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The National Weather Service in Denver has issued a Red Flag Warning for wind and low relative humidity, which is in effect from 11 AM to 8 PM MDT Sunday. The Fire Weather Watch is no longer in effect. * AFFECTED AREA...Fire Weather Zones 214, 240, 241, 242, 243, 244, 245, 246, 247 and 249. * TIMING...From 11 AM to 8 PM MDT Sunday. * WINDS...South 20 to 30 mph with gusts up to 45 mph. * RELATIVE HUMIDITY...As low as 10 percent. * IMPACTS...Conditions will be favorable for rapid fire spread. Avoid outdoor burning and any activity that may produce a spark and start a wildfire.
Total streamflow across the
Snake River
was last observed at
200,069
cfs, and is expected to yield approximately
396,832
acre-ft of water today; about 67%
of normal.
River levels are low and may signify a drought.
Average streamflow for this time of year is
298,630 cfs,
with recent peaks last observed
on
2011-05-27 when daily discharge volume was observed at
763,301 cfs.
Maximum discharge along the river is currently at the
Snake River Bl Mcduff Rapids At China Gardens
reporting a streamflow rate of 42,000 cfs.
However, the streamgauge with the highest stage along the river is the
Snake River At Hells Canyon Dam Id-Or State Line
with a gauge stage of 68.09 ft.
This river is monitored from 27 different streamgauging stations along the Snake River, the highest being situated at an altitude of 9,326 ft, the
Snake River Near Montezuma.
| Last Updated | 2025-04-27 |
| Discharge Volume | 396,832 ACRE-FT |
| Streamflow |
200,068.8 cfs
+11145.8 cfs (+5.9%) |
| Percent of Normal | 67.0% |
| Maximum |
763,301.0 cfs
2011-05-27 |
| Seasonal Avg | 298,630 cfs |
The Snake River is a major river of the greater Pacific Northwest region in the United States. At 1,078 miles (1,735 km) long, it is the largest tributary of the Columbia River, in turn the largest North American river that empties into the Pacific Ocean. The Snake River rises in western Wyoming, then flows through the Snake River Plain of southern Idaho, the rugged Hells Canyon on the Oregon–Idaho border and the rolling Palouse Hills of Washington, emptying into the Columbia River at the Tri-Cities, Washington.
The Snake River drainage basin encompasses parts of six U.S. states and is known for its varied geologic history. The Snake River Plain was created by a volcanic hotspot which now lies underneath the Snake River headwaters in Yellowstone National Park. Gigantic glacial-retreat flooding episodes that occurred during the previous Ice Age carved out canyons, cliffs and waterfalls along the middle and lower Snake River. Two of these catastrophic flooding events, the Missoula Floods and Bonneville Flood, significantly affected the river and its surroundings.
Prehistoric Native Americans lived along the Snake starting more than 11,000 years ago. Salmon from the Pacific Ocean spawned by the millions in the river, and were a vital resource for people living on the Snake downstream of Shoshone Falls. By the time Lewis and Clark explored the area, the Nez Perce and Shoshone were the dominant Native American groups in the region. Later explorers and fur trappers further changed and used the resources of the Snake River basin. At one point, sign language used by the Shoshones representing weaving baskets was misinterpreted to represent a snake, giving the Snake River its name.By the middle 19th century, the Oregon Trail had become well established, bringing numerous settlers to the Snake River region. Steamboats and railroads moved agricultural products and minerals along the river throughout the 19th and early 20th centuries. Starting in the 1890s, fifteen major dams have been built on the Snake River to generate hydroelectricity, enhance navigation, and provide irrigation water. However, these dams blocked salmon migration above Hells Canyon and have led to water quality and environmental issues in certain parts of the river. The removal of several dams on the lower Snake River has been proposed, in order to restore some of the river's once-tremendous salmon runs.
