Tsunamis in 1820

1820 Tsunami: Camano Island, WA, United States

1820 · Deaths: many · Probable tsunami

A tsunami caused by a landslide began at Camano Island, WA, United States in 1820. Its effects were recorded at 2 places.

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

Tsunami warnings in force

Travel times

How long the first wave took to reach each part of the ocean, one line for each hour up to 24, estimated from the source and the depth of the sea.

The travel times are computed in your browser, which needs JavaScript.

  • 1 to 4 hours
  • 5 to 6 hours
  • 7 to 14 hours
  • 15 hours and more

Computed in your browser the way NOAA’s own travel time maps are: the wave travels at the square root of gravity times the depth, over NOAA’s ETOPO1 depths averaged to a 10 arc-minute grid. Checked against NOAA NCEI’s maps for 21 tsunamis over the first 24 hours, these lines fall within 10 minutes of NCEI’s at half the points compared and within 52 minutes at 9 in 10. They give when the first wave could arrive, not how high it is; bays, harbors and island chains finer than the grid can see it later. Not for use in a warning: see tsunami.gov.

The tsunami

Date
1820
Source
Camano Island, WA, United States
Cause
Landslide
Runups recorded
2
Waters
Ocean
How certain
Probable tsunami
Source location
48.060° N, 122.360° W

The toll

Deaths
Some (about 51 to 100); Many (about 101 to 1,000) with the earthquake or eruption that caused it
Houses destroyed
Few (about 1 to 50)

Where the literature gives no number, NCEI records a description on a scale of 1 to 4, printed here in its words. Damage is in millions of US dollars of the year of the event, not adjusted for inflation.

What the record says

NCEI’s account, from the sources it cites.

Reference #11938:

Told by Mrs. William Shelton:

"The bluff slid in. People at Hat Island in the early summer morning saw Camano Island bluff smoking; they couldn't see it for the smoke; and there was something black coming towards them, and then they saw it was a wave. They fled to high land.Some of the men and women, and some of the children were drowned, and they found the bodies drifting on the beach.

When the point slid, trees and everything went, killed quite a few people living on the west side of Hat Island.

Houses, not a real village, all washed off and people killed."

Mr. John Brown, Snohomish, of Sandy Point added some other details. Old Indians told him the slide was an overhang, and the fall buried hundreds who were clamming there. The wave washed over to Hat Island and drowned hundreds who ere clamming there.

...it is pointed out that the naming of known recent historical persons of one's own family gives a historical basis that cannot lightly be dismissed. The story would indicate a date of 1820-1830 for the incident.

The numbers given by John Brown could be exaggerations, but it is certain that the clam beds at Camano Head and the northern end of Hat Island always have been the most important beds in the Snohomish area. Hence, being early on summer morning before the people were all up, the casualties may indeed have been very heavy, even running into hundreds, especially at the Head itself from which there was no escape.

Reference #11939:

The accounts also mention that some flooding may have occurred at Hibolb (a larger village on the northern Everett shoreline near the mouth of the Snohomish), but if damage occurred at all, it was limited. No mention is made of the wave at other low-lying sites in the vicinity, such as Sandy Point on Whidbey Island - the closest barrier beach and marsh to Camano Head.

Although the accounts leave many questions unanswered, the following seems fairly clear. Early on a summer morning in the early 1800s, a large landslide occurred at Camano Head, carrying standing trees to the beach, and burying many people living at the toe of the bluff. The landslide sounded like thunder and created large volumes of dust. The landslide also resulted in a tsunami that traveled south toward Hat Island, washing over the barrier beach, destroying houses or encampments and drowning many people.

The accounts make no mention of ground shaking, suggesting that the landslide was not associated with a major earthquake.

The Camano Head landslide is the only known example of a landslide on Puget Sound generating a tsunami large enough to cause significant loss of life.

Reference #11942:

One of the Snohomish villages was located beneath a bluff at the southern tip of Camano Island, Camano Head. Hundreds of people probably made their home in the huge, multi-family split cedar plank houses, as the clam beds on Camano were (and are) well known for their abundance. One early summer day, just as first dawn was beginning to lighten the eastern sky, that village was destroyed.

A sound like thunder awakened the families living in the village across the water on the northwestern shore of Hat Island -- perhaps also the people at Hebolb, the major village in north Everett. Staring intently toward the source of the sound, all the Hat Island people could see was a huge, impenetratble cloud off in the distance, and then something black beneath it and growing closer. A tidal wave! Men, women, and children raced off the beach for the higher ground, but the water crashed into them and swept away its victims. Many children especially were lost to the wave.

Every runup

Nearest the source first. Heights are above sea level at the time; a tide gauge reads half the wave’s full height.

WhereCountryKm from sourceWater height, mInland, mMeasured byFirst wave, UTCDeaths
Hat Island, WAUnited States5Eyewitness observation of water height
Hilbolb Village, WAUnited States13Eyewitness observation of water height

More

Every tsunami in 1820The 1800sTsunamis of United StatesAlerts 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 5666.