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.
Makurazaki City earthquake and Shindo history in 2017
枕崎市
This annual view includes only earthquakes from 2017 for which stations associated with Makurazaki City recorded Shindo.
Data period: 1 January–31 December 2017In 2017, stations associated with Makurazaki City reported local Shindo for 19 earthquakes. The highest local level recorded that year was Shindo 4.
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.
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 · 2017
19 observed earthquakes
- 震度1Nov 22, 2017, 11:16 JSTKagoshima BayShindo in this place: 1 · Event maximum Shindo: 2M2.810 km
- 震度3Nov 1, 2017, 00:46 JSTKagoshima BayShindo in this place: 3 · Event maximum Shindo: 4M3.710 km
- 震度1Oct 15, 2017, 08:34 JSTOff the west Coast of Satsuma PeninsulaShindo in this place: 1 · Event maximum Shindo: 2M4.6140 km
- 震度1Oct 2, 2017, 04:20 JSTAdjacent Sea of Tanegashima IslandShindo in this place: 1 · Event maximum Shindo: 1M4.140 km
- 震度3Aug 24, 2017, 14:34 JSTKagoshima BayShindo in this place: 3 · Event maximum Shindo: 4M4.510 km
- 震度1Aug 10, 2017, 22:02 JSTKagoshima BayShindo in this place: 1 · Event maximum Shindo: 2M2.810 km
- 震度1Aug 9, 2017, 05:57 JSTAmakusa and Ashikita Region, Kumamoto PrefectureShindo in this place: 1 · Event maximum Shindo: 2M3.010 km
- 震度1Aug 4, 2017, 10:15 JSTOff the west Coast of Satsuma PeninsulaShindo in this place: 1 · Event maximum Shindo: 1M3.30 km
Ground & J-SHIS
The context below uses the place's full available history and reference models; it is not part of the 2017 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 枕崎市高見町.
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 42% 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.
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 →