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Chapter 3 Prentice-Hall Earth Science 2006

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Presentation on theme: "Chapter 3 Prentice-Hall Earth Science 2006"— Presentation transcript:

1 Chapter 3 Prentice-Hall Earth Science 2006
Rocks Chapter 3 Prentice-Hall Earth Science 2006

2 Rock Cycle Rocks broken down into sediments Magma or lava cools
Sediments compacted & cemented Magma forms when rocks melt Rocks changed by heat or pressure

3 Igneous Rocks Formation Classification – Texture
Intrusive: magma cools and hardens Extrusive: lava cools and hardens Examples Granite and rhyolite Classification – Texture Coarse-grained – large crystals Fine-grained – small crystals Glassy – cools rapidly, no crystals Porphyritic – different sizes of crystals

4 Igneous Rocks Classification – Composition
Granitic – light colored silicate minerals Quartz, feldspar Basaltic – dark colored Basalt, gabbro

5 Sedimentary Rocks Formation
Weathering – removal of rock by physical or chemical forces Wind, water, ice, or gravity (rock falls) Compaction – squeezing of sediments that forces most water out of the rock Cementation – dissolved minerals are deposited in the tiny spaces in a rock. Acts like a glue.

6 Sedimentary Rocks Classification
Clastic – rocks made of weathered bits of rocks and minerals Examples: shale, breccia Chemical – Dissolved minerals precipitate from water solutions Limestone, chert, flint

7 Metamorphic Rocks Formation Agents Contact – hot magma moves into rock
Marble Regional – Large-scale deformation resulted from extreme pressure and temperature Agents Heat – provides the energy needed for chemical reactions Magma “bakes” rocks and recrystallize minerals

8 Metamorphic Rocks Classification
Stress (Pressure) – causes the spaces between minerals to close. Increases density Reactions in Solution – Hot solutions causes recrystallization by dissolving original minerals and depositing new ones. Classification Foliated – Pressure from contact metemorphism causes crystals to recrystallize at right angles to the direction of the force. Example: Gneiss

9 Metamorphic Rocks Nonfoliated – Does not have a banded appearance
Composed of one mineral Example: marble

10 Igneous Granite – Intrusive Rhyolite – Extrusive
Pumice – Extrusive (cools quickly) Andesite Obsidian Basalt Gabbro Table 1 on page 74

11 Sedimentary Shale – Clastic Breccia – Clastic
Conglomerate – Cementation Sandstone – Compaction/Cementation Coquina – Chemical/Biochemical Chert Coal Table 2 on page 79

12 Metamorphic Gneiss – Pressure or stress Marble – nonfoliated Quartzite
Anthracite Schist Slate Table 3 on page 84


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