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

Iida City earthquake and Shindo history in 2015

飯田市

This annual view includes only earthquakes from 2015 for which stations associated with Iida City recorded Shindo.

Data period: 1 January–31 December 2015
Data period: 1 January–31 December 2015

In 2015, stations associated with Iida City reported local Shindo for 10 earthquakes. The highest local level recorded that year was Shindo 2.

Observed events102015
Highest local Shindo22015
Data period: 1 January–31 December 2015 · 10 observed earthquakes

Observation history · 2015

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.

2015 · Clear filters
First observation: Feb 7, 2015

Observed events by year

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

All years
2015

Shindo observed in this place

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

All Shindo
172330405−05+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 2015 statistics.

Local seismic profile

Where the shaking usually comes from

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

3
Southern Nagano Prefecture長野県南部
22
2
Southern Ibaraki Prefecture茨城県南部
12
3
Off the Coast of Fukushima Prefecture福島県沖
11
3
Noto, Ishikawa Prefecture石川県能登地方
10
2
Western Aichi Prefecture愛知県西部
10
1
Hida, Gifu Prefecture岐阜県飛騨地方
9
Reference model · not a forecast J-SHIS (NIED) · 250 m · 5337261642

Ground conditions near an observation station

J-SHIS data for the 250 m mesh containing 飯田市馬場町.

J-SHIS / NIED

How to read these values

Landform classTerrace covered with volcanic ash soil火山灰台地

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.

AVS30368.2 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×1.07

For the same incoming wave, local ground conditions may make peak-motion velocity at the surface about 7% 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) · A20205

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 faultShimoina-ryuto fault zone下伊那竜東断層帯

Modelled magnitude: M7.2

Read about this model
#3Major active faultInadani fault zone (Southeastern part)伊那谷断層帯南東部

Modelled magnitude: M6.8

Read about this model
#4Other active faultMedian Tectonic Line-Akaishi-sanchi-seien fault zone中央構造線赤石山地西縁断層帯

Modelled magnitude: M7.7

Read about this model
#5Major active faultEnasan-Sanageyamakita fault zone恵那山-猿投山北断層帯

Modelled magnitude: M7.2

Read about this model
#6Major active faultSeinaiji toge fault zone清内路峠断層帯

Modelled magnitude: M6.8

Read about this model
#7Other active faultHiraoka fault平岡断層

Modelled magnitude: M7.0

Read about this model
#8Major 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
#9Major active faultItoigawa-Shizuoka-kozosen fault zone (Central northern segment/Central southern segment/Southern segment)糸魚川-静岡構造線断層帯(中北部と中南部と南部が同時に活動)

Modelled magnitude: M7.4

Read about this model
#10Major active faultInadani fault zone (Main part)伊那谷断層帯主部

Modelled magnitude: M7.3

Read about this model
#11Major 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
#12Major active faultKiso-sanmyaku-seien fault zone (Main part/Northern segment)木曽山脈西縁断層帯主部北部

Modelled magnitude: M6.9

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.