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LOCAL EARTHQUAKE HISTORY

Tateyama City earthquake and Shindo history in 2019

館山市

This annual view includes only earthquakes from 2019 for which stations associated with Tateyama City recorded Shindo.

Data period: 1 January–31 December 2019
Data period: 1 January–31 December 2019

In 2019, stations associated with Tateyama City reported local Shindo for 34 earthquakes. The highest local level recorded that year was Shindo 4.

Observed events342019
Highest local Shindo42019
Data period: 1 January–31 December 2019 · 34 observed earthquakes

Observation history · 2019

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.

2019 · Clear filters
First observation: Jan 26, 2015

Observed events by year

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

All years
2019

Shindo observed in this place

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

All Shindo
11721333415−05+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 2019 statistics.

Local seismic profile

Where the shaking usually comes from

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

4
Off the southeast Coast of Chiba Prefecture千葉県南東沖
48
4
Off the east Coast of Chiba Prefecture千葉県東方沖
48
4
Northwestern Chiba Prefecture千葉県北西部
33
3
Southern Ibaraki Prefecture茨城県南部
31
3
Southern Chiba Prefecture千葉県南部
21
3
Adjacent Sea of Izu-Oshima Island伊豆大島近海
18
Reference model · not a forecast J-SHIS (NIED) · 250 m · 5239368913

Ground conditions near an observation station

J-SHIS data for the 250 m mesh containing 館山市長須賀.

J-SHIS / NIED

How to read these values

Landform classMarine sand and gravel bars砂州・砂礫州

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.

AVS30166.0 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×2.12

For the same incoming wave, local ground conditions may make peak-motion velocity at the surface about 112% 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) · A12205

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.