Zona subduksi Cascadia: Perbedaan antara revisi
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== Pranala luar == |
== Pranala luar == |
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* {{cite web |title=Turbidite event history—Methods and implications for Holocene paleoseismicity of the Cascadia subduction zone |url=http://pubs.usgs.gov/pp/pp1661f |publisher=U.S. Geological Survey |id=Professional Paper 1661–F |editor=Robert Kayen |author=Chris Goldfinger |author2=C. Hans Nelson |author3=Ann E. Morey |author4=Joel E. Johnson |author5=Jason R. Patton |author6=Eugene Karabanov |author7=Julia Gutiérrez-Pastor |author8=Andrew T. Eriksson |author9=Eulàlia Gràcia |author10=Gita Dunhill |author11=Randolph J. Enkin |author12=Audrey Dallimore |author13=Tracy Vallier |year=2012}} |
* {{cite web |title=Turbidite event history—Methods and implications for Holocene paleoseismicity of the Cascadia subduction zone |url=http://pubs.usgs.gov/pp/pp1661f |publisher=U.S. Geological Survey |id=Professional Paper 1661–F |editor=Robert Kayen |author=Chris Goldfinger |author2=C. Hans Nelson |author3=Ann E. Morey |author4=Joel E. Johnson |author5=Jason R. Patton |author6=Eugene Karabanov |author7=Julia Gutiérrez-Pastor |author8=Andrew T. Eriksson |author9=Eulàlia Gràcia |author10=Gita Dunhill |author11=Randolph J. Enkin |author12=Audrey Dallimore |author13=Tracy Vallier |year=2012}} |
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* {{cite journal | author=Atwater, BF | title=Evidence for great Holocene earthquakes along the outer coast of Washington State| journal=[[Science (journal)|Science]] | volume=236 | issue=4804 | year=1987 | pages=942–44 | doi=10.1126/science.236.4804.942 | pmid=17812748|bibcode = 1987Sci...236..942A }} |
* {{cite journal | author=Atwater, BF | title=Evidence for great Holocene earthquakes along the outer coast of Washington State| journal=[[Science (journal)|Science]] | volume=236 | issue=4804 | year=1987 | pages=942–44 | doi=10.1126/science.236.4804.942 | pmid=17812748|bibcode = 1987Sci...236..942A }} |
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* [http://www.dailywireless.org/2009/04/21/cascadia-peril-09/ "Cascadia Peril '09"] at dailywireless.org |
* [http://www.dailywireless.org/2009/04/21/cascadia-peril-09/ "Cascadia Peril '09"] at dailywireless.org |
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Revisi per 29 Januari 2017 04.50
45°N 124°W / 45°N 124°W Zona subduksi Cascadia (juga disebut sebagai sesar Cascadia) adalah sebuah batas lempeng konvergen yang membentang dari utara Pulau Vancouver sampai utara California. Sesar tersebut merupakan sebuah zona subduksi yang sangat panjang yang memisahkan lempeng Penjelajah, Juan de Fuca, dan Gorda, di satu sisi, dan Lempeng Amerika Utara, di sisi yang lain.
Kota-kota besar yang akan terkena dampak gangguan zona subduksi tersebut meliputi Vancouver dan Victoria, British Columbia; Seattle, Washington; and Portland, Oregon.
Referensi
Pranala luar
- Chris Goldfinger; C. Hans Nelson; Ann E. Morey; Joel E. Johnson; Jason R. Patton; Eugene Karabanov; Julia Gutiérrez-Pastor; Andrew T. Eriksson; Eulàlia Gràcia; Gita Dunhill; Randolph J. Enkin; Audrey Dallimore; Tracy Vallier (2012). Robert Kayen, ed. "Turbidite event history—Methods and implications for Holocene paleoseismicity of the Cascadia subduction zone". U.S. Geological Survey. Professional Paper 1661–F.
- Atwater, BF (1987). "Evidence for great Holocene earthquakes along the outer coast of Washington State". Science. 236 (4804): 942–44. Bibcode:1987Sci...236..942A. doi:10.1126/science.236.4804.942. PMID 17812748.
- "Cascadia Peril '09" at dailywireless.org
- 9.0 Shakemap Scenario
- The Really Big One – University of California Television
- Great Earthquakes of the Pacific Northwest – Central Washington University