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.
Ashikita Town earthquake and Shindo history in 2017
芦北町
This annual view includes only earthquakes from 2017 for which stations associated with Ashikita Town recorded Shindo.
Data period: 1 January–31 December 2017Data period: 1 January–31 December 2017
In 2017, stations associated with Ashikita Town reported local Shindo for 0 earthquakes. The highest local level recorded that year was Shindo 2.
Observed events02017
Highest local Shindo22017
Data period: 1 January–31 December 2017 · 0 observed earthquakes
2017 · Shindo 4+ · Clear filtersObservation 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.
First observation: May 27, 2015
All yearsObserved events by year
Choose a year to update the event history and local Shindo distribution.
2017
All ShindoShindo observed in this place
The highest reading from stations in this place, not the maximum Shindo of the whole event.
Data period: 1 January–31 December 2017
Observation history · 2017
0 observed earthquakes
No observed earthquakes match these filters.
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.
6−
Kumamoto Region, Kumamoto Prefecture熊本県熊本地方
2575−
Amakusa and Ashikita Region, Kumamoto Prefecture熊本県天草・芦北地方
2034
Hyuganada Sea日向灘
373
Aso Region, Kumamoto Prefecture熊本県阿蘇地方
93
Off the west Coast of Satsuma Peninsula薩摩半島西方沖
82
Off the east Coast of Osumi Peninsula大隅半島東方沖
7Reference model · not a forecast J-SHIS (NIED) · 250 m · 4830335934
J-SHIS / NIEDGround conditions near an observation station
J-SHIS data for the 250 m mesh containing 芦北町芦北.
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 57% 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) · A43482
J-SHIS / NIEDEarthquake 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.
#1Major active faultHinagu fault zone (Yatsushirokai segment)日奈久断層帯八代海区間
Modelled magnitude: M6.8
Read about this model #2Major active faultHinagu fault zone (Hinagu segment)日奈久断層帯日奈久区間Modelled magnitude: M6.9
Read about this model #3Major active faultHinagu fault zone (Hinagu segment/Yatsushirokai segment)日奈久断層帯（日奈久区間と八代海区間が同時に活動）Modelled magnitude: M7.2
Read about this model #4Major active faultHinagu fault zone (All segment)日奈久断層帯 (全体が同時に活動)Modelled magnitude: M7.3
Read about this model #5Major active faultHinagu fault zone (Takano-Shirahata segment/Hinagu segment)日奈久断層帯（高野-白旗区間と日奈久区間が同時に活動）Modelled magnitude: M7.1
Read about this model #6Other active faultMinamata fault zone水俣断層帯Modelled magnitude: M6.8
Read about this model #7Major active faultIzumi fault zone出水断層帯Modelled magnitude: M6.5
Read about this model #8Major active faultFutagawa fault zone (Uto segment/Uto-hanto-hokugan segment)布田川断層帯（宇土区間と宇土半島北岸区間が同時に活動）Modelled magnitude: M7.0
Read about this model #9Major active faultFutagawa/Hinagu fault zone (Futagawa segment/all segment of Hinagu fault zone)布田川断層帯・日奈久断層帯 (布田川区間と日奈久断層帯全体が同時に活動)Modelled magnitude: M7.4
Read about this model #10Major active faultFutagawa/Hinagu fault zone (Futagawa segment/Takano-Shirahata segment/Hinagu segment)布田川断層帯・日奈久断層帯（布田川区間と高野-白旗区間と日奈久区間が同時に活動）Modelled magnitude: M7.3
Read about this model #11Major active faultFutagawa fault zone (All segment)布田川断層帯 (全体が同時に活動)Modelled magnitude: M7.2
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.
Local seismic profile
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.
8 min readJapan’s Shindo Scale: Earthquake Intensity Levels 0–7
Learn what Japan’s Shindo earthquake intensity scale measures, what levels 0, 5 Lower, 5 Upper and 7 mean, and why Shindo 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 →