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LOCAL EARTHQUAKE HISTORY

Karatsu City earthquake and Shindo history in 2019

唐津市

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

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

In 2019, stations associated with Karatsu City reported local Shindo for 8 earthquakes. The highest local level recorded that year was Shindo 2.

Observed events82019
Highest local Shindo22019
Data period: 1 January–31 December 2019 · 8 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: Mar 24, 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
162230405−05+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
Kumamoto Region, Kumamoto Prefecture熊本県熊本地方
76
2
Off the northwest Coast of Fukuoka Prefecture福岡県北西沖
12
2
Aso Region, Kumamoto Prefecture熊本県阿蘇地方
8
2
Hyuganada Sea日向灘
5
2
Ariake Sea有明海
5
2
Amakusa and Ashikita Region, Kumamoto Prefecture熊本県天草・芦北地方
5
Reference model · not a forecast J-SHIS (NIED) · 250 m · 5029174712

Ground conditions near an observation station

J-SHIS data for the 250 m mesh containing 唐津市西城内.

J-SHIS / NIED

How to read these values

Landform classLowland between coastal dunes and/or bars砂丘・砂州間低地

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.

AVS30194.5 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×1.85

For the same incoming wave, local ground conditions may make peak-motion velocity at the surface about 85% 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) · A41202

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.