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LOCAL EARTHQUAKE HISTORY

Kumagaya City earthquake and Shindo history in 2019

熊谷市

This annual view includes only earthquakes from 2019 for which stations associated with Kumagaya City recorded Shindo.

Data period: 1 January–31 December 2019
Data period: 1 January–31 December 2019

In 2019, stations associated with Kumagaya City reported local Shindo for 39 earthquakes. The highest local level recorded that year was Shindo 3.

Observed events392019
Highest local Shindo32019
Data period: 1 January–31 December 2019 · 39 observed earthquakes

Observation history · 2019

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.

2019 · Clear filters
First observation: Jan 20, 2015

Observed events by year

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

All years
2019

Shindo observed in this place

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

All Shindo
12621033405−05+06−06+070
Reference model · not a forecast

Ground & J-SHIS

The context below uses the place's full available history and reference models; it is not part of the 2019 statistics.

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
150
4
Off the Coast of Fukushima Prefecture福島県沖
63
2
Off the Coast of Ibaraki Prefecture茨城県沖
44
3
Northern Ibaraki Prefecture茨城県北部
43
4
Northwestern Chiba Prefecture千葉県北西部
41
3
Off the east Coast of Chiba Prefecture千葉県東方沖
16
Reference model · not a forecast J-SHIS (NIED) · 250 m · 5439138012

Ground conditions near an observation station

J-SHIS data for the 250 m mesh containing 熊谷市桜町.

J-SHIS / NIED

How to read these values

Landform classAlluvial fan扇状地

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.

AVS30313.1 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×1.23

For the same incoming wave, local ground conditions may make peak-motion velocity at the surface about 23% 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) · A11202

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

Read about this model
#2Major active faultOta fault太田断層

Modelled magnitude: M6.9

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#3Major active faultFukaya fault zone深谷断層帯

Modelled magnitude: M7.2

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#4Subduction-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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#5Major active faultOkubo fault大久保断層

Modelled magnitude: M7.0

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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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#9Major active faultAyasegawa fault (Kounosu-Ina segment)綾瀬川断層鴻巣-伊奈区間

Modelled magnitude: M6.5

Read about this model
#10Subduction-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

Read about this model

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.