Historical tsunamis · May 21, 1792

1792 Shimabara Bay, Kyushu Island tsunami

Japan

The tsunami of May 21, 1792 originated near Shimabara Bay, Kyushu Island (Japan).

Key facts

Date
May 21, 1792
Cause
Volcano, earthquake and landslide
Magnitude
M6.4
Maximum documented water height
55.0 m
Deaths
15,000
Injuries
707
Houses destroyed
6,200
Damage
severe (about US$ 5–25 million)
Observation records
24
Countries affected
1

It was triggered by a magnitude 6.4 earthquake.

The highest documented water height was 55.0 m (Futsu, Japan).

24 observation sites in 1 countries are recorded.

The database records 15,000 deaths.

Houses destroyed: 6,200.

Damage is estimated at severe (about US$ 5–25 million).

Map of observation sites

24

Each dot is a documented observation site; colour and size show the observed water height. The triangle marks the source.

Observations by country

CountryObservation recordsMaximum documented water heightDeathsEarliest arrival
Japan2455.0 m
Futsu
5,343—

Highest documented water heights

15 / 24

Individual documented observations for this event. Heights come from different measurement types and sources; not every location has a measured height.

Location / stationObserved heightDistance from sourceCountry
Futsu · Nagasaki55.00 m6 kmJapan
Kawachi, Kumamoto · Kumamoto23.40 m29 kmJapan
Ootao (Ohtao), Misumi · Kumamoto22.50 m22 kmJapan
Ootebaru, Ooyano Island · Kumamoto18.00 m20 kmJapan
Chikoozu · Kumamoto16.50 m30 kmJapan
Amakusa Islands · Nagasaki15.00 m29 kmJapan
Umedo (Umedoo) · Kumamoto14.90 m30 kmJapan
Shioya · Kumamoto14.70 m29 kmJapan
Oshimago, Ariake · Kumamoto12.30 m31 kmJapan
Mie, Shimabara · Nagasaki11.00 m7 kmJapan
Shirato, Ooyano Island · Kumamoto9.90 m20 kmJapan
Kyodomari, Yokoshima · Kumamoto9.60 m25 kmJapan
Seigenji, Nagasu · Kumamoto8.60 m25 kmJapan
Nagasu · Kumamoto5.70 m24 kmJapan
Dosaki · Nagasaki5.00 m8 kmJapan

Source: NOAA National Centers for Environmental Information (NCEI), Global Historical Tsunami Database. Confirmed events only. Deaths and damage are database estimates; older records are incomplete. Water heights come from different types of observation.