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Earthquake Machine Lite Michael Hubenthal - IRIS; Larry Braile - Purdue University; John Lahr - USGS; John Taber - IRIS Mechanical Modeling to Increase.

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Presentation on theme: "Earthquake Machine Lite Michael Hubenthal - IRIS; Larry Braile - Purdue University; John Lahr - USGS; John Taber - IRIS Mechanical Modeling to Increase."— Presentation transcript:

1 Earthquake Machine Lite Michael Hubenthal - IRIS; Larry Braile - Purdue University; John Lahr - USGS; John Taber - IRIS Mechanical Modeling to Increase Student Understanding of Complex Earth Systems

2 Guiding Question(s) What is an earthquake? What is the role of a model in science? How are scientific ideas constantly changing?

3 Have you even been outside at night and felt nervous or frightened? Calvin and Hobbes by Bill Watterson

4 Will the flashlight help us feel better here?

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6 Answer the following question on your sticky note… What is an Earthquake? ? ? ? ? ? ? ? ? ? ? ? ? ? ? ?

7 Calvin and Hobbes by Bill Watterson

8 B C EQ Machine - Lite Top View C Rubber Band Thin Tape Measure Wood Block w/ Sandpaper Tape Measure Sandpaper Wood Block Guide

9 B C EQ Machine - Lite Top View Bulk of the Plate Edge of the Plate Elastic Properties of Earth Materials Plate has Constant Velocity Here of 1cm/year

10 Seismic Moment M o = fault length x fault width x displacement x rigidity Moment Magnitude = M w = log M o /1.5 – 10.7

11 Seismic Moment M o = fault length x fault width x displacement x rigidity Visualizing magnitude with the model B Moment Magnitude = M w = log M o /1.5 – 10.7

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13 Distant forces cause a gradual build up of stress in the earth over tens or hundreds or thousands of years, slowly distorting the earth underneath our feet. Eventually, a pre- existing weakness in the earth--called a fault or a fault zone- -can not resist the strain any longer and fails catastrophically. Elastic Rebound Theory

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