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2025-12-22T17:00:00-07:00

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Kankakee River River Levels

Last Updated: December 22, 2025

The Kankakee River is a 133-mile river that flows through Indiana and Illinois.


Summary

Total streamflow across the Kankakee River was last observed at 3,254 cfs, and is expected to yield approximately 6,454 acre-ft of water today; about 32% of normal. River levels are low and may signify a drought. Average streamflow for this time of year is 10,169 cfs, with recent peaks last observed on 2018-02-22 when daily discharge volume was observed at 79,130 cfs.

Maximum discharge along the river is currently at the Kankakee River Near Wilmington reporting a streamflow rate of 2,220 cfs. However, the streamgauge with the highest stage along the river is the Kankakee River At Davis with a gauge stage of 6.48 ft. This river is monitored from 6 different streamgauging stations along the Kankakee River, the highest being situated at an altitude of 682 ft, the Kankakee River At Davis.

River Details

Last Updated 2025-12-22
Discharge Volume 6,454 ACRE-FT
Streamflow 3,254.0 cfs
-319.0 cfs (-8.93%)
Percent of Normal 32.0%
Maximum 79,130.0 cfs
2018-02-22
Seasonal Avg 10,169 cfs
       
River Streamflow Levels
Streamgauge Streamflow Gauge Stage 24hr Change (%) % Normal Minimum (cfs) Maximum (cfs) Air Temp Elevation
Kankakee River At Davis
USGS 05515500
584 cfs 6.48 ft -10.57
Kankakee River At Dunns Bridge
USGS 05517500
1310 cfs 4.89 ft -9.66
Kankakee River Nr Kouts
USGS 05517530
1360 cfs 5.68 ft -7.48
Kankakee River At Shelby
USGS 05518000
1920 cfs 6.45 ft 38.13
Kankakee River At Momence
USGS 05520500
1330 cfs 2.56 ft 12.71
Kankakee River Near Wilmington
USGS 05527500
2220 cfs 1.87 ft 7.77
Seasonal Discharge Comparison
Maximum Streamflow Discharge
Streamflow Elevation Profile

The Kankakee River ([ˌkæŋkəˈki]) is a tributary of the Illinois River, approximately 133 miles (214 km) long, in northwestern Indiana and northeastern Illinois in the United States. At one time, the river drained one of the largest wetlands in North America and furnished a significant portage between the Great Lakes and the Mississippi River. Significantly altered from its original channel, it flows through a primarily rural farming region of reclaimed cropland, south of Lake Michigan.