Major Flood
17 ft
Located in Roger Mills County, Oklahoma on the Washita River. Live water level data from USGS gauge 07316500, updated every 15 minutes.
Loading...
Loading...
Loading...
Flood stages defined by the National Weather Service. Gage height data from USGS Water Resources.
17 ft
15 ft
13.5 ft
12 ft
Flooding of agricultural lands occurs in Roger Mills and western Custer counties above the headwaters of Foss Lake. Cheyenne is not threatened... but the U.S. Highway 283 crossing between Cheyenne and Roll is impassable. The railroad along the river valley is overtopped near Strong City when the river stage rises above 20 feet. This flood will surpass the worst in history... which occurred on April 3 1934 ... and exceed all stages recorded since the completion of the upstream flood control project.
Flooding of agricultural lands occurs in Roger Mills and western Custer counties above the headwaters of Foss Lake. Cheyenne is not threatened... but the U.S. Highway 283 crossing between Cheyenne and Roll is impassable. The railroad along the river valley is overtopped near Strong City when the river stage rises above 20 feet. This flood will surpass the worst in history... which occurred on April 3 1934... and exceed all stages recorded since the completion of the upstream flood control project.
Flooding of agricultural lands occurs in Roger Mills and western Custer counties above the headwaters of Foss Lake. Cheyenne is not threatened... but the U.S. Highway 283 crossing between Cheyenne and Roll is impassable. The railroad along the river valley may be overtopped near Strong City when the river stage rises above 20 feet. This flood will approach the worst in history... which occurred on April 3 1934... and exceed all stages since the completion of the upstream flood control project.
Flooding of agricultural lands along the Washita River occurs in Roger Mills and western Custer counties above the headwaters of Foss Lake. The U.S. Highway 283 crossing between Cheyenne and Roll may be be impassable due to overflows. The railroad line along the river valley may be overtopped in the vicinity of Strong City. This flood may surpass the highest seen near Cheyenne since the completion of the upstream flood control project on the upper Washita River.
Flooding of agricultural lands along the Washita River occurs in Roger Mills and western Custer counties above the headwaters of Foss Lake. The U.S. Highway 283 crossing between Cheyenne and Roll may be be impassable due to overflows. This flood will be the highest seen near Cheyenne since the completion of the upstream flood control project on the upper Washita River.
Flooding of agricultural lands along the Washita River occurs in Roger Mills and western Custer counties above the headwaters of Foss Lake. The U.S. Highway 283 crossing between Cheyenne and Roll may be be impassable due to overflows. This flood will be the highest seen near Cheyenne since the completion of the upstream flood control project on the upper Washita River.
Flooding of agricultural lands along the Washita River occurs in Roger Mills and western Custer counties above the headwaters of Foss Lake. The U.S. Highway 283 crossing between Cheyenne and Roll may be impassable due to overflows. This flood will approach the highest seen near Cheyenne since the completion of the upstream flood control project on the upper Washita River.
Flooding of agricultural lands along the Washita River occurs in Roger Mills and western Custer counties above the headwaters of Foss Lake. The U.S. Highway 283 crossing between Cheyenne and Roll may be overtopped when the river stage rises above 15 feet.
Flooding of agricultural lands along the Washita River occurs in Roger Mills and western Custer counties above the headwaters of Foss Lake. U.S. Highway 283 between Cheyenne and Roll may be overtopped.
Flooding of agricultural lands along the Washita River occurs in Roger Mills and western Custer counties above the headwaters of Foss Lake.
Flooding of low-lying agricultural lands along the Washita River occurs in Roger Mills and western Custer counties above the headwaters of Foss Lake.
Flooding of low-lying agricultural lands along the Washita River may occur in Roger Mills and western Custer counties above the headwaters of Foss Lake.
Flooding of low-lying agricultural lands along the Washita River may occur in Roger Mills and western Custer counties above the headwaters of Foss Lake.
Expect near bankfull conditions along the Washita River in Roger Mills and western Custer counties above the headwaters of Foss Lake.
Expect near bankfull conditions along the Washita River in Roger Mills and western Custer counties above the headwaters of Foss Lake.
Impact statements from the National Weather Service, describing what typically happens at each water level.
Loading chart data...
| Date | Stage | Flow |
|---|---|---|
| Apr 28, 1954 | 20.24 ft | 69,800 cfs |
| Apr 2, 1934 | 19.2 ft | 52,000 cfs |
| May 22, 1941 | 18.5 ft | 40,000 cfs |
CHYO2
Washita River
Roger Mills, OK
35.6264°N, 99.6684°W
StormCast monitors this gauge and sends a push notification to your phone when the water level crosses into a new flood category — even at 3 AM.
The Washita River near Cheyenne gauge is maintained by USGS (site 07316500) and reports water levels every 15 minutes. Visit this page to see the latest reading updated live, or download StormCast to get push alerts when levels rise.
The NWS-defined flood stage for Washita River near Cheyenne is 13.5 feet. Action stage begins at 12 feet. Moderate flooding starts at 15 feet, and major flooding at 17 feet.
Download StormCast free on Google Play, go to River Gauges, and add Washita River near Cheyenne to your watchlist. StormCast will send a push notification to your phone whenever the water level crosses into a new NWS flood category.
The gauge is located in Roger Mills County, Oklahoma at coordinates 35.6264°N, 99.6684°W. USGS site number: 07316500. Data is provided by the U.S. Geological Survey and the National Weather Service.
Data provided by: US Geological Survey, Observations courtesy of U.S. Geological Survey, Observations courtesy of U.S. Army Corps of Engineers