Total streamflow across the
Tongue River
was last observed at
294
cfs, and is expected to yield approximately
583
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
1,694 cfs,
with recent peaks last observed
on
2019-05-31 when daily discharge volume was observed at
24,742 cfs.
Maximum discharge along the river is currently at the
Tongue River At Monarch
reporting a streamflow rate of 383 cfs.
However, the streamgauge with the highest stage along the river is the
Tongue River At Tongue R Dam Nr Decker Mt
with a gauge stage of 10.77 ft.
This river is monitored from 8 different streamgauging stations along the Tongue River, the highest being situated at an altitude of 4,072 ft, the
Tongue River Near Dayton.
Last Updated | 2025-04-23 |
Discharge Volume | 583 ACRE-FT |
Streamflow |
294.0 cfs
-14.0 cfs (-4.55%) |
Percent of Normal | 17.35% |
Maximum |
24,742.0 cfs
2019-05-31 |
Seasonal Avg | 1,694 cfs |
Streamgauge | Streamflow | Gauge Stage | 24hr Change (%) | % Normal | Minimum (cfs) | Maximum (cfs) | Air Temp | Elevation |
---|---|---|---|---|---|---|---|---|
Tongue River Near Dayton
USGS 06298000 |
48 cfs | 1.73 ft | 0 | |||||
Tongue River At Monarch
USGS 06299980 |
383 cfs | 3.36 ft | ||||||
Tongue River At State Line Nr Decker Mt
USGS 06306300 |
294 cfs | 2.81 ft | -4.55 | |||||
Tongue River At Tongue R Dam Nr Decker Mt
USGS 06307500 |
196 cfs | 10.77 ft | 0 | |||||
Tongue R At Birney Day School Br Nr Birney Mt
USGS 06307616 |
211 cfs | 1.3 ft | 0 | |||||
Tongue R Bl Brandenberg Bridge Nr Ashland Mt
USGS 06307830 |
186 cfs | 2.82 ft | -4.12 | |||||
Tongue River At Miles City Mt
USGS 06308500 |
207 cfs | 2.26 ft | -2.82 | |||||
Tongue River At Akra
USGS 05101000 |
89 cfs | 8.41 ft | -5.11 |
The Tongue River is a 90.4-mile-long (145.5 km) tributary of the Pembina River in northeastern North Dakota in the United States. It drains an area of the prairie country near the Canada–US border in the extreme northeast corner of the state in the watershed of the Red River.
It rises in eastern Cavalier County and flows in a direct course east-northeast into Pembina County, passing the towns of Cavalier, Neche and Bathgate. It joins the Pembina from the south approximately 2 miles (3 km) upstream from the mouth of the Pembina on the Red River.
Upstream of Cavalier, the river passes through Icelandic State Park, where Renwick Dam causes it to form Lake Renwick. Below the dam, foot trails follow the river in the Gunlogson Arboretum Nature Preserve.