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

Takayama City earthquake and Shindo history in 2019

高山市

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

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

In 2019, stations associated with Takayama City reported local Shindo for 30 earthquakes. The highest local level recorded that year was Shindo 3.

Observed events302019
Highest local Shindo32019
Data period: 1 January–31 December 2019 · 30 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 1, 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
1222632405−05+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
Hida, Gifu Prefecture岐阜県飛騨地方
243
3
Central Nagano Prefecture長野県中部
168
4
Southern Nagano Prefecture長野県南部
65
5−
Noto, Ishikawa Prefecture石川県能登地方
59
4
Eastern Toyama Prefecture富山県東部
28
3
Off the Coast of Noto Peninsula能登半島沖
22
Reference model · not a forecast J-SHIS (NIED) · 250 m · 5437128032

Ground conditions near an observation station

J-SHIS data for the 250 m mesh containing 高山市桐生町.

J-SHIS / NIED

How to read these values

Landform classAlluvial fan扇状地

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.

AVS30395.5 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×1.01

For the same incoming wave, local ground conditions may make peak-motion velocity at the surface about 1% 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) · A21203

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 faultKokufu fault zone高山・大原断層帯国府断層帯

Modelled magnitude: M6.6

Read about this model
#2Major active faultTakayama fault zone高山・大原断層帯高山断層帯

Modelled magnitude: M6.9

Read about this model
#3Major active faultSakaitoge-Kamiya fault zone (Main part)境峠・神谷断層帯主部

Modelled magnitude: M7.0

Read about this model
#4Other active faultKuchiudo-Yamanokuchi fault口有道-山之口断層

Modelled magnitude: M7.0

Read about this model
#5Major active faultInohana fault zone高山・大原断層帯猪之鼻断層帯

Modelled magnitude: M6.5

Read about this model
#6Major active faultItoigawa-Shizuoka-kozosen fault zone (All segment)糸魚川-静岡構造線断層帯(全体が同時に活動)

Modelled magnitude: M7.5

Read about this model
#7Other active faultFurukawa fault zone (Toichi-gawa fault)古川断層帯(戸市川断層)

Modelled magnitude: M6.8

Read about this model
#8Subduction-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
#9Major active faultAtera fault zone (Main part/Northern segment)阿寺断層帯主部北部

Modelled magnitude: M6.4

Read about this model
#10Major active faultShokawa fault zone庄川断層帯

Modelled magnitude: M7.2

Read about this model
#11Major active faultAtotsugawa fault zone跡津川断層帯

Modelled magnitude: M7.2

Read about this model
#12Major active faultAtera fault zone (Main part/Southern segment)阿寺断層帯主部南部

Modelled magnitude: M7.2

Read about this model
#13Major active faultUshikubi fault zone牛首断層帯

Modelled magnitude: M7.1

Read about this model
#14Major active faultInadani fault zone (Main part)伊那谷断層帯主部

Modelled magnitude: M7.3

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.