the e-WV encyclopedia, the dams were improperly placed, and the same 1861 flood that ended the navigation project destroyed the salt works forever. The industry that followed was timber. From the 1800s through the 1920s, the Guyandotte was logged to feed West Virginia's hardwood trade — oak, poplar, cherry, walnut, ash, and maple — with log drives running the river and Wyoming County sawmills cutting through stands that supplied the gun-stock and furniture industries. The 1920s exhaustion of the cherry and poplar stands, the 1925 start of state forestry conservation, and the 1930s creation of national forests ended large-scale logging.

Coal came next. From the 1880s into the 1940s, the West Virginia coal industry dominated the region, using the Guyandotte watershed's tributaries to feed the Chesapeake & Ohio Railway. The pressure on the river accumulated across a century of logging, mining, agricultural, and industrial impacts — the same pressure that later drove the 1972-2000 Clean Water Act assessments and the WVDEP's modern Total Maximum Daily Load program.

The modern era of engineering finally succeeded where the nineteenth century had failed. In 1980, the U.S. Army Corps of Engineers completed R.D. Bailey Lake, a flood-control impoundment on the upper Guyandotte that transformed the river's lower hydrology. That reservoir now anchors the R.D. Bailey Lake Wildlife Management Area, making the once-untamable river a centerpiece of recreation and conservation. Since 2010, the WVDEP and Guyandotte River Watershed partnerships have addressed those hundred years of impacts through streambank stabilization, native fish restocking — including muskellunge, walleye, and the endangered diamond darter — and Abandoned Mine Lands restoration. Designated a water trail under the Great Kanawha Resource Conservation and Development program, the Guyandotte today carries the Guyandotte Water Trail and supports smallmouth bass and walleye fishing along its length.