TONGUE RIVER

RIVER LEVELS
April 23, 2025


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
       
River Streamflow Levels
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
Seasonal Discharge Comparison
Maximum Streamflow Discharge

Weather Forecast

Streamflow Elevation Profile

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.