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This is a demonstration of the principle of elastic rebound for the cause and recurrence of earthquakes. Under the Elastic Rebound Theory, the continuous motion of plates on Earth causes stress to build up at the boundaries between the plates, where friction keeps the boundaries locked. Stress is continually building up, and earthquakes act to relieve that stress. In the demonstration, the two sides of a fault are represented by sandpaper-covered blocks resting on a sandpaper-covered board. A weight rests on the block to apply a chosen amount of pressure on the sandpaper (defining the frictional strength of the fault). A spring is attached to the block and to a string, on which a constant pull is maintained. This apparatus is used to discover when the stress causes the blocks to move. Conclusions on earthquake recurrence (seismicity) may then be drawn.
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No cost
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DLESE Catalog ID:
DLESE-000-000-006-231
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This resource is part of
'Demonstrations of Geophysical Principles Applicable to the Properties and Processes of the Earth's Interior'
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Author:
Jeffrey S. Barker Geological Sciences and Environmental Studies, Binghamton University |