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LOCAL EARTHQUAKE HISTORY

Suwa City earthquake and Shindo history in 2022

諏訪市

This annual view includes only earthquakes from 2022 for which stations associated with Suwa City recorded Shindo.

Data period: 1 January–31 December 2022
Data period: 1 January–31 December 2022

In 2022, stations associated with Suwa City reported local Shindo for 2 earthquakes. The highest local level recorded that year was Shindo 3.

Observed events22022
Highest local Shindo32022
Data period: 1 January–31 December 2022 · 2 observed earthquakes

Observation history · 2022

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.

2022 · Shindo 2+ · Clear filters
First observation: Jan 30, 2015

Observed events by year

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

All years
2022

Shindo observed in this place

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

All Shindo
1122231405−05+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 2022 statistics.

Local seismic profile

Where the shaking usually comes from

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

3
Central Nagano Prefecture長野県中部
24
3
Southern Ibaraki Prefecture茨城県南部
21
3
Southern Nagano Prefecture長野県南部
18
2
Hida, Gifu Prefecture岐阜県飛騨地方
18
3
Off the Coast of Fukushima Prefecture福島県沖
17
4
Noto, Ishikawa Prefecture石川県能登地方
15
Reference model · not a forecast J-SHIS (NIED) · 250 m · 5438005842

Ground conditions near an observation station

J-SHIS data for the 250 m mesh containing 諏訪市湖岸通り.

J-SHIS / NIED

How to read these values

Landform classDelta and coastal lowland三角州・海岸低地

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.

AVS30188.9 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×1.90

For the same incoming wave, local ground conditions may make peak-motion velocity at the surface about 90% 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) · A20206

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 faultItoigawa-Shizuoka-kozosen fault zone (Central northern segment)糸魚川−静岡構造線断層帯中北部

Modelled magnitude: M7.0

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#2Subduction-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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#3Major active faultItoigawa-Shizuoka-kozosen fault zone (Central southern segment)糸魚川−静岡構造線断層帯中南部

Modelled magnitude: M6.8

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#4Major active faultSakaitoge-Kamiya fault zone (Main part)境峠・神谷断層帯主部

Modelled magnitude: M7.0

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#5Major active faultItoigawa-Shizuoka-kozosen fault zone (Northern segment/Central northern segment)糸魚川-静岡構造線断層帯(北部と中北部が同時に活動)

Modelled magnitude: M7.2

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#6Major active faultItoigawa-Shizuoka-kozosen fault zone (Northern segment/Central northern segment/Central southern segment)糸魚川-静岡構造線断層帯(北部と中北部と中南部が同時に活動)

Modelled magnitude: M7.4

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#7Major active faultItoigawa-Shizuoka-kozosen fault zone (Central northern segment/Central southern segment)糸魚川-静岡構造線断層帯(中北部と中南部が同時に活動)

Modelled magnitude: M7.1

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#8Subduction-zone earthquakeSagami Trough earthquakes (M8 class)相模トラフ沿いのM8クラスの地震

Modelled magnitude: M7.9–8.6

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#9Other active faultKirigamine fault zone霧ヶ峰断層帯

Modelled magnitude: M7.0

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#10Major active faultMutoyama-Narai fault zone霧訪山-奈良井断層帯

Modelled magnitude: M6.7

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#11Major active faultItoigawa-Shizuoka-kozosen fault zone (Southern segment)糸魚川−静岡構造線断層帯南部

Modelled magnitude: M7.0

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#12Major 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

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#13Major 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

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#14Major active faultItoigawa-Shizuoka-kozosen fault zone (Central southern segment/Southern segment)糸魚川-静岡構造線断層帯(中南部と南部が同時に活動)

Modelled magnitude: M7.3

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#15Major active faultInadani fault zone (Main part)伊那谷断層帯主部

Modelled magnitude: M7.3

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#16Major 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

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#17Major active faultNagano-bonchi-seien fault zone (All segment)長野盆地西縁断層帯(全体が同時に活動)

Modelled magnitude: M7.3

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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.