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LOCAL EARTHQUAKE HISTORY

Nemuro City earthquake and Shindo history in 2017

根室市

This annual view includes only earthquakes from 2017 for which stations associated with Nemuro City recorded Shindo.

Data period: 1 January–31 December 2017
Data period: 1 January–31 December 2017

In 2017, stations associated with Nemuro City reported local Shindo for 45 earthquakes. The highest local level recorded that year was Shindo 3.

Observed events452017
Highest local Shindo32017
Data period: 1 January–31 December 2017 · 45 observed earthquakes

Observation history · 2017

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.

2017 · Clear filters
First observation: Jan 16, 2015

Observed events by year

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

All years
2017

Shindo observed in this place

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

All Shindo
1352634405−05+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 2017 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 southeast Coast of the Nemuro Peninsula根室半島南東沖
198
5−
Off the Coast of Kushiro釧路沖
124
3
Off the east Coast of Hokkaido北海道東方沖
107
4
Off the southeast Coast of Etorofu Island択捉島南東沖
50
3
Adjacent Kunashiri Island国後島付近
44
3
Central and southern Kushiro Region, Hokkaido釧路地方中南部
28
Reference model · not a forecast J-SHIS (NIED) · 250 m · 6445749644

Ground conditions near an observation station

J-SHIS data for the 250 m mesh containing 根室市弥栄.

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.

AVS30175.1 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×2.02

For the same incoming wave, local ground conditions may make peak-motion velocity at the surface about 102% 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) · A01223

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.