Historical tsunamis · Nov 5, 1938, 10:50 AM UTC

1938 Sanriku tsunami

Japan

The tsunami of Nov 5, 1938, 10:50 AM UTC originated near Sanriku (Japan).

Key facts

Date
Nov 5, 1938, 10:50 AM UTC
Cause
Earthquake
Magnitude
M7.6
Depth
30 km
Maximum documented water height
0.56 m
Observation records
12
Countries affected
1

It was triggered by a magnitude 7.6 earthquake at a depth of 30 km.

The highest documented water height was 0.56 m (Hanabuchi, Japan).

12 observation sites in 1 countries are recorded.

Map of observation sites

12

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

Tsunami arrival times

Documented arrival times from the NOAA/NCEI database, showing the earliest recorded location per country. Coverage is incomplete: a country without an entry was not necessarily spared.

  1. 0:00 hEarthquake (origin) · Nov 5, 1938, 10:50 AM UTC
  2. 0:30 hJapan · Choshi · 0.14 m

11 places with a documented arrival time

Observations by country

CountryObservation recordsMaximum documented water heightDeathsEarliest arrival
Japan120.56 m
Hanabuchi
—0:30 h

Highest documented water heights

12 / 12

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
Hanabuchi · Miyagi0.56 m132 kmJapan
Onahama · Fukushima0.40 m77 kmJapan
Tsukihama · Miyagi0.32 m153 kmJapan
Kesennumagyoko · Miyagi0.25 m189 kmJapan
Hachinohe · Aomori0.22 m370 kmJapan
Ishinomaki · Miyagi0.15 m140 kmJapan
Oshima (Shiogamako) · Miyagi0.15 m137 kmJapan
Shiogama · Miyagi0.15 m137 kmJapan
Choshi · Chiba0.14 m177 kmJapan
Ayukawa · Miyagi—123 kmJapan
Hakodate · Hokkaido—509 kmJapan
Miyako · Iwate—273 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.