Linog sa Sanriku (1933)

Linog sa Sanriku (1933)
	An banwaan nin Massakicho, Sola nin Ōfunato, Iwate pagkatapos kan pangyayari
	Linog sa Sanriku (1933) (Kinában)
UTC time	1933-03-02 17:30:59
Mga pangyayari nin ISC	Plantilya:EQ-isc-link
USGS-ANSS	ComCat
Lokal na petsa	Marso 3, 1933
Lokal na oras	02:30:48 JST
Magnitudo	8.4 Mw
Rarom	20 km (12 mi)
Episentro	39°7.7′N 144°7′E / 39.1283°N 144.117°ETagboan: 39°7.7′N 144°7′E / 39.1283°N 144.117°E
Tipo	Dip-slip – Intraplato
Apektadong mga lugar	Hapon
Dolnop	Maabot sa 28.7 m (94 ft); sa Ryori, Kesen, Iwate, Tōhoku
Mga nagadan	1,522 mga nagadan,; 1,542 nawawara,; 12,053 na katawo an nalugadan

An Linog sa Sanriku kan 1933 (昭和三陸地震, Shōwa Sanriku Jishin) nangyari sa Sanriku coast kan Rehiyon Tōhoku kan Honshū, Hapon kan Marso 2 na may moment magnitude na 8.4. An konektadong dolnop nagkawsa nin lakop na destroso.

Linog

An episentro yaon sa baybayon, 290 kilometres (180 mi) sa sirangan kan syudad nin Kamaishi, Iwate. An mayor na pagkabigla nangyari kan alas 02:31 nin aga lokal na oras kan Marso 3, 1933 (17:31 UTC Marso 2, 1933), asin nagsukol nin 8.4 sa moment magnitude scale.^[2] Ini yaon sa haros parehong kinamumugtakan kan linog sa Sanriku 1896 asin nangyari ini sa harayo sa banwaan na an pagyugyog dai man gayong nakadanyar. Mga tolong oras pagkatapos kan mayor na pagkabigla nagkaigwa nin magnitude na 6.8 aftershock, na sinundan nin 76 pang mga aftershock (na may magnitude na 5.0 o mas halangkaw pa) sa laog nin anom na bulan.^[3] Ini sarong intraplato na pangyayari na nangyari sa laog kan Plato nin Pasipiko,^[4]asin an focal mechanism nagpahiling nin normal na faulting. ^[5]

Danyos

Dawa ngani dikit an danyos na nagigibo gikan sa pagkabigla, an dolnop, na naitala na nakaabot sa langkaw na 28.7 metres (94 ft) sa Ōfunato, Iwate, nagkawsa nin mahiwas na danyos, asin nagraot nin kadakol na harong asin nagkawsa nin kadakol na kaswalti.^[6]An dolnop rinaot an labing 7,000 na harong sa amihanan na baybayon kan Hapon, na labing 4,885 an inanod. An dolnop naitala man sa Haway na may langkaw na 9.5 feet (2.9 m), asin nagresulta man sa kadikit na danyos.^[2] An bilang kan mga nagadan uminabot sa 1,522 katawo na kumpirmadong nagadan, 1,542 an nawawara, asin 12,053 an nalugadan. Pinakamasakitan an banwaan nin Tarō, Iwate (ngunyan parte kan syudad nin Miyako), na 98% kan mga harong kaini an nadestroso asin 42% kan populasyon kaini an nagadan.^[7]

Mga tala

↑ Kanamori, H. (1977), "The energy release in great earthquakes" (PDF), Journal of Geophysical Research, American Geophysical Union, 82 (20): 2981–2987, Bibcode:1977JGR....82.2981K, doi:10.1029/JB082i020p02981, archived from the original (PDF) on 2016-09-20, retrieved 2025-07-22
1 2 "Historical Earthquakes:The 1933 Sanriku earthquake". United States Geological Survey. 14 March 2008. Archived from the original on 2008-07-24. Retrieved 2008-07-16. Unknown parameter |url-status= ignored (help)
↑ The Meiji Sanriku Earthquake (June 15, 1896, M 8 1/2) and Sanriku Earthquake (March 3, 1933, M 8.1)
↑ "日本海溝・千島海溝周辺海溝型地震に関する専門調査会報告" by 日本海溝・千島海溝周辺海溝型地震に関する専門調査会
↑ Lay, T.; Ammon, C. J.; Kanamori, H.; Kim, M. J.; Xue, L. (2011), "Outer trench-slope faulting and the 2011 M w 9.0 off the Pacific coast of Tohoku Earthquake", Earth, Planets and Space, Springer Science+Business Media, 63 (7): 713, Bibcode:2011EP&S...63..713L, doi:10.5047/eps.2011.05.006 
↑ Masayuki Nakao, "The Great Meiji Sanriku Tsunami". Association for the Study of Failure
↑ Corkill, Edan, "Heights of survival", Japan Times, 12 June 2011, pp. 9–10.

Mga panluwas na takod

[1] Kanamori, H. (1977), "The energy release in great earthquakes" (PDF), Journal of Geophysical Research, American Geophysical Union, 82 (20): 2981–2987, Bibcode:1977JGR....82.2981K, doi:10.1029/JB082i020p02981, archived from the original (PDF) on 2016-09-20, retrieved 2025-07-22

[USGS-2] 1 2 "Historical Earthquakes:The 1933 Sanriku earthquake". United States Geological Survey. 14 March 2008. Archived from the original on 2008-07-24. Retrieved 2008-07-16. Unknown parameter |url-status= ignored (help)

[3] The Meiji Sanriku Earthquake (June 15, 1896, M 8 1/2) and Sanriku Earthquake (March 3, 1933, M 8.1)

[4] "日本海溝・千島海溝周辺海溝型地震に関する専門調査会報告" by 日本海溝・千島海溝周辺海溝型地震に関する専門調査会

[5] Lay, T.; Ammon, C. J.; Kanamori, H.; Kim, M. J.; Xue, L. (2011), "Outer trench-slope faulting and the 2011 M w 9.0 off the Pacific coast of Tohoku Earthquake", Earth, Planets and Space, Springer Science+Business Media, 63 (7): 713, Bibcode:2011EP&S...63..713L, doi:10.5047/eps.2011.05.006 

[6] Masayuki Nakao, "The Great Meiji Sanriku Tsunami". Association for the Study of Failure

[7] Corkill, Edan, "Heights of survival", Japan Times, 12 June 2011, pp. 9–10.

[1]

[2]

[3]

[4]

[5]

[6]

[7]