Goto City earthquake and Shindo history
五島市
Earthquakes for which stations associated with Goto City reported an actual Shindo observation.
Latest observation: Sep 19, 2026, 09:07 PM JSTLocal seismic profile
Since Mar 14, 2015, stations associated with Goto City have reported a local reading for 35 earthquakes. Shindo 1 was most common, while the highest local level, Shindo 3, was recorded 2 times.
Latest observationSep 19, 2026
Highest local Shindo3
Observed events35Mar 14, 2015–Sep 19, 2026
Associated observation stations9JMA
Latest observation: Sep 19, 2026
Recent observed earthquakes
No local observation in the last 7 days. Latest observation: Sep 19, 2026
震度1
Sep 19, 2026, 09:07 PM JSTAmakusanada Sea
震度1M4.4 · 10 km · 97 km
Aug 12, 2026, 01:05 PM JSTAmakusa and Ashikita Region, Kumamoto Prefecture
震度1M4.9 · 10 km · 163 km
Aug 6, 2026, 07:59 AM JSTAmakusa and Ashikita Region, Kumamoto Prefecture
震度1M5.1 · 10 km · 163 km
Jul 29, 2026, 10:19 PM JSTAmakusa and Ashikita Region, Kumamoto Prefecture
震度1M5.8 · 0 km · 156 km
Jul 28, 2026, 11:02 PM JSTKumamoto Region, Kumamoto Prefecture
震度1M4.8 · 10 km · 172 km
Jul 28, 2026, 05:08 PM JSTAmakusa and Ashikita Region, Kumamoto Prefecture
M6.1 · 0 km · 165 km
9 Associated observation stations
Open this place on the mapStations and strongest local observations
The map combines stations assigned to this place with earthquakes that produced its strongest local readings.
Mar 14, 2015 to Sep 19, 2026 · 35 records
Observation history
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: Mar 14, 2015
All yearsObserved events by year
Choose a year to update the event history and local Shindo distribution.
All years
All ShindoShindo observed in this place
The highest reading from stations in this place, not the maximum Shindo of the whole event.
Latest observation: Sep 19, 2026
Recent observed earthquakes
35 observed earthquakes
- 震度1Sep 19, 2026, 21:07 JSTAmakusanada SeaShindo in this place: 1 · Event maximum Shindo: 3M4.410 km
- 震度1Aug 12, 2026, 13:05 JSTAmakusa and Ashikita Region, Kumamoto PrefectureShindo in this place: 1 · Event maximum Shindo: 4M4.910 km
- 震度1Aug 6, 2026, 07:59 JSTAmakusa and Ashikita Region, Kumamoto PrefectureShindo in this place: 1 · Event maximum Shindo: 4M5.110 km
- 震度1Jul 29, 2026, 22:19 JSTAmakusa and Ashikita Region, Kumamoto PrefectureShindo in this place: 1 · Event maximum Shindo: 5−M5.80 km
- 震度1Jul 28, 2026, 23:02 JSTKumamoto Region, Kumamoto PrefectureShindo in this place: 1 · Event maximum Shindo: 4M4.810 km
- 震度1Jul 28, 2026, 17:08 JSTAmakusa and Ashikita Region, Kumamoto PrefectureShindo in this place: 1 · Event maximum Shindo: 5−M6.10 km
- 震度3Jul 28, 2026, 16:27 JSTKumamoto Region, Kumamoto PrefectureShindo in this place: 3 · Event maximum Shindo: 7M7.110 km
- 震度1Dec 22, 2023, 06:06 JSTOff the west Coast of Satsuma PeninsulaShindo in this place: 1 · Event maximum Shindo: 1M3.310 km
Ground & J-SHIS
A change in the number of observations cannot by itself predict a larger earthquake.
Local seismic profile
Where the shaking usually comes from
Source regions of earthquakes observed here, ordered by the number of reports.
3
Off the west Coast of Satsuma Peninsula薩摩半島西方沖
123
Kumamoto Region, Kumamoto Prefecture熊本県熊本地方
72
Adjacent Sea of Goto Islands五島列島近海
71
Amakusa and Ashikita Region, Kumamoto Prefecture熊本県天草・芦北地方
41
Amakusanada Sea天草灘
11
Off the west Coast of Ogasawara Islands小笠原諸島西方沖
1Local seismic profile
Recent observations in long-term context
A change in the number of observations cannot by itself predict a larger earthquake.
Reference model · not a forecast J-SHIS (NIED) · 250 m · 4928063613
J-SHIS / NIEDGround conditions near an observation station
J-SHIS data for the 250 m mesh containing 五島市木場町.
How to read these values
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.
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 36% 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.
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 Explained: What Levels 0–7 Mean
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 →