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2026-01-04T17:00:00-07:00

The National Weather Service in Denver has issued a Fire Weather Watch for wind and low relative humidity, which is in effect from Sunday morning through Sunday afternoon. * AFFECTED AREA...Fire Weather Zones 214, 216, 239, 240 and 241. * TIMING...From late Sunday morning through Sunday afternoon. * WINDS...West 10 to 20 mph with gusts 30 to 45 mph. * RELATIVE HUMIDITY...12 to 18%. * IMPACTS...Conditions will be favorable for rapid fire spread. Avoid outdoor burning and any activity that may produce a spark and start a wildfire.


Kanawha River River Levels

Last Updated: January 2, 2026

The Kanawha River is a tributary of the Ohio River, running 97 miles through West Virginia.


Summary

Total streamflow across the Kanawha River was last observed at 14,710 cfs, and is expected to yield approximately 29,177 acre-ft of water today; about 38% of normal. River levels are low and may signify a drought. Average streamflow for this time of year is 38,424 cfs, with recent peaks last observed on 2019-02-25 when daily discharge volume was observed at 237,000 cfs.

Maximum discharge along the river is currently at the Kanawha River At Charleston reporting a streamflow rate of 8,440 cfs. This is also the highest stage along the Kanawha River, with a gauge stage of 18.17 ft at this location. This river is monitored from 2 different streamgauging stations along the Kanawha River, the highest being situated at an altitude of 622 ft, the Kanawha River At Kanawha Falls.

River Details

Last Updated 2026-01-02
Discharge Volume 29,177 ACRE-FT
Streamflow 14,710.0 cfs
-2620.0 cfs (-15.12%)
Percent of Normal 38.28%
Maximum 237,000.0 cfs
2019-02-25
Seasonal Avg 38,424 cfs
       
River Streamflow Levels
Streamgauge Streamflow Gauge Stage 24hr Change (%) % Normal Minimum (cfs) Maximum (cfs) Air Temp Elevation
Kanawha River At Kanawha Falls
USGS 03193000
6270 cfs 4.14 ft -13.28
Kanawha River At Charleston
USGS 03198000
8440 cfs 18.17 ft -16.44
Seasonal Discharge Comparison
Maximum Streamflow Discharge
Streamflow Elevation Profile

The Kanawha River ( 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 valley has been a significant industrial region of the state since early in the 19th century.
It is formed at the town of Gauley Bridge in northwestern Fayette County, approximately 35 mi (56 km) SE of Charleston, by the confluence of the New and Gauley rivers. It flows generally northwest, in a winding course on the unglaciated Allegheny Plateau, through Fayette, Kanawha, Putnam, and Mason counties, past the cities of Charleston and St. Albans, and numerous smaller communities. It joins the Ohio at Point Pleasant.
Paleo-Indians, the earliest indigenous peoples, lived in the valley and the heights by 10,000 BC as evidenced by archaeological artifacts such as Clovis points. A succession of prehistoric cultures developed, with the Adena culture beginning the construction of numerous skilled earthwork mounds and enclosures more than 2000 years ago. Some of the villages of the Fort Ancient culture survived into the times of European contact.
The area was a place of competition among historical American Indian nations. Invading from their base in present-day New York, the Iroquois drove out or conquered Fort Ancient culture peoples, as well as such tribes as the Huron and Conoy. By right of conquest, the Iroquois, Lenape (Delaware), and Shawnee reserved the area as a hunting ground. They resisted European-American settlement during the colonial years.
The river valley contains significant deposits of coal and natural gas. In colonial times, the wildly fluctuating level of the river prevented its use for transportation. The removal of boulders and snags on the lower river in the 1840s allowed navigation, which was extended upriver after the construction of locks and dams starting in 1875. The river is now navigable to Deepwater, an unincorporated community about 20 miles (32 km) upriver from Charleston. A thriving chemical industry along its banks provides a significant part of the local economy.