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METAMORPHIC ROCK
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METAMORPHIC ROCK. Metamorphic – Formed from older “parent rock” (either igneous or sedimentary) under intense heat and/or pressure far beneath the earth’s.

Dec 24, 2015

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Derick Leonard
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Page 1: METAMORPHIC ROCK. Metamorphic – Formed from older “parent rock” (either igneous or sedimentary) under intense heat and/or pressure far beneath the earth’s.

METAMORPHIC ROCK

Page 2: METAMORPHIC ROCK. Metamorphic – Formed from older “parent rock” (either igneous or sedimentary) under intense heat and/or pressure far beneath the earth’s.

• Metamorphic – Formed from older “parent rock” (either igneous or sedimentary) under intense heat and/or pressure far beneath the earth’s surface.

Page 3: METAMORPHIC ROCK. Metamorphic – Formed from older “parent rock” (either igneous or sedimentary) under intense heat and/or pressure far beneath the earth’s.

Formation of Metamorphic RockMeaning to change shape

Changes with temperature and pressure, but remains solid

Usually takes place deep in the Earth

Page 4: METAMORPHIC ROCK. Metamorphic – Formed from older “parent rock” (either igneous or sedimentary) under intense heat and/or pressure far beneath the earth’s.

Types of MetamorphismContact Metamorphism: occurs when rocks are heated by nearby magma

Regional Metamorphism: occurs deep in the Earth where pressures build up and are able to create a chemical change in rocks

Page 5: METAMORPHIC ROCK. Metamorphic – Formed from older “parent rock” (either igneous or sedimentary) under intense heat and/or pressure far beneath the earth’s.

Composition of Metamorphic Rocks

• Minerals that were present in the rock when it formed may not be stable in the new temperature and pressure conditions.

• Original minerals change into minerals that are more stable in the new conditions.

Page 6: METAMORPHIC ROCK. Metamorphic – Formed from older “parent rock” (either igneous or sedimentary) under intense heat and/or pressure far beneath the earth’s.

Index Minerals

• Many of these minerals ONLY form in metamorphic rocks. Some of these form only at certain temperatures and pressures.

• These minerals are known as Index Minerals, and are used to estimate the temperature, depth, and pressure at which a rock undergoes metamorphism.

• Ex of Index Minerals – biotite mica, chlorite, garnet, kyanite, muscovite mica, sillimanite, and staurolite.

Page 7: METAMORPHIC ROCK. Metamorphic – Formed from older “parent rock” (either igneous or sedimentary) under intense heat and/or pressure far beneath the earth’s.

Textures of Metamorphic Rocks

Foliated- mineral grains are arranged in planes or bands. - Results when rocks are subjected to both high temperatures and high pressures. - Typically associated with regional metamorphism

gneiss

Page 8: METAMORPHIC ROCK. Metamorphic – Formed from older “parent rock” (either igneous or sedimentary) under intense heat and/or pressure far beneath the earth’s.

As shale is exposed to more and more heat and pressure, it continually changes into different types of metamorphic rock

Page 9: METAMORPHIC ROCK. Metamorphic – Formed from older “parent rock” (either igneous or sedimentary) under intense heat and/or pressure far beneath the earth’s.

Textures of Metamorphic Rocks

Nonfoliated- mineral grains are not arranged in planes or bands-May result when rocks are subjected to high temperatures and low pressures- Typically associated with small scale, contact metamorphism

Marble

Page 10: METAMORPHIC ROCK. Metamorphic – Formed from older “parent rock” (either igneous or sedimentary) under intense heat and/or pressure far beneath the earth’s.

Examples

• Sandstone Quartzite

• Shale Slate

Page 11: METAMORPHIC ROCK. Metamorphic – Formed from older “parent rock” (either igneous or sedimentary) under intense heat and/or pressure far beneath the earth’s.

Examples

Limestone Marble

Granite Gneiss

Page 12: METAMORPHIC ROCK. Metamorphic – Formed from older “parent rock” (either igneous or sedimentary) under intense heat and/or pressure far beneath the earth’s.

Metamorphic Rock QUESTIONS

Determine if the following rock samples are foliated or non-foliated:

Amphibolite Quartzite Phyllite

Foliated