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J-SHIS EARTHQUAKE SOURCE MODEL

Futagawa 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）

What this earthquake source model represents and how to read its data.

Reference model · not a forecast
Modelled magnitudeMw 7

The range of earthquake sizes represented by the whole model.

Chance within 30 years0.13%

The long-term chance that an earthquake represented by this model occurs within that period.

Chance within 50 years0.21%

The long-term chance that an earthquake represented by this model occurs within that period.

This model in plain language

J-SHIS classifies this as a major active-fault model. It represents the underground area that may rupture along the fault, not one predicted earthquake. The model covers an overall magnitude of Mw 7. Its source elements span depths of 3–16.86 km below the surface. Its 30-year long-term probability is 0.13%, not a prediction of a date.

Japan terrain and the source model in 3D

Use the terrain map and city labels to locate the approximate source area, then switch below ground to inspect its generalised extent and depth. It does not reproduce the original source elements or show future epicentres or rupture progression.

Ctrl-drag to tilt · city names remain visible on the map

Colour shows generalised depthShallow3 kmMid-range9.9 kmDeep16.9 km

The 3D terrain gives geographic and city context. The coloured surfaces are coarse regular display cells projected from the underground source area—not the original J-SHIS geometry. They do not show future epicentres or shaking intensity.

How to read the model data

Modelled magnitudeMw 7

Magnitude describes the overall size of the modelled earthquake, not the Shindo felt in a particular place. The same magnitude can produce different shaking depending on distance, depth and ground conditions. A range shows both model limits.

Occurrence probability
Within 30 years0.13%Within 50 years0.21%

Probabilities are long-term values in the Y2020 model. They do not predict an earthquake on a particular day, in a particular year or at one exact location. Some models do not provide a value.

Places where J-SHIS considers this model

In J-SHIS calculations, this model is among the leading earthquake sources for these places. It does not mean the earthquake will start inside their boundaries or that every place would shake in the same way.

  1. Kikuchi City
  2. Gyokuto Town
  3. Ozu Town
  4. Minamiaso Village
  5. Kumamoto Kita Ward
  6. Aso City
  7. Koshi City
  8. Kumamoto
  9. Arao City
  10. Tamana City
  11. Yamaga City
  12. Nagasu Town
Show 29 more places
  1. Nagomi Town
  2. Kikuyo Town
  3. Nishihara Village
  4. Hikawa Town
  5. Omuta City
  6. Western Yatsushiro City
  7. Mifune Town
  8. Mashiki Town
  9. Kosa Town
  10. Shimabara City
  11. Kumamoto Chuo Ward
  12. Kumamoto Higashi Ward
  13. Kamiamakusa City
  14. Uki City
  15. Amakusa City
  16. Unzen City
  17. Minamishimabara City
  18. Yamato Town
  19. Reihoku Town
  20. Tara Town
  21. Nagasaki
  22. Isahaya City
  23. Uto City
  24. Kashima Town
  25. Kumamoto Nishi Ward
  26. Ashikita Town
  27. Kumamoto Minami Ward
  28. Saga
  29. Fukuoka

Technical model data

J-SHIS identifiers and calculation parameters. You do not need them for an everyday reading of this page.

Model version
Y2020
The edition of J-SHIS data used on this page.
Probability case
MAX
MAX is the J-SHIS calculation case used on this page. It does not mean a certain ‘worst case’ event.
J-SHIS code
F01300D
The identifier used for this model inside J-SHIS.
Estimation method code
SIM
An abbreviation for the statistical process used to calculate probability. It is not a danger grade.
Source elements
2
Source elements are the pieces J-SHIS uses to build the source shape. A larger count means a more detailed or complex model; it is not a hazard score, a fault count or the number of expected earthquakes.
Depth
3–16.86 km
The modelled depth range below the ground surface.
Element length
22–32 km
The length of individual source elements, not necessarily the total length of a fault zone.
Element width
16 km
The width of the inclined source elements below ground.
Dip angle
60 °
The element’s tilt from horizontal: 0° is horizontal and 90° is vertical.
Strike
236.1–243.2 °
The compass direction in which an element extends, measured clockwise from north.
Display grid cells
15
Regular aggregated grid cells used to depict the source area. This is not the number of source records or original shapes.

Source and limitations

Source: J-SHIS, operated by Japan’s National Research Institute for Earth Science and Disaster Resilience (NIED). JISHINDESU organises the Y2020 maximum-case data for presentation. This page is not an earthquake prediction, building-safety assessment or evacuation notice. Use current JMA and local-authority information for safety decisions.

In accordance with the J-SHIS terms, we publish only model-level summaries and coarse display geometry that cannot reproduce the original vertex sequences. This is not a redistributed copy of the source dataset.

Data retrieved: 05/09/2026

Open the source data in J-SHIS ↗J-SHIS terms of use ↗Explore local earthquake history →