Metamorphic rocks

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Transcript of Metamorphic rocks

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I. Parent Rocks

Rocks that have been changed from an original “parent”

rock

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II. How are Metamorphic Rocks Formed?

Formed under tremendous heat, great pressure, and chemical reactions

Can make new minerals Most are found on or near plate

boundariesMetamorphism is changing one type of

rock into another as a result of heat(from mantle), Pressure (from layers above) and/or chemical reactions.

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III. Where does the Heat Come From?

The heat comes from: 1. Mantle2. Pressure of the

layers3. Movement of

the Plates on Earth

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Earth’s Plates

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IV. What does Metamorphism change?

Metamorphic rocks can change:

1. a rocks appearance, texture

2. crystal structure3. mineral content It can form from a/an: 1. Igneous2. Sedimentary3. Another

metamorphic rock!

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a. Foliated – mineral crystals are arranged in parallel layers or bands

Examples: Schist, slate, and gneiss

b. Nonfoliated – rocks are not banded and do not break into layers Examples: Marble and quartizite

V. Types of Metamorphic Rocks

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Foliated

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Non-foliated

NON-Foliated

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VI. Contact vs. Regional Metamorphism

Contact

Small AreaRegional

Large Area

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Examples

Used in construction of buildings

and walkways

Used in tables, floors, and

roofing

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Tier 1 MetamorphicPicture

1 picture of foliated

1 picture of non-foliated

Must have correct rock

names Must be

presented in an organized/colorfu

l way

ChartComplete chart Must do research DOES NOT have

to be colorful