Total streamflow across the
Guyandotte River
was last observed at
1,090
cfs, and is expected to yield approximately
2,162
acre-ft of water today; about 69%
of normal.
River levels are low and may signify a drought.
Average streamflow for this time of year is
1,583 cfs,
with recent peaks last observed
on
2015-03-05 when daily discharge volume was observed at
30,900 cfs.
Maximum discharge along the river is currently at the
Guyandotte River At Man
reporting a streamflow rate of 968 cfs.
This is also the highest stage along the Guyandotte River, with a gauge stage of
6.12 ft at this location.
This river is monitored from 3 different streamgauging stations along the Guyandotte River, the highest being situated at an altitude of 1,139 ft, the
Guyandotte River Near Baileysville.
| Last Updated | 2025-12-05 |
| Discharge Volume | 2,162 ACRE-FT |
| Streamflow |
1,090.0 cfs
-88.0 cfs (-7.47%) |
| Percent of Normal | 68.86% |
| Maximum |
30,900.0 cfs
2015-03-05 |
| Seasonal Avg | 1,583 cfs |
| Streamgauge | Streamflow | Gauge Stage | 24hr Change (%) | % Normal | Minimum (cfs) | Maximum (cfs) | Air Temp | Elevation |
|---|---|---|---|---|---|---|---|---|
|
Guyandotte River Near Baileysville
USGS 03202400 |
200 cfs | 3.43 ft | -22.18 | |||||
|
Guyandotte River At Man
USGS 03203000 |
968 cfs | 6.12 ft | ||||||
|
Guyandotte River At Logan
USGS 03203600 |
890 cfs | 5.88 ft | -3.37 |
The Guyandotte River is a tributary of the Ohio River, approximately 166 mi (267 km) long, in southwestern West Virginia in the United States. It was named after the French term for the Wendat Native Americans. It drains an area of the unglaciated Allegheny Plateau south of the Ohio between the watersheds of the Kanawha River to the northeast and Twelvepole Creek and the Big Sandy River to the southwest. Via the Ohio River, it is part of the Mississippi River watershed.