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Metamorphic Rocks CH 3 Prentice Hall p. 82-86 CH 3 Prentice Hall p. 82-86.

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Metamorph ic Rocks CH 3 Prentice Hall p. 82-86
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Page 1: Metamorphic Rocks CH 3 Prentice Hall p. 82-86 CH 3 Prentice Hall p. 82-86.

MetamorphicRocks

MetamorphicRocksCH 3 Prentice Hall

p. 82-86CH 3 Prentice Hall

p. 82-86

Page 2: Metamorphic Rocks CH 3 Prentice Hall p. 82-86 CH 3 Prentice Hall p. 82-86.

Formation of Metamorphic Rocks

• Heat and Pressure deep beneath Earth’s surface can change any rock (ig, sed or met) into metamorphic rock.

• Forces inside Earth push rock down towards the heat of the Mantle.

Page 3: Metamorphic Rocks CH 3 Prentice Hall p. 82-86 CH 3 Prentice Hall p. 82-86.

Formation of Metamorphic Rocks

• Pockets of magma can also provide heat.

• Pressure is due to the weight of the overlying rock. (Deeper=greater pressure)

Page 4: Metamorphic Rocks CH 3 Prentice Hall p. 82-86 CH 3 Prentice Hall p. 82-86.
Page 5: Metamorphic Rocks CH 3 Prentice Hall p. 82-86 CH 3 Prentice Hall p. 82-86.

Foliated

Parent Rock Metamorphic Rock

Granite Gneiss

Shale Slate

Non-Foliated

Parent Rock Metamorphic Rock

Limestone Marble

Sandstone Quartzite

Classifying (Parent Rocks)

Page 6: Metamorphic Rocks CH 3 Prentice Hall p. 82-86 CH 3 Prentice Hall p. 82-86.

Classifying Metamorphic Rocks

Page 7: Metamorphic Rocks CH 3 Prentice Hall p. 82-86 CH 3 Prentice Hall p. 82-86.

Uses of Metamorphic Rocks


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