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Earthquake Machine
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.
Intended for grade levels:
  • Middle (6-8)
  • High (9-12)
  • College (13-14)
Type of resource:
  • For the classroom:
    • Presentation / Demo
Subject:
  • Geological Sciences:
    • Geophysics
  • Natural hazards
Technical requirements:
No specific technical requirements, just a browser required
Cost / Copyright:
No cost
Copyright and Other Restrictions Information is Unknown
DLESE Catalog ID: DLESE-000-000-006-231
Educational standards:
  • National Science Education Standards (NSES):
    • 5-8:
      • Unifying concepts and processes:
        • Evidence, models, and explanation
      • B - Physical science:
        • Motion and forces
      • D - Earth and space science:
        • Structure of the earth system
    • 9-12:
      • Unifying concepts and processes:
        • Evidence, models, and explanation
      • B - Physical science:
        • Motions and forces
      • D - Earth and space science:
        • Energy in the earth system
Related resources:
This resource is part of 'Demonstrations of Geophysical Principles Applicable to the Properties and Processes of the Earth's Interior'
Resource contact / Creator / Publisher:
Author: Jeffrey S. Barker
Geological Sciences and Environmental Studies, Binghamton University