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LOCAL EARTHQUAKE HISTORY

Oyodo Town earthquake and Shindo history in 2017

大淀町

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

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

In 2017, stations associated with Oyodo Town reported local Shindo for 3 earthquakes. The highest local level recorded that year was Shindo 1.

Observed events32017
Highest local Shindo12017
Data period: 1 January–31 December 2017 · 3 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: Jun 5, 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
132030405−05+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
Nara Prefecture奈良県
6
3
Kiisuido Strait紀伊水道
6
3
Southern Wakayama Prefecture和歌山県南部
5
4
Northern Osaka Prefecture大阪府北部
3
1
Northern Wakayama Prefecture和歌山県北部
3
2
Off the southeast Coast of Mie Prefecture三重県南東沖
2
Reference model · not a forecast J-SHIS (NIED) · 250 m · 5135466341

Ground conditions near an observation station

J-SHIS data for the 250 m mesh containing 大淀町土田.

J-SHIS / NIED

How to read these values

Landform classGravelly terrace砂礫質台地

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.

AVS30490.2 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×0.84

For the same incoming wave, local ground conditions may make peak-motion velocity at the surface about 16% 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) · A29442

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.

#1Major active faultMedian Tectonic Line (MTL) fault zone (Gojoya segment)中央構造線断層帯(五条谷区間)

Modelled magnitude: M6.8

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#2Other active faultMedian Tectonic Line Gojo中央構造線五条

Modelled magnitude: M7.4

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#3Subduction-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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#4Major active faultMedian Tectonic Line (MTL) fault zone (FROM Gojoya segment TO Sanuki-sanmyaku-nanen western segment)中央構造線断層帯(五条谷区間~讃岐山脈南縁西部区間が同時に活動)

Modelled magnitude: M7.7

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#5Major active faultMedian Tectonic Line (MTL) fault zone (FROM Gojoya segment TO Ishizuchi-sanmyaku-hokuen western segment)中央構造線断層帯(五条谷区間~石鎚山脈北縁西部区間が同時に活動)

Modelled magnitude: M7.7

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#6Major active faultMedian Tectonic Line (MTL) fault zone (FROM Gojoya segment TO Sanuki-sanmyaku-nanen eastern segment)中央構造線断層帯(五条谷区間~讃岐山脈南縁東部区間が同時に活動)

Modelled magnitude: M7.6

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#7Major active faultMedian Tectonic Line (MTL) fault zone (FROM Gojoya segment TO Kitan-kaikyo - Naruto-Kaikyo segment)中央構造線断層帯(五条谷区間~紀淡海峡-鳴門海峡区間が同時に活動)

Modelled magnitude: M7.4

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#8Major active faultMedian Tectonic Line (MTL) fault zone (FROM Gojoya segment TO Negoro segment)中央構造線断層帯(五条谷区間~根来区間が同時に活動)

Modelled magnitude: M7.1

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#9Major active faultNara-bonchi toen fault zone奈良盆地東縁断層帯

Modelled magnitude: M6.9

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#10Major active faultMedian Tectonic Line (MTL) fault zone (FROM Negoro segment TO Sanuki-sanmyaku-nanen western segment)中央構造線断層帯(根来区間~讃岐山脈南縁西部区間が同時に活動)

Modelled magnitude: M7.7

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#11Major active faultIkoma fault zone生駒断層帯

Modelled magnitude: M6.9

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#12Major active faultMedian Tectonic Line (MTL) fault zone (FROM Negoro segment TO Ishizuchi-sanmyaku-hokuen western segment)中央構造線断層帯(根来区間~石鎚山脈北縁西部区間が同時に活動)

Modelled magnitude: M7.6

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#13Major active faultMedian Tectonic Line (MTL) fault zone (FROM Negoro segment TO Sanuki-sanmyaku-nanen eastern segment)中央構造線断層帯(根来区間~讃岐山脈南縁東部区間が同時に活動)

Modelled magnitude: M7.5

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#14Major 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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#15Major 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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#16Major active faultMedian Tectonic Line (MTL) fault zone (FROM Kongo-sanchi-toen segment TO Ishizuchi-sanmyaku-hokuen western segment)中央構造線断層帯(金剛山地東縁区間~石鎚山脈北縁西部区間が同時に活動)

Modelled magnitude: M7.8

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#17Major active faultMedian Tectonic Line (MTL) fault zone (FROM 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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#18Major 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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#19Major active faultMedian Tectonic Line (MTL) fault zone (FROM Kongo-sanchi-toen segment TO Sanuki-sanmyaku-nanen western segment)中央構造線断層帯(金剛山地東縁区間~讃岐山脈南縁西部区間が同時に活動)

Modelled magnitude: M7.7

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#20Major active faultMedian Tectonic Line (MTL) fault zone (FROM Kongo-sanchi-toen segment TO Ishizuchi-sanmyaku-hokuen segment)中央構造線断層帯(金剛山地東縁区間~石鎚山脈北縁区間が同時に活動)

Modelled magnitude: M7.7

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#21Major active faultMedian Tectonic Line (MTL) fault zone (FROM Gojoya segment TO Ishizuchi-sanmyaku-hokuen segment)中央構造線断層帯(五条谷区間~石鎚山脈北縁区間が同時に活動)

Modelled magnitude: M7.7

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#22Major active faultMedian Tectonic Line (MTL) fault zone (FROM Kongo-sanchi-toen segment TO Sanuki-sanmyaku-nanen eastern segment)中央構造線断層帯(金剛山地東縁区間~讃岐山脈南縁東部区間が同時に活動)

Modelled magnitude: M7.6

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#23Major active faultMedian Tectonic Line (MTL) fault zone (FROM Kongo-sanchi-toen segment TO Kitan-kaikyo - Naruto-Kaikyo segment)中央構造線断層帯(金剛山地東縁区間~紀淡海峡-鳴門海峡区間が同時に活動)

Modelled magnitude: M7.5

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#24Major active faultMedian Tectonic Line (MTL) fault zone (FROM Kongo-sanchi-toen segment TO Negoro segment)中央構造線断層帯(金剛山地東縁区間~根来区間が同時に活動)

Modelled magnitude: M7.3

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#25Major active faultMedian Tectonic Line (MTL) fault zone (FROM Kongo-sanchi-toen segment TO Gojoya segment)中央構造線断層帯(金剛山地東縁区間~五条谷区間が同時に活動)

Modelled magnitude: M7.0

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#26Major 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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#27Major active faultMedian Tectonic Line (MTL) fault zone (FROM Negoro segment TO Houyo-kaikyo - Yufuin segment)中央構造線断層帯(根来区間~豊予海峡-由布院区間が同時に活動)

Modelled magnitude: M7.8

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#28Major active faultMedian Tectonic Line (MTL) fault zone (FROM Negoro segment TO Ishizuchi-sanmyaku-hokuen segment)中央構造線断層帯(根来区間~石鎚山脈北縁区間が同時に活動)

Modelled magnitude: M7.7

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#29Major active faultMedian Tectonic Line (MTL) fault zone (Kongo-sanchi-toen segment)中央構造線断層帯(金剛山地東縁区間)

Modelled magnitude: M6.4

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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.