Total streamflow across the
Nolichucky River
was last observed at
3,150
cfs, and is expected to yield approximately
6,248
acre-ft of water today; about 54%
of normal.
River levels are low and may signify a drought.
Average streamflow for this time of year is
5,836 cfs,
with recent peaks last observed
on
2020-02-07 when daily discharge volume was observed at
98,300 cfs.
Maximum discharge along the river is currently at the
Nolichucky River At Embreeville
reporting a streamflow rate of 2,020 cfs.
However, the streamgauge with the highest stage along the river is the
Nolichucky River Below Nolichucky Dam
with a gauge stage of 42.3 ft.
This river is monitored from 3 different streamgauging stations along the Nolichucky River, the highest being situated at an altitude of 1,533 ft, the
Nolichucky River At Embreeville.
Last Updated | 2025-04-30 |
Discharge Volume | 6,248 ACRE-FT |
Streamflow |
3,150.0 cfs
-280.0 cfs (-8.16%) |
Percent of Normal | 53.98% |
Maximum |
98,300.0 cfs
2020-02-07 |
Seasonal Avg | 5,836 cfs |
The Nolichucky River is a 115-mile (185 km) river that flows through Western North Carolina and East Tennessee, in the southeastern United States. Traversing the Pisgah National Forest and the Cherokee National Forest in the Blue Ridge Mountains, the river's watershed is home to some of the highest mountains in the Appalachians, including Mount Mitchell, the highest point in the eastern United States. The river is a tributary of the French Broad River, and is impounded by Nolichucky Dam near Greeneville, Tennessee.