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LOCAL EARTHQUAKE HISTORY

Hiranai Town earthquake and Shindo history in 2015

平内町

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

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

In 2015, stations associated with Hiranai Town reported local Shindo for 18 earthquakes. The highest local level recorded that year was Shindo 4.

Observed events182015
Highest local Shindo42015
Data period: 1 January–31 December 2015 · 18 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 17, 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
162833415−05+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.

5−
Off the east Coast of Aomori Prefecture青森県東方沖
140
4
Off the Coast of Iwate Prefecture岩手県沖
56
4
Off the Coast of Sanriku三陸沖
36
4
Off the Coast of Urakawa浦河沖
17
4
Mutsu Bay陸奥湾
11
3
Off the Coast of Miyagi Prefecture宮城県沖
11
Reference model · not a forecast J-SHIS (NIED) · 250 m · 6140371612

Ground conditions near an observation station

J-SHIS data for the 250 m mesh containing 平内町小湊.

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.

AVS30364.9 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×1.08

For the same incoming wave, local ground conditions may make peak-motion velocity at the surface about 8% 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) · A02301

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.

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.