Historical tsunamis · Mar 25, 2007, 12:41 AM UTC

2007 Honshu: W Coast tsunami

Japan

The tsunami of Mar 25, 2007, 12:41 AM UTC originated near Honshu: W Coast (Japan).

Key facts

Date
Mar 25, 2007, 12:41 AM UTC
Cause
Earthquake
Magnitude
M6.7
Depth
8 km
Maximum documented water height
0.10 m
Deaths
1
Injuries
359
Houses destroyed
13,556
Damage
severe (about US$ 5–25 million)
Observation records
6
Countries affected
1

It was triggered by a magnitude 6.7 earthquake at a depth of 8 km.

The highest documented water height was 0.10 m (Noto (Suzushi Nagahashi), Japan).

6 observation sites in 1 countries are recorded.

The database records 1 deaths.

Houses destroyed: 13,556.

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

Map of observation sites

6

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) · Mar 25, 2007, 12:41 AM UTC
  2. 0:06 hJapan · Toyama · 0.03 m

6 places with a documented arrival time

Observations by country

CountryObservation recordsMaximum documented water heightDeathsEarliest arrival
Japan60.11 m
Noto (Suzushi Nagahashi)
—0:06 h

Highest documented water heights

6 / 6

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
Noto (Suzushi Nagahashi) · Ishikawa0.11 m53 kmJapan
Kanazawa · Ishikawa0.09 m80 kmJapan
Wajima · Ishikawa0.04 m28 kmJapan
Toyama · Toyama0.03 m85 kmJapan
Fushikiko · Toyama—74 kmJapan
Shinminato · Toyama—77 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.