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LOCAL EARTHQUAKE HISTORY

Gero City earthquake and Shindo history in 2022

下呂市

This annual view includes only earthquakes from 2022 for which stations associated with Gero City recorded Shindo.

Data period: 1 January–31 December 2022
Data period: 1 January–31 December 2022

In 2022, stations associated with Gero City reported local Shindo for 6 earthquakes. The highest local level recorded that year was Shindo 1.

Observed events62022
Highest local Shindo12022
Data period: 1 January–31 December 2022 · 6 observed earthquakes

Observation history · 2022

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.

2022 · Clear filters
First observation: Mar 4, 2015

Observed events by year

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

All years
2022

Shindo observed in this place

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

All Shindo
162030405−05+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 2022 statistics.

Local seismic profile

Where the shaking usually comes from

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

3
Hida, Gifu Prefecture岐阜県飛騨地方
51
4
Southern Nagano Prefecture長野県南部
22
4
Noto, Ishikawa Prefecture石川県能登地方
15
3
Central and western Mino, Gifu Prefecture岐阜県美濃中西部
14
3
Eastern Mino, Gifu Prefecture岐阜県美濃東部
8
2
Off the Coast of Noto Peninsula能登半島沖
7
Reference model · not a forecast J-SHIS (NIED) · 250 m · 5337516932

Ground conditions near an observation station

J-SHIS data for the 250 m mesh containing 下呂市森.

J-SHIS / NIED

How to read these values

Landform classValley bottom lowland谷底低地

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.

AVS30461.1 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×0.89

For the same incoming wave, local ground conditions may make peak-motion velocity at the surface about 11% lower 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) · A21220

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.

#1Major active faultAtera fault zone (Main part/Northern segment)阿寺断層帯主部北部

Modelled magnitude: M6.4

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#2Major active faultSami fault zone阿寺断層帯佐見断層帯

Modelled magnitude: M6.7

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#3Other active faultKuno-gawa fault久野川断層

Modelled magnitude: M6.8

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#4Major active faultShirakawa fault zone阿寺断層帯白川断層帯

Modelled magnitude: M6.8

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#5Major active faultInohana fault zone高山・大原断層帯猪之鼻断層帯

Modelled magnitude: M6.5

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#6Other active faultKuchiudo-Yamanokuchi fault口有道-山之口断層

Modelled magnitude: M7.0

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#7Other active faultWakatochi-toge fault若栃峠断層

Modelled magnitude: M6.7

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#8Major active faultTakayama fault zone高山・大原断層帯高山断層帯

Modelled magnitude: M6.9

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#9Major active faultAko fault zone赤河断層帯

Modelled magnitude: M6.6

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#10Subduction-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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#11Major active faultNagaragawa-joryu fault zone長良川上流断層帯

Modelled magnitude: M6.8

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#12Major active faultAtera fault zone (Main part/Southern segment)阿寺断層帯主部南部

Modelled magnitude: M7.2

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#13Major active faultShokawa fault zone庄川断層帯

Modelled magnitude: M7.2

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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.