SNOFLO
 



WEST OKAW RIVER

RIVER LEVELS
April 18, 2025


Winter Weather Advisory
2025-04-19T12:00:00-06:00

* WHAT...Snow expected. Total snow accumulations between 3 and 7 inches. * WHERE...Castle Rock. * WHEN...From 3 PM Friday to noon MDT Saturday. * IMPACTS...Plan on slippery road conditions. The hazardous conditions will impact the Friday evening commute.


Maximum discharge along the river is currently at the reporting a streamflow rate of cfs. This is also the highest stage along the West Okaw River, with a gauge stage of ft at this location. This river is monitored from 1 different streamgauging stations along the West Okaw River, the highest being situated at an altitude of ft, the .

       
River Streamflow Levels
Created with Highcharts 8.0.0Total River Discharge (cfs)
Seasonal Discharge Comparison
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Maximum Streamflow Discharge
Created with Highcharts 8.0.0YearAnnual Peak Discharge(cfs)

Weather Forecast

Streamflow Elevation Profile
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The West Okaw River is a tributary of the Kaskaskia River, which it joins in Moultrie County, Illinois. The West Okaw forms an arm of Lake Shelbyville where the natural rivers used to meet.
The name "Okaw" seems to be an alternative name for the Kaskaskia River, of Native American origin. The town of Okawville is located close to the Kaskaskia, but about 100 miles downstream from the West Okaw. The Okaw Valley Council of the Boy Scouts of America is also centered on the Kaskaskia River, far downstream from the West Okaw. This may explain why there is a "West Okaw", but no "East Okaw" or "Okaw" river: the West Okaw is the western fork of the Kaskaskia, which for some reason bears the alternative name for the River.
The West Okaw is about 32 miles (51 km) in length, as measured from the junction of the arms of Lake Shelbyville. This figure includes the drainage ditches, which extend the stream about eight miles above the natural channel.
The watershed of the West Okaw was formed during the Wisconsin glaciation, about 70,000 to 10,000 years before present. The Wisconsin ice sheet advanced roughly to the Lake Shelbyville Dam, forming a terminal moraine. The meltwater overtopped the moraine, forming the modern Kaskaskia River, which flowed on through land of older Illinoian Stage.

Regional Streamflow Levels