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.
Sukumo City earthquake and Shindo history in 2022
宿毛市
This annual view includes only earthquakes from 2022 for which stations associated with Sukumo City recorded Shindo.
Data period: 1 January–31 December 2022In 2022, stations associated with Sukumo City reported local Shindo for 29 earthquakes. The highest local level recorded that year was Shindo 5−.
Observation history · 2022
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 · 2022
29 observed earthquakes
- 震度1Dec 18, 2022, 03:06 JSTHyuganada SeaShindo in this place: 1 · Event maximum Shindo: 4M5.430 km
- 震度1Dec 11, 2022, 06:17 JSTBungosuido StraitShindo in this place: 1 · Event maximum Shindo: 1M3.340 km
- 震度1Nov 22, 2022, 10:24 JSTBungosuido StraitShindo in this place: 1 · Event maximum Shindo: 2M3.750 km
- 震度1Oct 13, 2022, 08:32 JSTBungosuido StraitShindo in this place: 1 · Event maximum Shindo: 1M2.740 km
- 震度1Oct 2, 2022, 00:02 JSTOff the east Coast of Osumi PeninsulaShindo in this place: 1 · Event maximum Shindo: 5−M5.830 km
- 震度1Aug 3, 2022, 20:20 JSTNanyo, Ehime PrefectureShindo in this place: 1 · Event maximum Shindo: 1M3.230 km
- 震度2Jun 14, 2022, 06:01 JSTBungosuido StraitShindo in this place: 2 · Event maximum Shindo: 2M4.150 km
- 震度1Jun 14, 2022, 00:58 JSTBungosuido StraitShindo in this place: 1 · Event maximum Shindo: 2M3.850 km
Ground & J-SHIS
The context below uses the place's full available history and reference models; it is not part of the 2022 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 宿毛市片島.
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 14% 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 #2Other active faultSukumo-Nakamura fault zone宿毛-中村断層帯Modelled magnitude: M7.2
Read about this model #3Major active faultMedian Tectonic Line (MTL) fault zone (All segment)中央構造線断層帯(全体が同時に活動)Modelled magnitude: M7.9
Read about this model #4Major active faultMedian Tectonic Line (MTL) fault zone (FROM Gojoya segment TO Houyo-kaikyo - Yufuin segment)中央構造線断層帯(五条谷区間~豊予海峡-由布院区間が同時に活動)Modelled magnitude: M7.9
Read about this model #5Major active faultMedian Tectonic Line (MTL) fault zone (FROM Kongo-sanchi-toen segment TO Iyonada segment)中央構造線断層帯(金剛山地東縁区間~伊予灘区間が同時に活動)Modelled magnitude: M7.8
Read about this model #6Major active faultMedian Tectonic Line (MTL) fault zone (FROM Gojoya segment TO Iyonada segment)中央構造線断層帯(五条谷区間~伊予灘区間が同時に活動)Modelled magnitude: M7.8
Read about this model #7Major active faultMedian Tectonic Line (MTL) fault zone (FROM Negoro segment TO Iyonada segment)中央構造線断層帯(根来区間~伊予灘区間が同時に活動)Modelled magnitude: M7.8
Read about this model #8Major active faultMedian Tectonic Line (MTL) fault zone (FROM Kitan-kaikyo - Naruto-Kaikyo segment TO Houyo-kaikyo - Yufuin segment)中央構造線断層帯(紀淡海峡-鳴門海峡区間~豊予海峡-由布院区間が同時に活動)Modelled magnitude: M7.8
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.
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 →