M3.5 Depth: 100.0 km

M3.5 Earthquake near zhong zha nei cun, bei hai dao (Japan)

UTC time: 2026-03-04 21:45:30 UTC Local time:

About this earthquake

On March 4, 2026 at 21:45 UTC, a magnitude M3.5 earthquake occurred near zhong zha nei cun, bei hai dao (Japan). The earthquake originated at an intermediate depth of about 100 km. Earthquakes of this magnitude are often felt but rarely cause damage.

The data is provided by EMSC and cross-checked across seismological networks. Japan: 3 earthquakes were recorded in the past 24 hours, the strongest reaching M4.7.

Details

Magnitude
M3.5
Depth
100.0 km
UTC time
2026-03-04 21:45:30 UTC
Local time
Country
State
bei hai dao
City
zhong zha nei cun
County
he xi jun
Village
zhong zha nei cun
Source
emsc
Coordinates
42.60000, 143.00000
Temperature
-4.0°C

Map

Depth profile

Depth profile Depth: 100 km (Intermediate) Surface Shallow Intermediate Deep 0 km 70 km 300 km 700 km 100 km
Intermediate
100 km
100 km — deeper than the regional average (35.1 km)
Regional average: 35.1 km
Why depth matters

Intermediate-depth quakes are felt across a wider area but usually cause less surface damage.

Depth classes per USGS

Volcanoes nearby

  • Maruyama
    Distance: 91 km ·Stratovolcano(es) ·Elevation: 2'013 m ·Last eruption: 1898 ·Japan
  • Tokachidake
    Distance: 94 km ·Stratovolcano(es) ·Elevation: 2'077 m ·Last eruption: 2004 ·Japan
  • Taisetsuzan
    Distance: 119 km ·Stratovolcano(es) ·Elevation: 2'291 m ·Last eruption: 1739 ·Japan
  • Akan
    Distance: 120 km ·Caldera ·Elevation: 1'499 m ·Last eruption: 2026 ·Japan
  • Shikotsu
    Distance: 133 km ·Caldera ·Elevation: 1'320 m ·Last eruption: 1981 ·Japan
  • Kuttara
    Distance: 151 km ·Stratovolcano(es) ·Elevation: 549 m ·Last eruption: 1820 ·Japan

Historic earthquake map · Japan

Explore recent and long-term earthquake activity in this country. Use filters to narrow down by magnitude, depth, and date range.

Country statistics · Japan

View earthquake KPIs, strongest and latest events, and averages for this country.

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