February 16, 1953 Tsunami: Columbia River Valley, WA, United States
A tsunami caused by a landslide began at Columbia River Valley, WA, United States on February 16, 1953 at 11:43 UTC. The water rose as high as 4.8 meters. Its effects were recorded at 1 place.
Where the waves reached
The source (white) and every runup with a place, colored by the water height recorded there. A ring is a runup NCEI marks doubtful.
- Under 1 m
- 1 to 3 m
- 3 to 10 m
- 10 to 30 m
- 30 m and more
- Height not recorded
The tsunami
- Date
- February 16, 1953, 11:43 UTC
- Source
- Columbia River Valley, WA, United States
- Cause
- Landslide
- Maximum water height
- 4.8 m (15.7 ft)
- Runups recorded
- 1
- Waters
- A lake or river, not the ocean
- How certain
- Definite tsunami
- Source location
- 48.570° N, 118.150° W
The toll
The record gives no deaths, injuries or damage for this tsunami.
What the record says
NCEI’s account, from the sources it cites.
A series of landslides on Roosevelt Lake, Washington, near the February 14 slide site generated at least ten waves which crossed the lake and reached the maximum lake shore level 16 feet above the existing lake level. One exceeded the sixteen foot level. A block of material was observed as it dropped into the lake and made a mound of white water one-fourth as high as the terrace. The waves crossed the lake. The wave fronts were vertical walls of water; some had a dome-shaped surface just behind the vertical wall. On the average the waves crossed the lake in one and one-half minutes or at a rate of 4,000 feet per minute. This is in good agreement for a lake depth of about 140 feet indicating the wave traveled as a gravity wave. (Reference #237)
Reference #1695:
The initial failure mass at 8:15 p.m., February 14, 1953. Blocks of earth caved into the lake intermittently until February 19. Thunderous noises accompanied the initial failure and the subsequent caving. Many large waves were formed on the lake.
February 16, 1953, 3:43 a.m. Initial failure. The noises from this slide awakened everyone in the Z. A. Carson household across the lake. Caving and enlarging continued throughout the morning. At least 10 waves crossed the lake and reached the maximum lake-level shoreline, or 16 feet in height. One wave was higher and reached above the high waterline. A block of material was observed as it dropped into the lake and made a mound of white water one-fourth the height of the terrace. Waves crossed the lake. The wave fronts were vertical walls of water; some waves had a dome-shaped surface just behind the vertical wall. On the average the waves crossed the lake in 1% minutes, or at a rate of 4,000 feet per minute.
Note: location approximate
Every runup
Nearest the source first. Heights are above sea level at the time; a tide gauge reads half the wave’s full height.
| Where | Country | Km from source | Water height, m | Inland, m | Measured by | First wave, UTC | Deaths |
|---|---|---|---|---|---|---|---|
| F.D. Roosevelt Lake, WA, WA | United States | 4.8 | Eyewitness observation of water height |
More
Every tsunami in 1953The 1900sTsunamis of United StatesThis day in weather historyAlerts in force
Sources
Tsunami events and runups from NOAA’s National Centers for Environmental Information, Global Historical Hazard Database, cited as NCEI/WDS, doi:10.7289/V5PN93H7. Public domain. Read 2026-09-24. NCEI tsunami event 1832.