The tsunami wave, generated by the earthquake in Japan on March 11, 2011, hit the west coast of the United States many hours later. The Santa Cruz Yacht Harbor in Santa Cruz, California (pictured above, at the Murray Street bridge) experienced seiching, in which the tsunami wave oscillates in the constricted channel of the harbor from a few minutes to a few hours. Boats and floating u-docks were torn free from their moorings, and floated slowly but unattended. Many boats were damaged as a result. [See more]
Soon after the devastating tsunamis in the Indian Ocean on December 26, 2004 and in Japan on March 11, 2011, many people have asked, "Could such a tsunami happen in the United States?" This web page summarizes what we know about tsunamis that have struck the U.S. in the past, providing a foundation for estimating tsunami likelihood in the future. Below, we outline the sources of data that can help answer the question, and indicate when large tsunamis have happened and how large they were, for specific regions of the United States.
Figure from USGS Circular 1187: “Surviving a Tsunami—Lessons from Chile, Hawaii, and Japan”: An earthquake along a subduction zone happens when the leading edge of the overriding plate breaks free and springs seaward, raising the sea floor and the water above it. This uplift starts a tsunami. Meanwhile, the bulge behind the leading edge collapses, thinning the plate and lowering coastal areas.
Tsunamis are ocean waves caused by large earthquakes and landslides that occur near or under the ocean. Scientists do not use the term "tidal wave" because these waves are not caused by tides. Tsunami waves are unlike typical ocean waves generated by wind and storms. When tsunamis approach shore, the behave like a very fast moving tide that extends far inland. A rule of thumb is that if you see the tsunami, it is too late to out run it. Most tsunamis do not "break" like the curling, wind-generated waves popular with surfers. Even "small" tsunamis (for example, 6 feet in height) are associated with extremely strong currents, capable of knocking someone off their feet. Because of complex interactions with the coast, tsunami waves can persist for many hours. As with many natural phenomena, tsunamis can range in size from micro-tsunamis detectable only by sensitive instruments on the ocean floor to mega-tsunamis that can affect the coastlines of entire oceans, as with the Indian Ocean tsunami of 2004. If you hear a tsunami warning or if you feel strong shaking at the coast or very unusual wave activity (e.g., the sea withdrawing far from shore), it is important to move to high ground and stay away from the coast until wave activity has subsided (usually several hours to days). For more general information on tsunamis and what to do during a tsunami warning, please visit sites sponsored by FEMA, the National Weather Service, state agencies, Pacific Marine Environmental Laboratory, NOAA, and the USGS.
In this web page, we will focus mainly on the historic information (1). The National Geophysical Data Center (part of NOAA), maintains a worldwide catalog of historic tsunamis. This catalog includes two types of measurements: runup observations from eyewitness accounts and wave height readings from tide gauge stations, most often located in harbors. In scientific terms, runup refers to the vertical height a wave reaches above a reference sea level as it washes ashore. Wave height is the vertical measurement of the wave before it reaches shore. Inundation distance is the horizontal distance a tsunami reaches landward from the shoreline. More information on tsunami measurements can be found at the NGDC Tsunami Introduction Page.
Hawaiʻi has a long recorded history of tsunamis. Tsunamis have come from both earthquakes around the Pacific rim or "Ring of Fire", termed teletsunamis or far-field tsunamis, and from earthquakes and landslides near Hawaiʻi, termed local tsunamis. One of the largest and most devastating tsunamis Hawaiʻi has experience was a teletsunami in 1946 from an earthquake along the Aleutian subduction zone. Runup heights reached a maximum of 33-55 feet and 159 people were killed. Other important teletsunamis include one from the 1960 M=9.5 earthquake in southern Chile and one from the 1964 M=9.2 earthquake in the Gulf of Alaska. Local tsunamis have also hit Hawaiʻi, primarily from earthquakes and large-scale subsidence along the south flank of Kilauea. The largest of these were in 1868 that killed 81 people, and another in 1975. Overall, approximately 32 tsunamis with runup greater than 1 meter have occurred in Hawaiʻi since 1811.
This photo provides a nice east-facing view of the entire bay and its surroundings. Cenotaph Island (center of the bay), and La Chaussee Spit (thin strip of land at bay's mouth) are visible. The mountains at the head of the bay are part of the Fairweather Range. The non-forested areas of land lining the shore of the bay mark the approximate extent of the tsunami's runup. Photo courtesy of USC Tsunami Research Center.
