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LOCAL EARTHQUAKE HISTORY

Kozagawa Town earthquake and Shindo history in 2017

古座川町

This annual view includes only earthquakes from 2017 for which stations associated with Kozagawa Town recorded Shindo.

Data period: 1 January–31 December 2017
Data period: 1 January–31 December 2017

In 2017, stations associated with Kozagawa Town reported local Shindo for 4 earthquakes. The highest local level recorded that year was Shindo 1.

Observed events42017
Highest local Shindo12017
Data period: 1 January–31 December 2017 · 4 observed earthquakes

Observation history · 2017

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.

2017 · Clear filters
First observation: Feb 6, 2015

Observed events by year

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

All years
2017

Shindo observed in this place

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

All Shindo
142030405−05+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 2017 statistics.

Local seismic profile

Where the shaking usually comes from

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

3
Southern Wakayama Prefecture和歌山県南部
13
3
Kiisuido Strait紀伊水道
9
4
Nara Prefecture奈良県
8
1
Northern Wakayama Prefecture和歌山県北部
8
2
Off the south Coast of Wakayama Prefecture和歌山県南方沖
5
2
Southern Tokushima Prefecture徳島県南部
3
Reference model · not a forecast J-SHIS (NIED) · 250 m · 5035254622

Ground conditions near an observation station

J-SHIS data for the 250 m mesh containing 古座川町峯.

J-SHIS / NIED

How to read these values

Landform classMountain山地

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.

AVS30641.3 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×0.67

For the same incoming wave, local ground conditions may make peak-motion velocity at the surface about 33% 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) · A30424

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.