Earthquake Magnitudes, Subduction Zones, and Tsunamis

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Vocabulary flashcards covering earthquake magnitude determinants, famous subduction zone megathrust events, and tsunami generation mechanisms from Chapter 1 to 5.

Last updated 5:54 AM on 9/30/26
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13 Terms

1
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Rupture area

A key factor controlling earthquake magnitude defined by how long a fault breaks and how deep the rupture extends into the Earth's crust.

2
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Fault slip

The distance or amount that two sides of a fault move past each other during an earthquake.

3
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Rock rigidity

Also referred to as rock stiffness, this property controls the amount of elastic energy that can build up before a fault breaks.

4
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Wilson Coversmith

Researchers associated with empirical relations that relate earthquake magnitude to rupture length, rupture area, and rupture dimensions.

5
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San Andreas Fault

A right-lateral strike-slip transform fault approximately 750 miles750\,\text{miles} long that is incapable of producing a magnitude 9.09.0 or greater earthquake due to its fault geometry.

6
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2011 Japan Earthquake

A magnitude 9.09.0 earthquake occurring in March 2011 offshore along the Japan Trench, caused by subduction of the Pacific plate beneath Japan.

7
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1964 Great Alaska Earthquake

A magnitude 9.29.2 earthquake occurring in Prince William Sound, recognized as the largest earthquake ever recorded in the United States and the second largest in history.

8
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George Placker

The USGS geologist who applied the newly forming theory of plate tectonics to explain the 1964 Alaska earthquake as a megathrust earthquake.

9
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Megathrust earthquake

A powerful earthquake produced by periodic slip along the low-angle interface where an oceanic plate subducts beneath an overriding continental plate.

10
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2004 Sumatra Earthquake

A massive subduction earthquake caused by the India plate subducting, where the fault rupture spread northward sequentially like a zipper.

11
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Thrust fault

A shallow-angle reverse fault where the overlying plate thrusts up over the subducting plate during convergent plate movement.

12
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Splay faulting

A phenomenon where displacement branches into steeply dipping faults off the main megathrust fault, causing concentrated ocean floor uplift and generating rapid, large tsunamis.

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Patton Bay Fault

A splay fault involved in the 1964 Alaska earthquake that experienced 9 meters9\,\text{meters} of displacement, causing localized uplift of the continental shelf.