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LOCAL EARTHQUAKE HISTORY

Noto Town earthquake and Shindo history in 2018

能登町

This annual view includes only earthquakes from 2018 for which stations associated with Noto Town recorded Shindo.

Data period: 1 January–31 December 2018
Data period: 1 January–31 December 2018

In 2018, stations associated with Noto Town reported local Shindo for 1 earthquakes. The highest local level recorded that year was Shindo 1.

Observed events12018
Highest local Shindo12018
Data period: 1 January–31 December 2018 · 1 observed earthquakes

Observation history · 2018

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.

2018 · 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
2018

Shindo observed in this place

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

All Shindo
112030405−05+06−06+070
Data period: 1 January–31 December 2018

Observation history · 2018

1 observed earthquakes

  1. 震度1Dec 20, 2018, 15:58 JSTEastern Toyama PrefectureShindo in this place: 1 · Event maximum Shindo: 3M4.210 km
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 2018 statistics.

Local seismic profile

Where the shaking usually comes from

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

6−
Noto, Ishikawa Prefecture石川県能登地方
276
4
Off the Coast of Noto Peninsula能登半島沖
53
4
Adjacent Sado佐渡付近
18
4
Off the west Coast of Ishikawa Prefecture石川県西方沖
16
3
Off the Coast of Joetsu and Chuetsu, Niigata Prefecture新潟県上中越沖
13
2
Toyama Bay富山湾
5
Reference model · not a forecast J-SHIS (NIED) · 250 m · 5537717123

Ground conditions near an observation station

J-SHIS data for the 250 m mesh containing 能登町宇出津.

J-SHIS / NIED

How to read these values

Landform classValley bottom lowland谷底低地

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.

AVS30268.7 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×1.40

For the same incoming wave, local ground conditions may make peak-motion velocity at the surface about 40% 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) · A17463

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.