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Page 1: Ch. 11 Notes

Ch. 11 NotesDeformation of the Crust

Page 2: Ch. 11 Notes

How Rock Deforms

Earth’s surface changes constantly Isostasy

When lithosphere and asthenosphere are balanced

If weight of lithosphere changes, it sinks or rises until there is a balance again

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How Rock Deforms

Stress Force exerted on a rock

as lithosphere moves Types of stress:

Compression – squeezes and shortens

Tension – stretches and pulls

Shear stress – parts pushed in opposite directions

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How Rock Deforms

Strain When rock changes its shape or volume

because of stress Stress doesn’t always change a rock, it can

“bounce back”

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How Rock Deforms

Folds Bend in rock layers

that results from stress

Result of compression or shear stress

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How Rock Deforms

Faults Break in rock where surrounding rock moves Earthquakes occur along fault lines

Page 7: Ch. 11 Notes

Mountain Ranges

Mountain ranges believed to be formed by once active tectonic plates Results of collisions between:

Continental and oceanic crust Oceanic crust and oceanic crust Continental crust and continental crust


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