Because Alaska, including the Aleutian Islands, is bordered to the south by a major subduction zone capable of generating large earthquakes, Alaska has experienced a number of damaging tsunamis. By far, the one that stands out is the tsunami generated from the 1964 M=9.2 earthquake that occurred in the Gulf of Alaska. Not only was a Pacific-wide tsunami generated from this great earthquake, but landslides in the coastal fjords such as Valdez also generated localized, but extremely damaging waves. Alaska's famous fjords are also the source for another type of "tsunami": one in which landslides perched on the steep walls of fjords catastrophically fail and splash into the water, generating extreme wave heights, such as the 1958 Lituya Bay landslide. Again this is a localized phenomenon that does not produce teletsunamis as with tsunamis produced by great earthquakes. Overall, approximately 16 tsunamis of all sources with runup greater than 1 meter have occurred in Alaska since 1853.
Read the article about the 1964 event: Source and progression of a submarine landslide and tsunami: The 1964 Great Alaska earthquake at Valdez - Pure and Applied Geophysics 2014
The historic record of tsunamis along the U.S. west coast includes mainly teletsunamis, generated from large earthquakes around the Pacific Rim. However, using detailed Japanese historic accounts, scientists have determine that a tsunami was generated on January 26, 1700 by a local earthquake close to magnitude 9, offshore the Pacific Northwest (the Cascadia subduction zone). Analysis of geologic deposits indicates that a number of earthquakes, possibly of magnitude 8-9, have occurred in the past, indicating that future tsunamis from the Cascadia subduction zone are possible. Of the teletsunamis that have struck the West Coast, the 1964 Gulf of Alaska tsunami caused the most extensive damage, particularly in Crescent City, California. Overall, approximately 28 tsunamis with runup greater than 1 meter have occurred along the U.S. West Coast since 1812.
Read USGS publications:
In historic times, tsunami waves recorded along the Gulf Coast have all been less than 1 meter. Some of the reports are from the 1964 Gulf of Alaska earthquake recorded in Louisiana and Texas and are technically termed a seiche. A seiche is an oscillation of a body of water, typically caused by atmospheric disturbances, but in this case caused by the ground motion from the earthquake. Seiches can also occur in lakes from earthquake movements. There are a couple of early 20th-century reports of tsunami waves from Caribbean earthquakes along the Gulf Coast that are difficult to evaluate, but the wave heights all appear to be less than 1 meter.
Because there are no major subduction zones in the Atlantic Ocean, except for where it borders the Caribbean Sea, there has been a relatively low frequency of tsunamis compared to the Pacific Ocean. The most famous Atlantic tsunami is the 1755 Lisbon tsunami that was generated by an earthquake on a fault offshore Portugal. The most noteworthy North America local tsunami is the 1929 M=7.2 Grand Banks earthquake near Newfoundland, Canada. This is a complex event; most, if not all, of the tsunami energy may have been triggered by a submarine landslide. The maximum tsunami runup from this event was 2-7 meters concentrated on the coast of Newfoundland, though it was recorded as far south as South Carolina. Like the Gulf Coast, there a couple of reports of small tsunamis from Caribbean earthquakes, all less than 1 meter.
Read an article in the USGS Coastal and Marine Research Newsletter Sound Waves: Submarine Landslides as Potential Triggers of Tsunamis That Could Strike the U.S. East Coast
Puerto Rico and the U.S. Virgin Islands are more susceptible than other locations in the eastern U.S., because of a subduction zone that lies beneath the Caribbean Sea, capable of generating large earthquakes. The web site of the Puerto Rico Tsunami Warning and Mitigation Program also asks whether a tsunami similar to the one in the Indian Ocean could hit the Caribbean region. An event in 1867 off the Virgin Islands is thought to have generated waves 12 meters high. The tsunami with the greatest amount of damage in Puerto Rico was in 1918 from an earthquake off the Mona Passage. With a maximum runup of 6 meters, the tsunami itself killed 40 people with an additional 76 people killed by the earthquake. The Caribbean region as a whole has a history of other earthquakes that have caused damaging tsunamis.
These historic reports are largely based on the tsunami catalog maintained by NOAA's National Geophysical Data Center (NGDC). More tsunami resources can be found on NGDC's Tsunami Data and Information page.