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J-SHIS EARTHQUAKE SOURCE MODEL

Median Tectonic Line (MTL) fault zone (FROM Ishizuchi-sanmyaku-hokuen segment TO Iyonada segment)

中央構造線断層帯（石鎚山脈北縁区間～伊予灘区間が同時に活動）

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

Reference model · not a forecast
Modelled magnitudeMw 7.6

The range of earthquake sizes represented by the whole model.

Chance within 30 years—

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

Chance within 50 years—

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 7.6. Its source elements span depths of 2–16 km below the surface. It considers 2 rupture patterns; this is not the number of expected earthquakes.

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 depthShallow2 kmMid-range9 kmDeep16 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 7.6

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 years—Within 50 years—

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. Ainan Town
  2. Waki Town
  3. Yusuhara Town
  4. Saiki City
  5. Tsukumi City
  6. Bungo Ohno City
  7. Tabuse Town
  8. Uwajima City
  9. Yawatahama City
  10. Seiyo City
  11. Uchiko Town
  12. Ikata Town
Show 48 more places
  1. Usuki City
  2. Kudamatsu City
  3. Kitsuki City
  4. Yufu City
  5. Hikari City
  6. Hirao Town
  7. Ozu City
  8. Oita City
  9. Beppu City
  10. Himeshima Village
  11. Hiji Town
  12. Kaminoseki Town
  13. Kunisaki City
  14. Suo Oshima Town
  15. Hiroshima City Asaminami Ward
  16. Yanai City
  17. Iyo City
  18. Tobe Town
  19. Bungotakada City
  20. Usa City
  21. Kokonoe Town
  22. Toon City
  23. Shunan City
  24. Kumakogen Town
  25. Hiroshima City Naka Ward
  26. Hiroshima City Minami Ward
  27. Hiroshima City Nishi Ward
  28. Otake City
  29. Nakatsu City
  30. Hatsukaichi City
  31. Etajima City
  32. Fuchu Town
  33. Saka Town
  34. Hofu City
  35. Susaki City
  36. Niyodogawa Town
  37. Iwakuni City
  38. Matsuyama City
  39. Ochi Town
  40. Hiroshima City Higashi Ward
  41. Hiroshima City Aki Ward
  42. Kaita Town
  43. Okawa Village
  44. Hidaka Village
  45. Ibara City
  46. Takehara City
  47. Osakikamijima Town
  48. Imabari City

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
F0201GI
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
6
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
2–16 km
The modelled depth range below the ground surface.
Element length
30–92 km
The length of individual source elements, not necessarily the total length of a fault zone.
Element width
12–18 km
The width of the inclined source elements below ground.
Dip angle
40–90 °
The element’s tilt from horizontal: 0° is horizontal and 90° is vertical.
Strike
240.7–253.9 °
The compass direction in which an element extends, measured clockwise from north.
Rupture patterns
2
Alternative rupture arrangements or sequences considered by the model.
Display grid cells
49
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 →