Igneous Rock

Sedimentary Rock

Metamorphic Rock

Igneous pattern Metamorphic pattern Sedimentary pattern

-Forms when hot, liquid, rock crystallizes (cools and solidifies).

Magma forms 3 ways:1. Rock is heated2. Pressure released3. Change composition

Basalt lava (glowing rock) oozes over basalt lava flow Holt

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a. Intrusive Igneous Rock-Forms inside Earth-slow cooling

b. Extrusive Igneous Rock-Forms on surface (exterior) of Earth-Fast cooling

Felsic Rock-Light colored -made of aluminum, potassium, silicon, and sodium.

Mafic Rock-Dark colored-Made of calcium, iron, and magnesium.

Course-grained Fine-grained

Course-grained Fine-grained

a. Composition of Igneous Rock

-Slow cooling forms large crystals. (Coarse-grained Texture)

-Fast cooling forms small crystals. (Fine-grained Texture)

-Rate of cooling influences crystal size.

Fast cooling = small crystals

Slow cooling = large crystals

Show Holt Visual: Igneous Rock Texture

1. What size crystal forms from extrusive rock?

2. What is one way magma forms?3. Generally speaking what color are felsic

rocks?4. Quality of rock based on the size, shape, and arrangement of grains is referred to as…5. What are the 2 characteristics that

geologist study to identify rock:?

Rock ID practiceUse the rock key to identify the various rocks on your table:

Igneous Rocks Classified according to composition & texture

Glassy- shiny and look like glass, not organized into crystals.

Ex: obsidian

Fine-grained-made of interlocking crystals. Ex: basalt

BASALT

More Igneous Rocks…

Course Grained Texture- Granite

More Igneous Rocks…Porous- no crystals, cools rapidly, looks

like a sponge. Ex: pumice

Diffferent size crystals locked together

More Igneous Rocks…

More Igneous Rocks…

Strata layers of rock.

Stratification The process in which sedimentary rocks are arranged in layers. H

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Cycle

1. Clastic forms when rock or mineral fragments are cemented together.

2. Chemical forms when minerals crystallize out of solution, such as sea water, to become rock.

3. Organic forms from the remains of once-living plants and animals.

Ex: Limestone Coal

Chalk

-Rocks that have undergone a change in texture, structure, or composition.

-Changes in heat and pressure cause rocks to change from one form to another.

Contact Metamorphism◦ Rock undergoes

metamorphism when it comes in contact with magma or is heated by nearby magma.

Regional Metamorphism

-Pressure builds up in rock that is buried deep below rock formations or when large pieces of rock collide.

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

Nonfoliated-The texture of metamorphic rock in which the mineral grains are not arranged in planes or bands.