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LOCAL EARTHQUAKE HISTORY

Edogawa City earthquake and Shindo history

江戸川区

Earthquakes for which stations associated with Edogawa City reported an actual Shindo observation.

Latest observation: Oct 8, 2026, 04:13 AM JST
Local seismic profile

Since Jan 10, 2015, stations associated with Edogawa City have reported a local reading for 546 earthquakes. Shindo 1 was most common, while the highest local level, Shindo 4, was recorded 5 times.

Latest observationOct 8, 2026
Highest local Shindo4
Observed events546Jan 10, 2015–Oct 8, 2026
Associated observation stations3JMA
Latest observation: Oct 8, 2026

Recent observed earthquakes

No local observation in the last 7 days. Latest observation: Oct 8, 2026

3 Associated observation stations

Stations and strongest local observations

The map combines stations assigned to this place with earthquakes that produced its strongest local readings.

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Associated observation stationsStations: JMA observation catalogue · basemap: OpenFreeMap
Jan 10, 2015 to Oct 8, 2026 · 546 records

Observation history

This history counts earthquakes observed at stations in the place, not earthquakes whose epicentre lies inside its boundary. Counts can change as stations are updated and older or corrected observations are added.

First observation: Jan 10, 2015

Observed events by year

Choose a year to update the event history and local Shindo distribution.

All years
All years

Shindo observed in this place

The highest reading from stations in this place, not the maximum Shindo of the whole event.

All Shindo
13612139341455−05+06−06+070
Reference model · not a forecast

Ground & J-SHIS

A change in the number of observations cannot by itself predict a larger earthquake.

Local seismic profile

Where the shaking usually comes from

Source regions of earthquakes observed here, ordered by the number of reports.

4
Southern Ibaraki Prefecture茨城県南部
103
4
Northwestern Chiba Prefecture千葉県北西部
99
4
Off the Coast of Fukushima Prefecture福島県沖
42
2
Off the Coast of Ibaraki Prefecture茨城県沖
41
3
Off the east Coast of Chiba Prefecture千葉県東方沖
36
3
Northern Ibaraki Prefecture茨城県北部
31
Local seismic profile

Recent observations in long-term context

Latest calendar year342026
Average completed year46.511
Shindo 3 or higher46Shindo ≥ 3

A change in the number of observations cannot by itself predict a larger earthquake.

Reference model · not a forecast J-SHIS (NIED) · 250 m · 5339464934

Ground conditions near an observation station

J-SHIS data for the 250 m mesh containing 東京江戸川区中央.

J-SHIS / NIED

How to read these values

Landform classDelta and coastal lowland三角州・海岸低地

A landform class assigned to the whole 250 m mesh and used to estimate AVS30. The name alone does not determine safety, and it is model data rather than a borehole survey at the station.

AVS30135.3 m/s

The average speed of an S-wave through the upper 30 metres. A lower value generally indicates softer material that can amplify shaking more. J-SHIS uses this value to estimate the amplification shown to the right. It is not predicted Shindo.

Surface velocity amplification×2.52

For the same incoming wave, local ground conditions may make peak-motion velocity at the surface about 152% higher than at engineering bedrock (Vs = 400 m/s). This value describes motion velocity—it does not multiply magnitude or forecast ground acceleration.

Ground conditions can change over short distances. These values do not rate the whole place or the safety of a building, and they cannot predict an earthquake. Source: J-SHIS (NIED), V4 model; processed for presentation by JISHINDESU.

Reference model · not a forecast J-SHIS (NIED) · A13123

Earthquake scenarios affecting this place

Official J-SHIS models ranked for their potential impact on this municipality.

J-SHIS / NIED

#1 means the model ranks highest in the J-SHIS result for this place under the same settings. It is not a ranking of which earthquake will happen next.

Magnitude on a card describes the size of the whole earthquake model, not the Shindo expected here. Local shaking also depends on distance, depth and ground conditions.

#1Subduction-zone earthquakeSagami Trough earthquakes (M8 class)相模トラフ沿いのM8クラスの地震

Modelled magnitude: M7.9–8.6

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#2Subduction-zone earthquakeLarge Earthquakes along the Nankai Trough南海トラフ沿いで発生する大地震

Modelled magnitude: M8.2–9.1

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#3Major active faultAyasegawa fault (Ina-Kawaguchi segment)綾瀬川断層伊奈-川口区間

Modelled magnitude: M6.5

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#4Major active faultFukaya fault zone深谷断層帯

Modelled magnitude: M7.2

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#5Major active faultTachikawa fault zone立川断層帯

Modelled magnitude: M6.8

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#6Major active faultFukaya/Ayasegawa fault zone (All segment)深谷断層・綾瀬川断層(全体が同時に活動)

Modelled magnitude: M7.5

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#7Major active faultFukaya/Ayasegawa fault zone (Fukaya fault zone/Kounosu-Ina segment)深谷断層・綾瀬川断層(深谷断層と鴻巣-伊奈区間が同時に活動)

Modelled magnitude: M7.4

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#8Major active faultFukaya/Ayasegawa fault zone (Kounosu-Ina segment/Ina-Kawaguchi segment)深谷断層・綾瀬川断層(鴻巣-伊奈区間と伊奈-川口区間が同時に活動)

Modelled magnitude: M7.0

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#9Subduction-zone earthquakeMega earthquakes along the Japan Trench (Great East Japan Earthquake 2011 type)日本海溝沿いの超巨大地震(東北地方太平洋沖型)

Modelled magnitude: M8.6–9.0

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J-SHIS 2020 model, 30-year period and Shindo 6-lower threshold. This is not a prediction of a particular earthquake. Source: J-SHIS (NIED); processed for presentation by JISHINDESU.

Local seismic profile

Nearby places

Municipalities nearest to the representative station position.