OTE - Oregon Travel Experience

Great Tsunami of 1700

Posted on: October 15th, 2024 in Historical Marker Audio Tours, Historical Marker Details |

During the 18th century, Native American villages occupied the mouths of nearly every stream along this coastline-including here at Siletz Bay. References to great flooding and ground shaking events are recorded in the oral traditions of many Pacific Northwest coastal tribes. These stories include instructions about how to prepare for large flooding events.

On January 26, 1700, the earth shook violently in the throes of a magnitude 9+ earthquake that occurred along the great offshore fault system called the Cascadia Subduction Zone. From northern California to British Columbia the ocean floor heaved upward approximately 20 feet, and within 10=20 minutes a giant wave 30-40 feet high reached the shore. The wave probably struck this beach 22 minutes after the earthquake and fully inundated the coast in about 30-35 minutes. Devastating waves from this event continued to strike the entire coastline for several hours, flooding beaches, bays, tidal channels, and marshes.

From geologic records, we know that major earthquakes and tsunamis occur along this segment of the Pacific coast every 100-1000 years, and on average about every 500 years- we also know what to do when the earth shakes: Protect yourself during the earthquake by Dropping, Covering and Holding On. After the shaking stops, travel immediately inland and uphill. There will be no official warning. The earthquake is your warning. Do not return to the beach or low-lying areas- giant waves may strike for several hours after the earthquake. Wait for official notice from authorities that the danger has passed before returning into the tsunami evacuation zone. It is easy to imagine the terror, tremendous loss of life, and destruction that occurred here at Siletz Bay, and along the entire coastline in the wake of the great tsunami of 1700. But you can survive these large earthquakes and tsunamis by being prepared.

Location: Schooner Creek Wayside, south end of Lincoln City

Sponsors: Department of Geology & Minerals, Oregon Emergency Management

Learn More: Visit Oregon Encyclopedia

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