Metamorphic Rock Lecture

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Meta = change Morph = shape

Metamorphic Rock are rocks in which the structure, texture, or composition of the rock have changed.

The change is caused by heat, pressure, or a combination of both.

Deformation = a change in the shape of a rock caused by a force placed on it. The rock is squeezed and stretched causing it to fold and bend.

Two ways rock can undergo metamorphism:

Contact Metamorphism

Regional Metamorphism

Contact Metamorphism

Heated by nearby magma

More intense the closer the rock is to the magma

Near igneous intrusions

Some minerals can change into other minerals because of the heat

Regional Metamorphism

Caused by pressure built up deep in the ground

Caused when large pieces of the Earth’s crust collide with each other

Causes rock to become deformed and chemically changed

These types of metamorphic rocks are found far below most continental rock formations

Composition of Metamorphic Rock

Mineral composition of rocks can change as the rocks undergo metamorphism

The heat and pressure cause minerals to change into other minerals

INDEX MINERALS = Minerals that are used by geologists to estimate the temperature, depth within the Earth, and pressure at which a rock undergoes metamorphism

Textures of Metamorphic Rock

Two types: Foliated and Nonfoliated

Foliated Metamorphic Rock

Foliated = the texture of metamorphic rock in which the mineral grains are arranged in planes or bands

The effects of metamorphism depend on the amount of heat and pressure applied

More heat and pressure = cause minerals to separate into distinct bands

Sedimentary Shale

Slate

Phyllite

Schist

Gneiss

Nonfoliated Metamorphic Rock

Nonfoliated = The texture of metamorphic rock in which the minerals are not arranged in planes or bands

Usually made up on one or only a few minerals

Recrystalization = when minerals change in composition or crystals change in size due to the intense heat and pressure

Quartz sandstone . . . Quartzite

Limestone . . . . . . . . . . . Marble

Review:

Meta = change Morph = shape

Metamorphic Rock = rocks in which the structure , texture , or composition of the rock have changed.

The change is caused by heat, pressure, or a combination of both.

Deformation = a change of shape, the rock is squeezed . . . stretched . . . folded . . . bent

Two ways rock can undergo metamorphism:

Contact Metamorphism (heat)

Regional Metamorphism (pressure)

Composition of Metamorphic Rock

Mineral composition of rocks can change

Causes = heat and pressure

INDEX MINERALS = Minerals used to estimate the temperature, depth, and pressure

Textures of Metamorphic Rock

Foliated = mineral grains are arranged in planes or bands o More heat and pressure = cause minerals to separate into distinct bands

Nonfoliated = minerals are not arranged in planes or bands o One or only a few minerals o Recrystalization = minerals change in composition or crystals change in size

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