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Kyoto Prefecture (京都府) — Earthquake Risk & History

Kinki region · Based on HERP official data

Risk Level: High

Kyoto's millennium of accumulated wooden cultural heritage makes earthquake damage uniquely devastating to world heritage. The Arima-Takatsuki Fault Zone and Yamasiro Basin faults encircle the city, and basin topography amplifies ground motion.

Fault Lines & Seismic Characteristics

Active Faults & Trenches

  • Yamashiro Basin Fault Zone
  • Arima–Takatsuki Fault Zone
  • Hokusetsu Fault Zone

Seismic Characteristics

The Arima-Takatsuki Fault Zone runs east–west through southern Kyoto Prefecture, capable of an M7.5 earthquake. Multiple faults encircle the Yamasiro Basin beneath Kyoto City, causing seismic wave amplification. Kyoto is inland with no tsunami risk, but a direct strike would cause catastrophic loss of wooden cultural heritage.

Earthquake History

  • M7.3

    1995

    Hanshin-Awaji Earthquake — Intensity 4–5 in Kyoto; some older buildings damaged

    📖 Wikipedia
  • M6.5

    1830

    Kyoto earthquake — direct strike beneath the city; ~280 dead; extensive temple and shrine damage

  • M7.5

    1596

    Keicho Fushimi earthquake — Fushimi Castle collapsed; widespread damage across Kyoto

※ Showing M6+ or historically significant events. Source: JMA database and historical earthquake records.

Future Probability — HERP Official Assessment

30-Year Probability (Official Figure)

수% 이하 — M7.5 earthquake on the Arima-Takatsuki Fault Zone (30-year window)

Long-term evaluation by the Earthquake Research Committee. Recurrence interval is thousands of years, but a Kyoto direct earthquake would produce Intensity 7 and cause massive cultural heritage loss.

Traveler Safety Information

Finding Evacuation Shelters

  • Search "避難所" (hinanjo) on Google Maps to find the nearest shelter from your current location
  • Install NHK World or Safety tips (Japan Tourism Agency app) — both send English earthquake alerts
  • Kyoto Prefecture official disaster prevention page (Japanese) — includes shelter maps

Basic Action Rules

  • At check-in, locate emergency exits and escape routes
  • On strong shaking: protect your head, open a door to secure an exit, do not use elevators
  • Near coasts or rivers: move to high ground immediately — do not wait for a tsunami warning
  • Emergency numbers: Police 110 · Ambulance/Fire 119
  • Contact your embassy in Tokyo for emergency consular assistance

Research & Official Sources AI summary

  • Kyoto's cultural heritage and earthquake risk

    Kyoto's extraordinary concentration of wooden UNESCO World Heritage buildings face severe vulnerability to a direct earthquake. A major event would cause cultural heritage loss alongside infrastructure collapse.

    Source: 교토부 문화환경부 (2021)
  • Basin amplification effect in the Kyoto Basin

    The Kyoto Basin is enclosed by mountains on all sides, causing seismic wave amplification through repeated internal reflection. The same magnitude earthquake produces stronger shaking inside the Kyoto Basin than in open terrain.

    Source: 교토대학 방재연구소 (2022)

Related Guides

⚠️ Notice
Seismic characteristics and research summaries on this page are AI-generated from publicly available data by JMA, Cabinet Office, and HERP. Historical earthquake data (year, magnitude, damage) is based on official records, but key figures should always be cross-checked with the latest official sources. This page does not predict future earthquakes.