Tanna Fault
Tanna Fault (丹那断層, Tanna Dansō) is a left lateral strike-slip fault which runs along the northeast side of Izu Peninsula south 30 km to Izu City in Japan. It was responsible for the magnitude 7.0 1930 North Izu earthquake (北伊豆地震).[1]
References
- ^ Shimazaki, K.; Somerville, P. (1979), "Static and dynamic parameters of the Izu-Oshima, Japan earthquake of January 14, 1978", Bulletin of the Seismological Society of America, 69 (5), Seismological Society of America: 1343
External links
- Kannami official website (Japanese)
- Masato Koyama's Home Page - Shizuoka University (Japanese)
Wikimedia Commons has media related to Tanna Fault.
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Tectonic plates of East and North Asia (Eurasian Plate-Pacific Plate Convergence Zone)
- Amur Plate
- Okhotsk Plate
- Philippine Sea Plate
- Yangtze Plate
- Mariana Plate
- Okinawa Plate
- Philippine Mobile Belt
- Aomori Bay West Coast Fault Zone
- Baikal Rift Zone
- Haiyuan Fault
- Fukozu Fault
- Futagawa-Hinagu fault zone
- Idosawa Fault
- Itoigawa-Shizuoka Tectonic Line
- Izu–Bonin–Mariana Arc
- Japan Median Tectonic Line
- Longmenshan Fault
- Neodani Fault
- Nojima Fault
- Northeastern Japan Arc
- Philippine Fault System
- Senya Fault
- Tanna Fault
- Ulakhan Fault
- Urasoko fault
35°05′47″N 139°01′04″E / 35.09639°N 139.01778°E / 35.09639; 139.01778