SNOFLO
 

       




TONGUE RIVER

RIVER LEVELS
March 26, 2025


Total streamflow across the Tongue River was last observed at 315 cfs, and is expected to yield approximately 625 acre-ft of water today; about 25% of normal. River levels are low and may signify a drought. Average streamflow for this time of year is 1,272 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 10.29 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 2025-03-26
Discharge Volume 625 ACRE-FT
Streamflow 315.0 cfs
+60.0 cfs (+23.53%)
Percent of Normal 24.77%
Maximum 24,742.0 cfs
2019-05-31
Seasonal Avg 1,272 cfs
       
River Streamflow Levels
Created with Highcharts 8.0.0Total River Discharge (cfs)17. Mar18. Mar19. Mar20. Mar21. Mar22. Mar23. Mar24. Mar25. Mar26. Mar0200400
Seasonal Discharge Comparison
Created with Highcharts 8.0.0Total River Discharge (cfs)1. Mar1. Apr1. May1. Jun1. Jul1. Aug1. Sep1. Oct1. Nov1. Dec1. Jan05k10k15k
Maximum Streamflow Discharge
Created with Highcharts 8.0.0YearAnnual Peak Discharge(cfs)201020112012201320142015201620172018201920202021202220232024202520261001k10k100k

Weather Forecast

Streamflow Elevation Profile
Created with Highcharts 8.0.0

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.