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Rocks

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Title: Slide 1 Author: Paul Montreuil Last modified by: EMSISD Created Date: 11/1/2005 3:24:19 AM Document presentation format: On-screen Show (4:3) – PowerPoint PPT presentation

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Title: Rocks


1
Rocks
2
Rocks
  • Rocks are classified by how they formed and what
    theyre made of
  • There are 3 general classes of rocks
  • Igneous
  • Sedimentary
  • Metamorphic

3
Igneous Rocks
Are formed when lava and magma cool to form solid
rock
4
Igneous Rocks
  • Extrusive are formed once magma reaches the
    surface and cools
  • Ex basalt, pumice
  • Intrusive are formed from magma that cools and
    solidifies within the crust, which may later be
    uncovered by the process of erosion
  • Ex granite gabbro

5
Sedimentary Rock
Are formed when sediments (sand clay, and silt)
are compressed and become solid rock
6
Sedimentary Rock
  • Formed by wind, water, snow or organisms breaking
    down other rocks into sediments
  • Most sediments are deposited on the bottom of
    lakes, rivers and seas, and then compressed to
    form rock.
  • Cover about 75 of Earths surface
  • Many sedimentary rocks have been moved by water,
    wind, waves, currents, ice or gravity.

7
sandstone
shale
limestone
Common examples
Halite (rock salt)
chalk
coal
8
Metamorphic Rocks
Metamorphic rocks form when existing rocks are
heated or squeezed they recrystallize and might
change chemically.
9
Metamorphic Rocks
  • All kinds of rocks can be changed
  • Can change the crystal structure, texture, or can
    form new minerals

marble
limestone
gneiss
granite
10
Rock Cycle
In the rock cycle, rocks change from one type to
another over millions of years. A rock in any
part of the cycle could become any other kind of
rock.
11
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12
cementation
Weathering and Erosion
Rock Cycle
Heat and Pressure
Cooling and Hardening
Melting
13
Minerals
14
Minerals
A mineral is an inorganic solid material with a
particular chemical makeup and orderly
arrangement of atoms.
15
Minerals
  • Rocks are usually composed of two or more
    minerals.
  • Minerals form from hardening of magma or lava
  • Mineral formation clues include size and how
    mineral crystals fit together.
  • Solid materials with a repeating pattern of
    atoms are called crystals.

16
Properties/Characteristics to Identify Minerals
  • Cleavage- splitting into thin sheets
  • Fracture- breaking into rough edges
  • Color- many different colors, not mineral
    specific
  • Shape (habit)- special arrangement of atoms, if
    grown unimpeded
  • Luster- describes how light reflects from a
    minerals surface.

17
Properties/Characteristics to Identify Minerals
  • Streak- is the color powder produced when a
    mineral is scratched on an unglazed white tile.
  • Hardness- Mohs scale is used to classify
    minerals from 1 (softest, talc) to 10 (hardest,
    diamond). It is also a test of which minerals
    scratch or are scratched by others.

18
Properties/Characteristics to Identify Minerals
  • Other properties of minerals include magnetism,
    double refraction, taste, or reactions with acid.

19
Common Minerals
Rare minerals which can be cut and polished are
gems. This makes them ideal for jewelry.
20
Common Minerals
An ore contains enough useful mineral to be sold
at a profit. Copper is an example of an ore.
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