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Earthquakes can be produced at any plate boundary, however, subduction zones generally create the world's largest, most destructive ruptures. In the image above, the larger the magnitude of the earthquake, the brighter the color. These large ruptures are seen clearly as the Pacific Ring of Fire. Image Credit: John Nelson, IDV Solutions. This site is under construction. Off the east coast of Honshu Island, Japan. East of South Sandwich Islands, South Atlantic. Off the west coast of Etchoropo, Mexico.

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Tectonophysics.com | Under Construction | tectonophysics.com Reviews
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Earthquakes can be produced at any plate boundary, however, subduction zones generally create the world's largest, most destructive ruptures. In the image above, the larger the magnitude of the earthquake, the brighter the color. These large ruptures are seen clearly as the Pacific Ring of Fire. Image Credit: John Nelson, IDV Solutions. This site is under construction. Off the east coast of Honshu Island, Japan. East of South Sandwich Islands, South Atlantic. Off the west coast of Etchoropo, Mexico.
<META>
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1 dynamic regions
2 japan
3 san andreas
4 geological terms
5 subduction
6 thrust faults
7 coming soon
8 recent large seismicity
9 date
10 magnitude
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Tectonophysics.com | Under Construction | tectonophysics.com Reviews

https://tectonophysics.com

Earthquakes can be produced at any plate boundary, however, subduction zones generally create the world's largest, most destructive ruptures. In the image above, the larger the magnitude of the earthquake, the brighter the color. These large ruptures are seen clearly as the Pacific Ring of Fire. Image Credit: John Nelson, IDV Solutions. This site is under construction. Off the east coast of Honshu Island, Japan. East of South Sandwich Islands, South Atlantic. Off the west coast of Etchoropo, Mexico.

INTERNAL PAGES

tectonophysics.com tectonophysics.com
1

Tectonophysics.com | Under Construction

http://www.tectonophysics.com/Japan/Japan.html

This site is under construction. The tectonic regime of Japan is complex. Off the northeast coast of Honshu Island, the Pacific plate subducts below the Eurasian plate at the Japan Trench. Off the southeast coast of Japan, the Philippine Sea plate subducts below the Eurasian plate at the Nankai Trough. These zones produce some of the world's largest megathrust rupture events and subsequent tsunamis. Hover over the image for a larger view.

2

Tectonophysics.com | Under Construction

http://www.tectonophysics.com/ThrustFaults/Thrust.html

This site is under construction. Thrust faults are a result of convergence. One side of the fault is called the hanging wall and the other side is called the footwall. Miners first used these terms, because they can hang their hats on the hanging wall and walk on the footwall. In thrust faults, the hanging wall moves up relative to the footwall. Thrust faults are reverse faults with smaller angles not exceeding 40 degrees.

3

Tectonophysics.com | Under Construction

http://www.tectonophysics.com/Subduction/subduction.html

This site is under construction. Subduction zones produce the majority of the world's large rupture events and tsunamis. The ground ruptures (breaks/snaps) during seismic events, which is why the term "rupture event" can be used for "earthquake". Subduction zones are the result of oceanic lithosphere sliding below either another oceanic plate or continental lithosphere.

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Earthquakes can be produced at any plate boundary, however, subduction zones generally create the world's largest, most destructive ruptures. In the image above, the larger the magnitude of the earthquake, the brighter the color. These large ruptures are seen clearly as the Pacific Ring of Fire. Image Credit: John Nelson, IDV Solutions. This site is under construction. Off the east coast of Honshu Island, Japan. East of South Sandwich Islands, South Atlantic. Off the west coast of Etchoropo, Mexico.

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