igneous rocks

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Igneous Rocks

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Igneous Rocks. Rock vs. Mineral. Rock - a naturally formed consolidated material composed of grains of one or more minerals. Mineral - a naturally occurring element or compound with a relatively constant chemical and structural composition. Three Rock Types. - PowerPoint PPT Presentation

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Page 1: Igneous Rocks

Igneous Rocks

Page 2: Igneous Rocks

Rock vs. Mineral• Rock- a naturally formed

consolidated material composed of grains of one or more minerals.

• Mineral- a naturally occurring element or compound with a relatively constant chemical and structural composition.

Page 3: Igneous Rocks

Three Rock Types1. Igneous: Rock formed from the cooling of

magma

2. Sedimentary: Rock formed from the accumulation and lithification (cementing) of weathered material.

3. Metamorphic: Rocks formed by the altering existing rock by heat and/or pressure.

Page 4: Igneous Rocks

The Rock Cycle

Page 5: Igneous Rocks

How do igneous rocks form?

IntrusiveExtrusive

Page 6: Igneous Rocks

Identification of Igneous Rocks

Texture: the size of the grains that make up the rock

Mineralogy: the minerals present in the rock

Page 7: Igneous Rocks

Textures:

Phaneritic (Fan-er-itic): all large grains Aphanitic (A-fan-itic): all small grains

Porphyritic (Poor-for-itic): large crystals surrounded by fine-grained matrix

Page 8: Igneous Rocks

Terms to explain to chemistry of igneous rocks:• Mafic: (May-fik) Silica deficient

igneous rocks with a high content of Magnesium, Iron, and Calcium. More dark minerals than light minerals.

• Felsic: (fell-sick) Silica rich igneous rock with a high percentage of potassium and sodium. Usually lots of quartz and feldspar.

Page 9: Igneous Rocks

Mineral content of Igneous Rocks

Page 10: Igneous Rocks

Intrusive Structures: Rock formations caused by the cooling of magma beneath the Earth’s Surface.

Page 11: Igneous Rocks

Shiprock, New Mexico

Formed when a volcano goes extinct (loses its heat source). The magma that was inside the volcano cools and hardens into a rock much harder than that on the surface.Eventually the volcano is weathered away, exposing the rock.

Page 12: Igneous Rocks

Devil’s Tower, WY

Page 13: Igneous Rocks

Dikes: Magma from below is pushed up into cracks in the existing rock.

Page 14: Igneous Rocks

Dikes from Intrusion

Page 15: Igneous Rocks

Magma Formation• molten rock created near the subduction zone.

• granitic magma ~ 650o C

• geothermal gradient – 3o C/100 m

• melting point increases with pressure; pressure increases with depth.

• mineral melting point is lowered by water under pressure.

Page 16: Igneous Rocks

Bowen’s Reaction Series• sequence in which minerals crystallize in

cooling magma.

Page 17: Igneous Rocks

Volcanism and Extrusive Rocks• pyroclastic (pyro = “fire”; clast = “broken”)• pyroclastic flow- mixture of gas and pyroclastic

debris.

• caldera-• pumice-• vesicles-• cinder cone-

Page 18: Igneous Rocks

Extrusive Rockspyroclastic flow(click the picture below for a short video pumice with vesicles

Page 19: Igneous Rocks

Pyroclastic Flows

Page 20: Igneous Rocks

volcanos

cinder cone caldera