Historical tsunamis · Nov 1, 1915, 7:23 AM UTC

1915 Sanriku tsunami

Japan

The tsunami of Nov 1, 1915, 7:23 AM UTC originated near Sanriku (Japan).

Key facts

Date
Nov 1, 1915, 7:23 AM UTC
Cause
Earthquake
Magnitude
M7.8
Depth
60 km
Maximum documented water height
1.00 m
Damage
limited (under US$ 1 million)
Observation records
3
Countries affected
2

It was triggered by a magnitude 7.8 earthquake at a depth of 60 km.

The highest documented water height was 1.00 m (Shizugawa Bay, Japan).

3 observation sites in 2 countries are recorded.

Outside the source country, the earliest documented arrival was at Tofino (Clayoquot),British Columbia (Canada) after 9:32 h.

Damage is estimated at limited (under US$ 1 million).

Map of observation sites

3

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 1, 1915, 7:23 AM UTC
  2. 9:32 hCanada · Tofino (Clayoquot),British Columbia · 0.06 m

1 places with a documented arrival time

Observations by country

CountryObservation recordsMaximum documented water heightDeathsEarliest arrival
Japan21.00 m
Shizugawa Bay
——
Canada10.06 m
Tofino (Clayoquot),British Columbia
—9:32 h

Highest documented water heights

3 / 3

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
Shizugawa Bay · Miyagi1.00 m133 kmJapan
Arahama Village · Miyagi0.90 m176 kmJapan
Tofino (Clayoquot),British Columbia · Bc0.06 m6,993 kmCanada

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.