Tanna Fault

Relief Map. Tanna Fault (right)

Tanna Fault surface rupture

Ravine of Tanna Fault viewed from N

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, Seismological Society of America, 69 (5): 1343

External links

Kannami official website (Japanese)
Masato Koyama's Home Page - Shizuoka University (Japanese)

Wikimedia Commons has media related to Tanna Fault.

Tectonic plates of East Asia (Eurasian Plate-Pacific Plate Convergence Zone)

Large	Amur Plate Okhotsk Plate Philippine Sea Plate Yangtze Plate

Small	Mariana Plate Okinawa Plate Philippine Mobile Belt

Faults and rift zones	Baikal Rift Zone Fukozu Fault 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

Trenches and troughs	Kuril Trench Mariana Trench Japan Izu-Ogasawara Trench Japan Trench Nankai Trough Sagami Trough Suruga Trough Okinawa Trough Ryukyu Trench Philippines Manila Trench Philippine Trench East Luzon Trench

Other	Boso Triple Junction

Coordinates: 35°05′47″N 139°01′04″E / 35.09639°N 139.01778°E / 35.09639; 139.01778

This article is issued from Wikipedia - version of the 9/9/2016. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.