Nhyeisha& Verenice
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Transcript of Nhyeisha& Verenice
Earthquakes
Nhyeisha &Verenice Core.1
Mrs. Collazoscience
• A strike –slip fault is a type of fault were rocks on either side move past each other sideways
Strike –Slip Fault
Shearing
• Stress that pushes a mass of rock in opposite directions
Compression
• Compression squeezes rock and make it fold that causes syncline which is a downward fold in rock caused by compression
What’s Stress
• Stress is a force that happens when rock changes its shape or volume
Plateau’s
A plateau is a large area of flat land
TensionStress that stretches rock so it became
thinner.
Hanging wall
• Hanging wall is something that helps the upper part of a fault.
Reverse fault
• A reversed fault is when the rock of the crust is pushed together
Normal fault
• A normal fault is when the hanging wall slides downward which is caused by tension
Foot wall
• The block of rock that forms the lower half of a fault
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