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Chapter Three

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Title: Chapter Three


1
Chapter Three
  • ROCKS

2
Section 3-1 Classifying Rocks
  • When studying a rock sample, geologists observe
    the rocks color and texture and determine its
    mineral composition.
  • Using color and texture, geologists can classify
    a rock according to its origin.
  • Texture is the look that results from the size,
    shape, and pattern of the rocks grains.

3
3-1
  • Coarse-grained the grains are large and easy to
    see.
  • Fined-grained the grains are small and can been
    seen under a microscope or hand-lens.
  • Some rocks grains results from the shape of the
    crystals that form the rock.
  • In other rocks, the grain shapes result from
    fragments of other rock.

4
Texture
5
Texture
6
3-1
  • The three major groups of rock are
  • Igneous forms from the cooling of molten rock.
  • Sedimentary forms when particles of other rocks
    of the remains of plants and animals are pressed
    and cemented together.
  • Metamorphic forms when an existing rock is
    changed by heat, pressure, or chemical reactions.

7
3-2 Igneous Rock
  • Igneous rock is any rock that forms from magma or
    lava. Most igneous rocks are made of mineral
    crystals. Igneous rocks are classified according
    to their origin, texture, and mineral
    composition.

8
Classification of Igneous Rock
9
Extrusive Rock
  • Extrusive rock is igneous rock formed from lava
    that erupted onto Earths surface.
  • Basalt is the most common extrusive rock.

10
Samples of Extrusive Rock
11
3-2
  • Intrusive rock Igneous rock that formed when
    magma hardened beneath the Earths surface.
  • Granite is the most abundant intrusive rock.
  • The texture of an igneous rock depends on the
    size and shape of its mineral crystals.

12
  • Texture may be fine-grained, coarse-grained,
    porphyritic, or glassy.
  • Fined-grained rapid cooling lava forms
    fined-grained.
  • Coarse-grained slow cooling lava forms
    coarse-grained.
  • Porphyritic large crystals scattered on top of
    small crystals. This occurs when magma cools in
    two stages, first slow, and then rapidly as magma
    moves near to the surface.

13
Samples of Intrusive RockGranite
14
Samples of Intrusive RockGabbros
15
Samples of Intrusive RockDiorite
16
3-2
  • Lava low in silica forms dark-colored rocks, such
    as basalt.
  • Magma that is high in silica usually forms light
    colored rocks, such as granite.
  • Many igneous rocks are hard, dense, and durable.
    People use igneous rock for tools and building
    materials.

17
3-3 Sedimentary Rock
  • Sedimentary rocks form from particles deposited
    by water and wind. Sand, mud, and pebbles.
    Sediment is small, solid pieces of material that
    come from rocks or living things.
  • Erosion running water or wind loosen and carry
    fragments of rock.
  • Deposition the process by which sediment settles
    out of the water or wind.
  • Compaction the process that presses sediments
    together.
  • Cementation the process in which dissolved
    minerals crystallize and glue particles of
    sediment together.

18
3-3
  • There are three major groups of sedimentary
    rocks
  • Clastic rock sedimentary rock that forms when
    rock fragments are squeezed together. Sandstone
    is a clastic rock formed from the compaction and
    cementation of sand.
  • Organic Rock forms where the remains of plants
    and animals are deposited in thick layers. Coal
    is formed from the remains of swamp plants and
    limestone is formed from the hard shells of
    living things seashells.
  • Chemical Rock when minerals that are dissolved
    in a solution crystallize. Chemical rocks also
    form from mineral deposits left when seas or
    lakes evaporate.

19
Samples of Sedimentary Rock
  • Sandstone

20
Samples of Sedimentary Rock
  • Gypsum

21
Samples of Sedimentary Rock
  • Shale

22
3-4 Rocks from Reefs
  • Coral animals are tiny relatives of jellyfish
    that live together in vast numbers. They build
    skeletons that grow together to form a structure
    called a coral reef.
  • Coral reefs only form in warm, shallow tropical
    waters.
  • When coral animals die, their skeletons remain,
    and new corals build on top of them.
  • There are three types of coral reefs fringing
    reefs, barrier reefs, and atolls.
  • A coral reef is really organic limestone.

23
Fringing Reef
24
Barrier Reef
25
Atoll Reef
26
Coral Reefs
27
Coral Reefs
28
3-5 Metamorphic Rock
  • Every metamorphic rock is a rock that has changed
    its form. Heat and pressure deep beneath Earths
    surface can change any rock into metamorphic
    rock. Metamorphic rock can form out of igneous,
    sedimentary, or other metamorphic rock.
  • Geologists classify metamorphic rocks by the
    arrangement of the grains that make up the rocks.
  • Metamorphic rocks that have their grains arranged
    in parallel layers or bands are said to be
    foliated slate is the most common.
  • Metamorphic rocks that have grains arranged
    randomly. Marble and Quartz.

29
Metamorphic Rock Samples
30
Metamorphic Rock Samples
  • Marble

31
Metamorphic Rock Sample
  • Quartz

32
3-6 Rock Cycle
  • Forces inside Earth and at the surface produce a
    rock cycle that builds, destroys, and changes the
    rocks in the crust.
  • The rock cycle is a series of processes on and
    beneath Earths surface that slowly change rocks
    from one kind to another.

33
The Rock Cycle
34
Rock Pictures - Lava
  • http//www.hoho.co.uk/html/lanzarote_lava_and_rock
    s.html
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