Total streamflow across the
Cowlitz River
was last observed at
43,890
cfs, and is expected to yield approximately
87,055
acre-ft of water today; about 188%
of normal.
River levels are high.
Average streamflow for this time of year is
23,320 cfs,
with recent peaks last observed
on
2020-02-07 when daily discharge volume was observed at
95,120 cfs.
Maximum discharge along the river is currently at the
Cowlitz River At Castle Rock
reporting a streamflow rate of 16,600 cfs.
This is also the highest stage along the Cowlitz River, with a gauge stage of
37.18 ft at this location.
This river is monitored from 4 different streamgauging stations along the Cowlitz River, the highest being situated at an altitude of 1,053 ft, the
Cowlitz River At Packwood.
Last Updated | 2025-03-28 |
Discharge Volume | 87,055 ACRE-FT |
Streamflow |
43,890.0 cfs
+3080.0 cfs (+7.55%) |
Percent of Normal | 188.21% |
Maximum |
95,120.0 cfs
2020-02-07 |
Seasonal Avg | 23,320 cfs |
The Cowlitz River is a river in the state of Washington in the United States, a tributary of the Columbia River. Its tributaries drain a large region including the slopes of Mount Rainier, Mount Adams, and Mount St. Helens.
The Cowlitz has a 2,586-square-mile (6,698 km2) drainage basin, located between the Cascade Range in eastern Lewis County, Washington and the cities of Kelso and Longview. The river is roughly 105 miles (169 km) long, not counting tributaries.
Major tributaries of the Cowlitz River include the Cispus River and the Toutle River, which was overtaken by volcanic mudflows (lahars) during the May 1980 eruption of Mount St. Helens.
When the smelt spawn in the Cowlitz River, the gulls go into a feeding frenzy that lasts for weeks. Kelso, Washington is known as the "Smelt Capital of the World".