Nhyeisha& Verenice

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Earthquakes Nhyeisha &Verenice Core.1 Mrs. Collazo science

Transcript of Nhyeisha& Verenice

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Earthquakes

Nhyeisha &Verenice Core.1

Mrs. Collazoscience

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• A strike –slip fault is a type of fault were rocks on either side move past each other sideways

Strike –Slip Fault

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Shearing

• Stress that pushes a mass of rock in opposite directions

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Compression

• Compression squeezes rock and make it fold that causes syncline which is a downward fold in rock caused by compression

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What’s Stress

• Stress is a force that happens when rock changes its shape or volume

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Plateau’s

A plateau is a large area of flat land

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TensionStress that stretches rock so it became

thinner.

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Hanging wall

• Hanging wall is something that helps the upper part of a fault.

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Reverse fault

• A reversed fault is when the rock of the crust is pushed together

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Normal fault

• A normal fault is when the hanging wall slides downward which is caused by tension

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Foot wall

• The block of rock that forms the lower half of a fault

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Web sites

• www.uh.edu/~jbutler/physical/earthquakes1.gif• www.wcsgabon.org/Bateke/PlateauBateke.JPG• facweb.bhc.edu/.../Geol101/study/structur.htm• www.indiana.edu/~g103/G103/week9/wk9.html• www.bdrg.esci.keele.ac.uk/.../norm_stress_ex.GIF• www.cert-la.com/images/07-04_Earthquakes.jpg• www.devils-punchbowl.com/pages/geologyfaults.html

• facweb.bhc.edu/.../Geol101/study/structur.htm• www.aero.polimi.it/.../CompressionBlock.jpg• www.seismo.unr.edu/ep/nvguide/images/sbg1b.gif• www.boiseschools.org/schools/north/hunicke/VO