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LOCAL EARTHQUAKE HISTORY

Sukumo City earthquake and Shindo history in 2019

宿毛市

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

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

In 2019, stations associated with Sukumo City reported local Shindo for 29 earthquakes. The highest local level recorded that year was Shindo 4.

Observed events292019
Highest local Shindo42019
Data period: 1 January–31 December 2019 · 29 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: Feb 3, 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
1202533415−05+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.

6−
Bungosuido Strait豊後水道
114
5−
Hyuganada Sea日向灘
87
4
Kumamoto Region, Kumamoto Prefecture熊本県熊本地方
30
3
Nanyo, Ehime Prefecture愛媛県南予
21
3
Iyonada Sea伊予灘
14
2
Aso Region, Kumamoto Prefecture熊本県阿蘇地方
10
Reference model · not a forecast J-SHIS (NIED) · 250 m · 4932350613

Ground conditions near an observation station

J-SHIS data for the 250 m mesh containing 宿毛市片島.

J-SHIS / NIED

How to read these values

Landform classHill丘陵

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.

AVS30341.6 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×1.14

For the same incoming wave, local ground conditions may make peak-motion velocity at the surface about 14% 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) · A39208

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.

#1Subduction-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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#2Other active faultSukumo-Nakamura fault zone宿毛-中村断層帯

Modelled magnitude: M7.2

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#3Major active faultMedian Tectonic Line (MTL) fault zone (All segment)中央構造線断層帯(全体が同時に活動)

Modelled magnitude: M7.9

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#4Major active faultMedian Tectonic Line (MTL) fault zone (FROM Gojoya segment TO Houyo-kaikyo - Yufuin segment)中央構造線断層帯(五条谷区間~豊予海峡-由布院区間が同時に活動)

Modelled magnitude: M7.9

Read about this model
#5Major active faultMedian Tectonic Line (MTL) fault zone (FROM Kongo-sanchi-toen segment TO Iyonada segment)中央構造線断層帯(金剛山地東縁区間~伊予灘区間が同時に活動)

Modelled magnitude: M7.8

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#6Major active faultMedian Tectonic Line (MTL) fault zone (FROM Gojoya segment TO Iyonada segment)中央構造線断層帯(五条谷区間~伊予灘区間が同時に活動)

Modelled magnitude: M7.8

Read about this model
#7Major active faultMedian Tectonic Line (MTL) fault zone (FROM Negoro segment TO Iyonada segment)中央構造線断層帯(根来区間~伊予灘区間が同時に活動)

Modelled magnitude: M7.8

Read about this model
#8Major active faultMedian Tectonic Line (MTL) fault zone (FROM Kitan-kaikyo - Naruto-Kaikyo segment TO Houyo-kaikyo - Yufuin segment)中央構造線断層帯(紀淡海峡-鳴門海峡区間~豊予海峡-由布院区間が同時に活動)

Modelled magnitude: M7.8

Read about this model

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.