JISHINDESUJapan earthquakes, down to the local station
EN
Open interactive map
MenuMore
LOCAL EARTHQUAKE HISTORY

Saiki City earthquake and Shindo history

佐伯市

Earthquakes for which stations associated with Saiki City reported an actual Shindo observation.

Latest observation: —
Local seismic profile

Since —, stations associated with Saiki City have reported a local reading for 0 earthquakes. Shindo 1 was most common, while the highest local level, Shindo —, was recorded 0 times.

Latest observation—
Highest local Shindo—
Observed events0—–—
Associated observation stations0JMA
Latest observation: —

Recent observed earthquakes

No local observation in the last 7 days. Latest observation: —

No place history is available yet.

— to — · 0 records

Observation history

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.

First observation: —

Observed events by year

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

All years
All years

Shindo observed in this place

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

All Shindo
102030405−05+06−06+070
Latest observation: —

Recent observed earthquakes

0 observed earthquakes

No observed earthquakes match these filters.

Reference model · not a forecast

Ground & J-SHIS

A change in the number of observations cannot by itself predict a larger earthquake.

Local seismic profile

Recent observations in long-term context

Latest calendar year00
Average completed year0.00
Shindo 3 or higher0Shindo ≥ 3

A change in the number of observations cannot by itself predict a larger earthquake.

Reference model · not a forecast J-SHIS (NIED) · A44205

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

Read about this model
#2Other active faultFukuragi fault福良木断層

Modelled magnitude: M6.8

Read about this model
#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

Read about this model
#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 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
#6Major active faultMedian Tectonic Line (MTL) fault zone (FROM Sanuki-sanmyaku-nanen eastern segment TO Houyo-kaikyo - Yufuin segment)中央構造線断層帯(讃岐山脈南縁東部区間~豊予海峡-由布院区間が同時に活動)

Modelled magnitude: M7.7

Read about this model
#7Major active faultMedian Tectonic Line (MTL) fault zone (FROM Sanuki-sanmyaku-nanen western segment TO Houyo-kaikyo - Yufuin segment)中央構造線断層帯(讃岐山脈南縁西部区間~豊予海峡-由布院区間が同時に活動)

Modelled magnitude: M7.7

Read about this model
#8Major active faultMedian Tectonic Line (MTL) fault zone (FROM Ishizuchi-sanmyaku-hokuen segment TO Houyo-kaikyo - Yufuin segment)中央構造線断層帯(石鎚山脈北縁区間~豊予海峡-由布院区間が同時に活動)

Modelled magnitude: M7.7

Read about this model
#9Major 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

Read about this model
#10Major 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
#11Major 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
#12Major active faultMedian Tectonic Line (MTL) fault zone (FROM Ishizuchi-sanmyaku-hokuen western segment TO Houyo-kaikyo - Yufuin segment)中央構造線断層帯(石鎚山脈北縁西部区間~豊予海峡-由布院区間が同時に活動)

Modelled magnitude: M7.6

Read about this model
#13Major active faultMedian Tectonic Line (MTL) fault zone (FROM Iyonada segment TO Houyo-kaikyo - Yufuin segment)中央構造線断層帯(伊予灘区間~豊予海峡-由布院区間が同時に活動)

Modelled magnitude: M7.6

Read about this model
#14Major active faultMedian Tectonic Line (MTL) fault zone (FROM Kitan-kaikyo - Naruto-Kaikyo segment TO Iyonada segment)中央構造線断層帯(紀淡海峡-鳴門海峡区間~伊予灘区間が同時に活動)

Modelled magnitude: M7.7

Read about this model
#15Major active faultMedian Tectonic Line (MTL) fault zone (FROM Sanuki-sanmyaku-nanen eastern segment TO Iyonada segment)中央構造線断層帯(讃岐山脈南縁東部区間~伊予灘区間が同時に活動)

Modelled magnitude: M7.7

Read about this model
#16Major active faultMedian Tectonic Line (MTL) fault zone (FROM Sanuki-sanmyaku-nanen western segment TO Iyonada segment)中央構造線断層帯(讃岐山脈南縁西部区間~伊予灘区間が同時に活動)

Modelled magnitude: M7.7

Read about this model
#17Major active faultMedian Tectonic Line (MTL) fault zone (FROM Ishizuchi-sanmyaku-hokuen segment TO Iyonada segment)中央構造線断層帯(石鎚山脈北縁区間~伊予灘区間が同時に活動)

Modelled magnitude: M7.6

Read about this model
#18Major active faultMedian Tectonic Line (MTL) fault zone (FROM Ishizuchi-sanmyaku-hokuen western segment TO Iyonada segment)中央構造線断層帯(石鎚山脈北縁西部区間~伊予灘区間が同時に活動)

Modelled magnitude: M7.5

Read about this model
#19Major active faultMedian Tectonic Line (MTL) fault zone (Iyonada segment)中央構造線断層帯(伊予灘区間)

Modelled magnitude: M7.4

Read about this model
#20Major active faultMedian Tectonic Line (MTL) fault zone (Houyo-kaikyo - Yufuin segment)中央構造線断層帯(豊予海峡−由布院区間)

Modelled magnitude: M7.2

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.