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Metamorphic Rocks. Metamorphic Rocks: form when heat and/or pressure change pre-existing rocks. – Metamorphism: the process of forming metamorphic rocks.

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Presentation on theme: "Metamorphic Rocks. Metamorphic Rocks: form when heat and/or pressure change pre-existing rocks. – Metamorphism: the process of forming metamorphic rocks."— Presentation transcript:

1 Metamorphic Rocks

2 Metamorphic Rocks: form when heat and/or pressure change pre-existing rocks. – Metamorphism: the process of forming metamorphic rocks.

3 Formation of Metamorphic Rocks Recrystallization: the process of increasing the size of the mineral crystals/clasts AND/OR changing the mineral composition WITHOUT MELTING. – HIGH heat and pressure allows atoms to rearrange Animation

4 Types of Metamorphism 1.Contact Metamorphism: caused by contact with extreme HEAT (magma/lava OR hot fluids) that will alter the rock. – No foliation

5 When extreme heat is added to a Quartz sandstone, you get Quartzite. When extreme heat is added to Limestone, you get Marble.

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7 Diorite (igneous) Marble (metamorphic) Limestone (sedimentary) Marble (metamorphic) Limestone (sedimentary) A thick body of diorite was injected between layers of limestone of the Helena Formation in northern Montana. The great heat of the intrusion baked the limestone above and below it into white marble.

8 Types of Metamorphism 2.Regional Metamorphism: occurs over wide regions when rocks are exposed to extreme heat AND pressure. – Foliated rocks – Folded rocks – Faulted rocks

9 Warped, distorted layers

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11 Folded Rock outcrop on I-68, Maryland

12 Textures of Metamorphic Rocks 1.Foliated rocks: have layers of mineral crystals – occurs when pressure aligns minerals into layers.

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15 In SLATY FOLIATION, rocks may split into flat, thin layers

16 In SCHISTOSE foliation, minerals have been squished into flakes of mica

17 In GNEISSIC foliation, minerals have been squished into bands of color (“zebra stripes”)

18 Textures of Metamorphic Rocks 2. Nonfoliated Rocks: not layered – rocks were not subjected to a directional pressure and/or – minerals are not flat Quartzite Marble

19 1.Foliation 2.Bent/Distorted Layers Key Identifying Features of Metamorphic Rocks

20 3. Key Identifier Minerals: – Garnet - Dark Red Color – Mica – Shiny, flaky mineral Key Identifying Features of Metamorphic Rocks

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22 Original RockAdd HEAT & PRESSURE Metamorphic Rock ShaleSlate Phyllite Schist Gneiss Quartz Sandstone Quartzite LimestoneMarble

23 Which metamorphic rock is nonfoliated, and composed of calcite?

24 Which metamorphic rock is foliated, and consists of ONLY mica?

25 Vocabulary Recrystallization: changing the size of mineral crystals or mineral composition without melting. Foliation: Mineral layering or banding

26 Slaty Foliation: Fine-grained and breaks into thin, smooth layers. Schistose Foliation: Medium-grained with high mica content. Gneissic Texture: Coarse-grained with banded minerals. Vocabulary


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