We now know that great earthquakes can occur in the Pacific Northwest, similar to those that have happened in Chile (1960), Alaska (1964), Indonesia (2004) and Japan (2011). In plate tectonic terms, such earthquakes are associated with: divergent boundaries (rift zones) within continents O mantle hot spots transform boundaries such as the San Andreas O convergent boundaries O divergent boundaries at mid-ocean ridges

Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
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We now know that great earthquakes can
occur in the Pacific Northwest, similar to
those that have happened in Chile (1960),
Alaska (1964), Indonesia (2004) and Japan
(2011). In plate tectonic terms, such
earthquakes are associated with:
divergent boundaries (rift zones) within
continents
O mantle hot spots
transform boundaries such as the San
Andreas
O convergent boundaries
O divergent boundaries at mid-ocean ridges
Transcribed Image Text:We now know that great earthquakes can occur in the Pacific Northwest, similar to those that have happened in Chile (1960), Alaska (1964), Indonesia (2004) and Japan (2011). In plate tectonic terms, such earthquakes are associated with: divergent boundaries (rift zones) within continents O mantle hot spots transform boundaries such as the San Andreas O convergent boundaries O divergent boundaries at mid-ocean ridges
Most major oceanic tsunamis are caused
by:
displacement of water by uplift or
subsidence of the ocean floor during
faulting
O huge submarine volcanic eruptions
O sudden strike-slip movement of the
seafloor or continental shelf
O earthquake-induced shaking of soft
sediments
O earthquake (seismic) waves shaking the
water near the epicenter
Transcribed Image Text:Most major oceanic tsunamis are caused by: displacement of water by uplift or subsidence of the ocean floor during faulting O huge submarine volcanic eruptions O sudden strike-slip movement of the seafloor or continental shelf O earthquake-induced shaking of soft sediments O earthquake (seismic) waves shaking the water near the epicenter
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