'Strike slip fault' presentation slideshows

FAULTING

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Physical Geology Review

Physical Geology Review. the expanse of material is vast!. Internal Structure of the Earth granitic/basaltic. crust = 0-40 km; mantle = 40-2900 km; outer core (liquid) = 2900-5200 km; inner core = 5200-6400 km. from: www.usgs.gov. Guidelines for Structural Analysis. reference frame

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Earthquakes

Earthquakes. What Is An Earthquake? Click here to find out. What is an earthquake?. Used to describe both sudden slip on a fault, and the resulting ground shaking and radiated seismic energy caused by the slip Caused by volcanic or plate activity,. http://eqseis.geosc.psu.edu.

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Interactive map

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Page created by W. G. Huang

Credit Digital Globe. Page created by W. G. Huang. Earthquake Parameters. 2010-01-12 at 21:53:10.4 UTC 18.47 N ; 72.55 W Mw=7.1; Depth=10 km. Taiwan. Page created by W. G. Huang. Earthquake Parameters. 2010-01-12 at 21:53:10.4 UTC 18.47 N ; 72.55 W Mw=7.1; Depth=10 km.

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Structural Geology Stress and Strain

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Chapter 4 Lesson 2

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EARTHQUAKE MAGNITUDE, INTENSITY, ENERGY, POWER LAW RELATIONS AND SOURCE MECHANISM

EARTHQUAKE MAGNITUDE, INTENSITY, ENERGY, POWER LAW RELATIONS AND SOURCE MECHANISM. Walter D. Mooney U.S. Geological Survey California, USA e-mail: mooney @ usgs.gov. EARTHQUAKE CLASSIFICATION MAGNITUDE CLASSIFICATION M ? 8.0 Great Earthquake

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Earthquakes

Earthquakes. Science. Earthquakes.

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Plate Tectonic Notes

Plate Tectonic Notes. Stress is the amount of force per unit area put on a given object. Deformation is the rock changing due to stress. * Three things determine how much stress a rock can handle: composition, temperature and amount of pressure. Types of Stress:.

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Chapter 4 Clicker Review

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Chapter 4 Clicker Review

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Rock Deformation

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THE DYNAMIC EARTH

THE DYNAMIC EARTH. http://www.youtube.com/watch?v=-z8zdoFLZME. http://www.youtube.com/watch?v=rn3oAvmZY8k. EARTHQUAKES. Earthquake. Release of energy when pressure and/or stress is built up between rocks Usually occurs along faults and plate boundaries

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Earthquakes: Faults and Waves

Earthquakes: Faults and Waves. Sarah Bennek Grade 9. Objectives. To be able to describe what happens to the earth at normal, reverse and strike slip faults. To be able to compare and contrast P-waves, S-waves, R-waves, and L-waves. Location of Earthquakes. Earthquakes happen along faults

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Geologic Maps

Geologic Maps. What the Colors Mean. Each color refers to the time period that the rock unit formed. What the Letters Mean. Each of the letters refers to some thing specific The first letter refers to when the rock unit formed The next one to two letters refer to the name of the rock unit

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Forces Inside Earth (43)

Forces Inside Earth (43). Once the elastic limit is passed, the rocks may break When rocks break, they move along surfaces called faults To relieve this stress, the rocks tend to bend, compress, or stretch. If the force is great enough, the rocks will break.

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