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LOCAL EARTHQUAKE HISTORY

Beppu City earthquake and Shindo history in 2025

別府市

This annual view includes only earthquakes from 2025 for which stations associated with Beppu City recorded Shindo.

Data period: 1 January–31 December 2025
Data period: 1 January–31 December 2025

In 2025, stations associated with Beppu City reported local Shindo for 21 earthquakes. The highest local level recorded that year was Shindo 3.

Observed events212025
Highest local Shindo32025
Data period: 1 January–31 December 2025 · 21 observed earthquakes

Observation history · 2025

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.

2025 · Clear filters
First observation: May 30, 2015

Observed events by year

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

All years
2025

Shindo observed in this place

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

All Shindo
1142532405−05+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 2025 statistics.

Local seismic profile

Where the shaking usually comes from

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

4
Central Oita Prefecture大分県中部
74
6−
Kumamoto Region, Kumamoto Prefecture熊本県熊本地方
37
3
Aso Region, Kumamoto Prefecture熊本県阿蘇地方
28
4
Hyuganada Sea日向灘
26
4
Bungosuido Strait豊後水道
16
2
Western Oita Prefecture大分県西部
11
Reference model · not a forecast J-SHIS (NIED) · 250 m · 4931737714

Ground conditions near an observation station

J-SHIS data for the 250 m mesh containing 別府市鶴見.

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.

AVS30314.4 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×1.23

For the same incoming wave, local ground conditions may make peak-motion velocity at the surface about 23% 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) · A44202

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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#2Major active faultNishiyama fault zone (All segment)西山断層帯 (全体が同時に活動)

Modelled magnitude: M7.5

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#3Major active faultHaneyama-Kuenohirayama fault zone万年山−崩平山断層帯

Modelled magnitude: M6.8

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#4Major active faultSuonada fault zone (Main part segment)周防灘断層帯(周防灘断層帯主部区間)

Modelled magnitude: M7.0

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#5Major 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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#6Major 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

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#7Major 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

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#8Major 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

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#9Major 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

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#10Major 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

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#11Major 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

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#12Major 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

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#13Major 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

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#14Major active faultHijiu fault zone日出生断層帯

Modelled magnitude: M6.9

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#15Major 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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#16Major 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

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#17Major 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

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#18Major 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

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#19Major 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

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#20Major 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

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#21Major 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

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#22Major 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

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#23Major 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

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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.