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LOCAL EARTHQUAKE HISTORY

Kutchan Town earthquake and Shindo history in 2020

倶知安町

This annual view includes only earthquakes from 2020 for which stations associated with Kutchan Town recorded Shindo.

Data period: 1 January–31 December 2020
Data period: 1 January–31 December 2020

In 2020, stations associated with Kutchan Town reported local Shindo for 2 earthquakes. The highest local level recorded that year was Shindo 2.

Observed events22020
Highest local Shindo22020
Data period: 1 January–31 December 2020 · 2 observed earthquakes

Observation history · 2020

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.

2020 · Clear filters
First observation: Feb 17, 2015

Observed events by year

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

All years
2020

Shindo observed in this place

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

All Shindo
112130405−05+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 2020 statistics.

Local seismic profile

Where the shaking usually comes from

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

4
Central and eastern Iburi Region, Hokkaido胆振地方中東部
18
3
Off the east Coast of Aomori Prefecture青森県東方沖
14
3
Off the Coast of Urakawa浦河沖
8
2
Southern Tokachi Region, Hokkaido十勝地方南部
7
2
Off the Coast of Sanriku三陸沖
5
3
Off the Coast of Iwate Prefecture岩手県沖
3
Reference model · not a forecast J-SHIS (NIED) · 250 m · 6440268021

Ground conditions near an observation station

J-SHIS data for the 250 m mesh containing 倶知安町南1条.

J-SHIS / NIED

How to read these values

Landform classBack marsh後背湿地

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.

AVS30180.4 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×1.97

For the same incoming wave, local ground conditions may make peak-motion velocity at the surface about 97% 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.

Local seismic profile

Nearby places

Municipalities nearest to the representative station position.