The Waccamaw River is a blackwater river that runs for 140 miles from North Carolina to South Carolina, eventually empties into the Atlantic Ocean. Updated daily.
Total streamflow across the
Waccamaw River
was last observed at
238
cfs, and is expected to yield approximately
472
acre-ft of water today; about 17%
of normal.
River levels are low and may signify a drought.
Average streamflow for this time of year is
1,375 cfs,
with recent peaks last observed
on
2018-09-22 when daily discharge volume was observed at
126,300 cfs.
Maximum discharge along the river is currently at the
Waccamaw River At Conway Marina At Conway
reporting a streamflow rate of 2,260 cfs.
This is also the highest stage along the Waccamaw River, with a gauge stage of
6.61 ft at this location.
This river is monitored from 3 different streamgauging stations along the Waccamaw River, the highest being situated at an altitude of 42 ft, the
Waccamaw River At Conway Marina At Conway.
| Last Updated | 2025-11-14 |
| Discharge Volume | 472 ACRE-FT |
| Streamflow |
238.0 cfs
-14.0 cfs (-5.56%) |
| Percent of Normal | 17.31% |
| Maximum |
126,300.0 cfs
2018-09-22 |
| Seasonal Avg | 1,375 cfs |
| Streamgauge | Streamflow | Gauge Stage | 24hr Change (%) | % Normal | Minimum (cfs) | Maximum (cfs) | Air Temp | Elevation |
|---|---|---|---|---|---|---|---|---|
|
Waccamaw River At Conway Marina At Conway
USGS 02110704 |
2260 cfs | 6.61 ft | -1.74 | |||||
|
Waccamaw River Near Longs
USGS 02110500 |
238 cfs | 3.62 ft | -5.56 | |||||
|
Waccamaw River At Freeland
USGS 02109500 |
121 cfs | 4.24 ft | -12.32 |
The Waccamaw River is a river, approximately 140 miles (225 km) long, in southeastern North Carolina and eastern South Carolina in the United States. It drains an area of approximately 1110 square miles (2886 km²) in the coastal plain along the eastern border between the two states into the Atlantic Ocean. Along its upper course, it is a slow-moving, blackwater river surrounded by vast wetlands, passable only by shallow-draft watercraft such as canoe. Along its lower course, it is lined by sandy banks and old plantation houses, providing an important navigation channel with a unique geography, flowing roughly parallel to the coast.