CLACKAMAS RIVER

RIVER LEVELS
April 21, 2025


Total streamflow across the Clackamas River was last observed at 7,770 cfs, and is expected to yield approximately 15,412 acre-ft of water today; about 70% of normal. Average streamflow for this time of year is 11,063 cfs, with recent peaks last observed on 2015-12-08 when daily discharge volume was observed at 72,200 cfs.

Maximum discharge along the river is currently at the Clackamas River Near Oregon City reporting a streamflow rate of 3,150 cfs. This is also the highest stage along the Clackamas River, with a gauge stage of 25.6 ft at this location. This river is monitored from 3 different streamgauging stations along the Clackamas River, the highest being situated at an altitude of 1,148 ft, the Clackamas River Above Three Lynx Creek.

Last Updated 2025-04-21
Discharge Volume 15,412 ACRE-FT
Streamflow 7,770.0 cfs
-500.0 cfs (-6.05%)
Percent of Normal 70.23%
Maximum 72,200.0 cfs
2015-12-08
Seasonal Avg 11,063 cfs
       
River Streamflow Levels
Streamgauge Streamflow Gauge Stage 24hr Change (%) % Normal Minimum (cfs) Maximum (cfs) Air Temp Elevation
Clackamas River Above Three Lynx Creek
USGS 14209500
2180 cfs 2.68 ft -3.96
Clackamas River At Estacada
USGS 14210000
2440 cfs 12.81 ft -11.27
Clackamas River Near Oregon City
USGS 14211010
3150 cfs 25.6 ft -3.08
Seasonal Discharge Comparison
Maximum Streamflow Discharge

Weather Forecast

Streamflow Elevation Profile

The Clackamas River is an approximately 83-mile (134 km) tributary of the Willamette River in northwestern Oregon, in the United States. Draining an area of about 940 square miles (2,435 km2), the Clackamas flows through mostly forested and rugged mountainous terrain in its upper reaches, and passes agricultural and urban areas in its lower third.
The river rises in eastern Marion County, about 55 miles (89 km) east-southeast of Salem. The headwaters are on the slopes of Olallie Butte in the Mount Hood National Forest, about 10 miles (16 km) north of Mount Jefferson, at an elevation of 4,909 feet (1,496 m) in the Cascade Range. The Clackamas flows briefly north and then flows northwest through the mountains, passing through North Fork Reservoir and Estacada. It then emerges from the mountains southeast of Portland. It joins the Willamette near Oregon City and forms the boundary between Oregon City and Gladstone.
The Clackamas provides hydroelectric power and drinking water for some of the Portland metropolitan area, and it supports runs of Coho salmon, spring and fall Chinook salmon, and summer and winter steelhead. The river's old-growth forests, its habitat for several species of birds, its healthy fish runs, and the recreational opportunities that it provides—such as fishing and whitewater rafting—led to the designation of more than half of the length of the river into the National Wild and Scenic Rivers System (NWSRS). This environment also allowed Native Americans to settle in the river's basin as early as 10,000 years ago.
Regulation of the river began in 1905 with the Cazadero Dam. In 1912, the River Mill Dam intercepted wood and coarse sediment. Later dams at North Fork, Oak Grove, Stone Creek, and Timothy Lake also intercepted wood sediment on the lower river.