Total streamflow across the
Cannonball River
was last observed at
140
cfs, and is expected to yield approximately
278
acre-ft of water today; about 131%
of normal.
River levels are high.
Average streamflow for this time of year is
107 cfs,
with recent peaks last observed
on
2019-03-29 when daily discharge volume was observed at
26,030 cfs.
Maximum discharge along the river is currently at the
Cannonball River At Breien
reporting a streamflow rate of 95.8 cfs.
However, the streamgauge with the highest stage along the river is the
Cannonball River At Regent
with a gauge stage of 4.85 ft.
This river is monitored from 3 different streamgauging stations along the Cannonball River, the highest being situated at an altitude of 2,436 ft, the
Cannonball River At Regent.
| Last Updated | 2025-11-26 |
| Discharge Volume | 278 ACRE-FT |
| Streamflow |
140.14 cfs
+12.55 cfs (+9.84%) |
| Percent of Normal | 131.28% |
| Maximum |
26,030.0 cfs
2019-03-29 |
| Seasonal Avg | 107 cfs |
| Streamgauge | Streamflow | Gauge Stage | 24hr Change (%) | % Normal | Minimum (cfs) | Maximum (cfs) | Air Temp | Elevation |
|---|---|---|---|---|---|---|---|---|
|
Cannonball River At Regent
USGS 06350000 |
5 cfs | 4.85 ft | -3.01 | |||||
|
Cannonball River Nr Raleigh
USGS 06351200 |
40 cfs | 2.42 ft | 13.51 | |||||
|
Cannonball River At Breien
USGS 06354000 |
96 cfs | 2.68 ft | 9.11 |
The Cannonball River (Lakota: Íŋyaŋwakağapi Wakpá) is a tributary of the Missouri River, approximately 135 mi (217 km) long, in southwestern North Dakota in the United States.It rises in the Little Missouri National Grassland, in the badlands north of Amidon in northern Slope County. It flows ESE past New England, Mott, and Burt. It is joined by Cedar Creek approximately 15 mi (24 km) southwest of Shields and flows northeast, past Shields, forming the northern border of Sioux County and the Standing Rock Indian Reservation. It joins the Missouri in Lake Oahe near Cannon Ball. The cannonball concretions found in the vicinity of this river are the source of its name.