Tsunamis in 1700

January 27, 1700 Tsunami: Cascadia Subduction Zone, United States

January 27, 1700 · Deaths: few · Definite tsunami

A tsunami caused by a magnitude 9 earthquake began at Cascadia Subduction Zone, United States on January 27, 1700 at 05:00 UTC. Its effects were recorded at 7 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

NOAA NCEI’s travel time map for this tsunami: one line for each hour after the source, showing how long the first wave took to reach each part of the ocean.

The map of NCEI’s lines needs JavaScript.

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

NCEI computed these with the TTT software from the epicenter and a 2-minute bathymetry grid. In NCEI’s words, “Calculated times are usually within 1 hour of the observed travel times, but can differ by more than one hour, particularly when the location is across the Pacific Basin.” The lines give when the first wave arrives, not how high it is. NCEI’s travel time maps.

The tsunami

Date
January 27, 1700, 05:00 UTC
Source
Cascadia Subduction Zone, United States
Cause
Earthquake
Earthquake
Magnitude 9
Runups recorded
7
Waters
Ocean
How certain
Definite tsunami
Source location
45.000° N, 125.000° W

The toll

Deaths
2; Few (about 1 to 50) with the earthquake or eruption that caused it
Damage
Severe (about $5 to $25 million)

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.

An unusually high tidal wave was observed on the coast of the Kii Peninsula and at Ozuchi (Iwate Prefecture). There are no reports about an earthquake. Was this a tsunami of remote origin. (Reference #414, first published in Russian, 1974). Reference #150 lists the source of the tsunami that attacked Otsuchi as off Miyagi Prefecture.

A Pacific tsunami flooded Japanese shores in January 1700. The waters drove villagers to high ground, damaged salt kilns and fishing shacks, drowned paddies and crops, ascended a castle moat, entered a government store house, washed away more than dozen buildings and spread flames that consumed twenty more. Return flows contributed to a nautical accident that sank tons of rice and killed two sailors. Samurai magistrates issued rice to afflicted villagers and requested lumber for those left homeless. A village headman received no advance warning from an earthquake; he wondered what to call the waves. (from p. 27 reference #2479)

Places flooded by the 1700 tsunami in Japan include Kuwagasaki, Tsugaruishi, Otsuchi, Miho and Tanabe. Some of the accounts mention damage in additional villages. In one account, the tsunami takes the form of rough seas that initiate a nautical accident near Nakaminato. (from p. 33 reference #2479)

A trans-Pacific reunion took place in 1996. Orphaned for nearly 300 years, the 1700 tsunami in Japan was reuinted, on the pages of a scientific journal, with an earthquake and tsunami in North America... The orphan dated the earthquake to the evening of January 26, 1700... and gave its approximate size as magnitude 9. (from p.93 reference #2479)

Today the 1700 tsunami is securely linked to a giant North American earthquake. The tie was strengthened in 1997 by tree-ring dating that narrowed the time window for a great Cascadia earthquake to the months between August 1699 and May 1700. The earthquake's enormity was confirmed in 2003 through improved estimates of the tsunami's size and from computer simulations of Cascadia earthquakes and of the tsunami itself... The tsunami's written record in Japan has become clearer too, with discovery in 1998 of the Miho headman's account, authentification in 2002 of the Nakaminato shipwreck certificate and explanation in 2004 of a discordant date from Tsugaruishi. (from p. 93 reference #2479)

The Cascadia Subduction Zone (CSZ) is situated off of the Pacific Northwest coast of North America, from Northern California to Vancouver Island, British Columbia. (from reference #2480)

If the 1700 tsunami came from Cascadia, we can estimate the origin time and magnitude of the earthquake. The earliest documented tsunami arrival time was around midnight on 27 January Japan time, or around 15:00 on 27 January GMT. Because tsunami travel time from Cascadia to Japan is about 10 hours, the earthquake origin time is estimated at around 5:00 27 January GMT or 21:00 on 26 January local time in Cascadia. This time is consistent with Native American legends that an earthquake occurred on a winter night. (reference #2654)

Reference #4153 summarizes oral traditions providing evidence for historical great earthquakes in the Cascadia Subduction Zone. A spectacular example mentioning both a tsunami and ground shaking that occurred just before the tsunami wave arrival, describes the destruction of Loht'a, the principle winter village of the Pachena Bay people on the west coast of Vancouver Island where about 100 fatalities.

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
KuwagasakiJapan7,2484Eyewitness observation of water heightday 27, 15:00
TsugaruishiJapan7,2525Eyewitness observation of water height
OtsuchiJapan7,2724Eyewitness observation of water heightday 27, 15:00
NakaminatoJapan7,576Eyewitness observation of water height2
MihoJapan7,8365.4Eyewitness observation of water height
ShinjoJapan8,122Eyewitness observation of water height
Tanabe, Kii PeninsulaJapan8,1255Eyewitness observation of water height

More

Every tsunami in 1700The 1700sTsunamis of United StatesThe earthquakeThis 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 361.