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LOCAL EARTHQUAKE HISTORY

Fujinomiya City earthquake and Shindo history in 2020

富士宮市

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

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

In 2020, stations associated with Fujinomiya City 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 · Shindo 2+ · Clear filters
First observation: Jan 21, 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
1232230405−05+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.

3
Northwestern Chiba Prefecture千葉県北西部
48
2
Southern Ibaraki Prefecture茨城県南部
34
3
Central Shizuoka Prefecture静岡県中部
30
3
Off the Coast of Fukushima Prefecture福島県沖
18
3
Eastern Shizuoka Prefecture静岡県東部
17
4
Eastern Region · Fuji Five Lakes, Yamanashi Prefecture山梨県東部・富士五湖
15
Reference model · not a forecast J-SHIS (NIED) · 250 m · 5238646943

Ground conditions near an observation station

J-SHIS data for the 250 m mesh containing 富士宮市弓沢町.

J-SHIS / NIED

How to read these values

Landform classVolcanic footslope火山山麓地

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.

AVS30280.2 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×1.35

For the same incoming wave, local ground conditions may make peak-motion velocity at the surface about 35% 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) · A22207

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.

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.