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.
Tsuruga City earthquake and Shindo history in 2016
敦賀市
This annual view includes only earthquakes from 2016 for which stations associated with Tsuruga City recorded Shindo.
Data period: 1 January–31 December 2016In 2016, stations associated with Tsuruga City reported local Shindo for 5 earthquakes. The highest local level recorded that year was Shindo 3.
Observation history · 2016
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.
Observed events by year
Choose a year to update the event history and local Shindo distribution.
Shindo observed in this place
The highest reading from stations in this place, not the maximum Shindo of the whole event.
Observation history · 2016
5 observed earthquakes
- 震度2Nov 19, 2016, 11:48 JSTSouthern Wakayama PrefectureShindo in this place: 2 · Event maximum Shindo: 4M5.460 km
- 震度3Oct 21, 2016, 14:07 JSTCentral Tottori PrefectureShindo in this place: 3 · Event maximum Shindo: 6−M6.610 km
- 震度2Apr 16, 2016, 01:25 JSTKumamoto Region, Kumamoto PrefectureShindo in this place: 2 · Event maximum Shindo: 6+M7.110 km
- 震度2Apr 1, 2016, 11:39 JSTOff the southeast Coast of Mie PrefectureShindo in this place: 2 · Event maximum Shindo: 4M6.110 km
- 震度2Mar 7, 2016, 05:58 JSTWakasa BayShindo in this place: 2 · Event maximum Shindo: 2M4.010 km
Ground & J-SHIS
The context below uses the place's full available history and reference models; it is not part of the 2016 statistics.
Where the shaking usually comes from
Source regions of earthquakes observed here, ordered by the number of reports.
Ground conditions near an observation station
J-SHIS data for the 250 m mesh containing 敦賀市松栄町.
How to read these values
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.
For the same incoming wave, local ground conditions may make peak-motion velocity at the surface about 44% 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.
Earthquake scenarios affecting this place
Official J-SHIS models ranked for their potential impact on this municipality.
#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.
Modelled magnitude: M8.2–9.1
Read about this model #2Major active faultShufukuji fault zone集福寺断層Modelled magnitude: M6.5
Read about this model #3Other active faultMimi-kawa fault zone耳川断層帯Modelled magnitude: M6.6
Read about this model #4Major active faultYanagase/Sekigahara fault zone (Main part/Southern segment)柳ヶ瀬・関ヶ原断層帯主部南部Modelled magnitude: M7.0
Read about this model #5Major active faultUrazoko-Yanagaseyama fault zone浦底-柳ヶ瀬山断層帯Modelled magnitude: M6.7
Read about this model #6Major active faultYanagase/Sekigahara fault zone (Main part/Central segment)柳ヶ瀬・関ヶ原断層帯主部中部Modelled magnitude: M6.6
Read about this model #7Other active faultOkukawanami fault奥川並断層Modelled magnitude: M6.7
Read about this model #8Major active faultBiwako-seigan fault zone (Northern part)琵琶湖西岸断層帯北部Modelled magnitude: M6.6
Read about this model #9Other active faultMihama-wan-oki fault美浜湾沖断層Modelled magnitude: M7.0
Read about this model #10Major active faultYoro-Kuwana-Yokkaichi fault zone養老−桑名−四日市断層帯Modelled magnitude: M7.2
Read about this model #11Other active faultHosenji fault zone宝泉寺断層帯Modelled magnitude: M6.9
Read about this model #12Major active faultKohoku-sanchi fault zone (Northwestern part)湖北山地断層帯北西部Modelled magnitude: M6.7
Read about this model #13Major active faultNosaka fault zone野坂断層帯Modelled magnitude: M6.8
Read about this model #14Major active faultYanagase/Sekigahara fault zone (Main part/Northern segment)柳ヶ瀬・関ヶ原断層帯主部北部Modelled magnitude: M7.0
Read about this model #15Major active faultKohoku-sanchi fault zone (Southeastern part)湖北山地断層帯南東部Modelled magnitude: M6.4
Read about this model #16Major active faultMikata fault zone三方断層帯Modelled magnitude: M6.7
Read about this model #17Major active faultHanaore fault zone/Northern segment花折断層帯北部Modelled magnitude: M6.7
Read about this modelJ-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.
Nearby places
Municipalities nearest to the representative station position.
Understand local Shindo in context
Guides to this place’s history, seismic intensity and notification tools.
Shindo is Japan’s earthquake intensity scale. See what shaking each level means, from 0 to 7, and why a local Shindo reading is different from magnitude.
Read guide →10 min readHow to use the JISHINDESU interactive mapA guide to the redesigned map panel: adding and switching places, ten years of history, filters, local Shindo readings, sharing and notifications.
Read guide →6 min readAre earthquakes becoming more frequent in Japan?How to compare earthquake counts fairly—and why a few active days do not prove a lasting increase.
Read guide →4 min readAway from home? Monitor earthquakes in your Japanese townUse home as the reference point and receive notifications without an account when a station within the selected radius reports your chosen Shindo level.
Read guide →