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Rocks: Materials of the Solid Earth Chapter 2

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Title: Volcanoes and Igneous Activity Earth - Chapter 4 Author: Stan & Cindy Hatfield Last modified by: Tonie Marsett Created Date: 12/18/2000 12:31:17 AM – PowerPoint PPT presentation

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Title: Rocks: Materials of the Solid Earth Chapter 2


1
Rocks Materials of the Solid EarthChapter 2
  • Earth Science, 6e
  • Modified by Dr. Kane

2
What is a Rock?
  • How would you define a rock and a mineral?

3
What types of Rocks are there?
  • Igneous Rocks from magma or lava
  • Origin igneous activity
  • Example granite or basalt
  • Sedimentary rocks from sediments
  • Origin weathering and erosion
  • Example sandstone or clay
  • Metamorphic rocks from stress
  • Origin mountain building
  • Example gneiss or marble

4
The rock cycle (page 45)
5
PART I IGNEOUS ROCKS
  • FEEDBACK
  • From what process igneous rocks from?

6
Origin of Magma (page 228)
  • Magma forms at three major geological settings
  • Divergent (mid ocean ridge)
  • Convergent (subduction zone)
  • Intra plate (hotspot)

7
Origin of Magma (page 148)
8
Mid Ocean Ridge (divergent)
9
Subduction Zone (Convergent)
10
Causes of Magma Formation
  • Decompression Melting (opening a bottle of soda)
  • Factors influencing magma formation
  • 1. Heat Increase
  • 2. Reduction of confining Pressure
  • 3. Increase in volatiles (gases)

11
Types of Igneous rocks
  • Magma cools and crystallizes
  • Inside the crust ? Plutonic or Intrusive rocks
  • Lava cools and crystallizes
  • Outside the crust ? volcanic or extrusive rocks

12
Classification of Igneous rocks
  • When identifying Igneous rocks look for
  • Grain Size (TEXTURE)
  • and
  • Rock color (CHEMICAL COMPOSITION)

13
Rate of Cooling and Crystal Size
  • Texture is size and arrangement of crystals
  • Crystal size is determined by the rate and depth
    of cooling of magma/lava
  • Slow rate forms large crystals
  • Fast rate forms microscopic crystals
  • Very fast rate forms glass

14
Feedback
  • The slower the rate of cooling, the smaller /
    larger the crystals?

15
Types of Textures
  • Phaneritic Coarse grain/slow cooling rate
  • Example Granite or Diorite
  • Aphanitic Fine grain/fast cooling rate
  • Example basalt or rhyolite
  • Glassy glasslike/very fast cooling rate
  • Example Obsidian (volcanic rock)

16
Types of Textures
  • Porphyritic Slow then rapid cooling
  • Example porphyry basalt, porphyry granite
  • Vesicular Full of holes due to gases
  • Example Vesicular basalt, scoria, and pumice
  • Pyroclastic Angular volcanic fragments cemented
    by ash from violent eruptions
  • Example tuff

17
Photomicrograph
18
Photomicrograph
19
Whats the texture?
20
Whats the texture?
21
Whats the texture?
22
Whats the texture?
23
Whats the texture?
24
Chemical Classification of Igneous rocks
  • Bowen's reaction series (page 53)
  • Minerals form in a systematic order
  • through
  • Discontinuous series (Olivine to Quartz) and
  • Continuous series (Feldspars series)
  • Magmatic Differentiation
  • First to form settle at the bottom

25
(No Transcript)
26
Feedback
  • Which mineral crystallizes first?
  • Which mineral crystallizes last?

27
Question
  • Can Olivine and Quartz be found together in the
    same rock?
  • Why?

28
Naming Igneous rocks
  • Granitic or Felsic rocks
  • Light-colored rocks
  • Rich in silica/poor in Fe and Mg
  • Form from melting of continental crust
  • Common rock is Granite (intrusive) or Rhyolite
    (volcanic)

29
Naming Igneous rocks
  • Basaltic or Mafic/ultramafic Rocks
  • Dark Rocks
  • Rich in Fe and Mg/poor in silica
  • Originate mostly from the oceanic crust at
    mid-ocean ridge, and the upper mantle
  • Common rock is Basalt (volcanic) or Gabbro
    (plutonic)

30
Texture? Mafic or Felsic?
31
Texture? Mafic or Felsic?
32
Naming Igneous rocks
  • Intermediate or Andesitic Rocks
  • Mineral and chemical composition are average of
    felsic and mafic rocks
  • Has dark minerals (pyroxene, amphibole, and mica)
    and light minerals (feldspar and quartz)
  • Silica content 50ltSiO2 lt60
  • Common rock is Andesite (volcanic) or Diorite
    (intrusive)
  • Found mostly at Suduction Zone

33
Naming Igneous Rocks
  • Ultramafic Rocks
  • Dark rocks
  • Very poor in silica SiO2 lt45
  • Originates from lower mantle and is found in
    oceanic floor at
  • mid-ocean ridge along mafic rocks
  • Typical rock is peridotite (intrusive) or
    Komatiite (volcanic)

34
Classification of igneous rocks
35
PART II Sedimentary rocks
  • FEEDBACK
  • From what geological process sedimentary rocks
    form?

36
Weathering
  • Two kinds of weathering
  • 1. Mechanical weathering
  • Breaking of rocks into smaller pieces
  • Processes of mechanical weathering
  • Frost wedging (freezing and thawing/exfoliation)
  • Unloading (exposure to surface)
  • Biological activity (burrow animals)

37
Frost wedging (page 55)
38
Joint-controlled weathering in igneous rocks
39
Unloading and exfoliation of igneous rocks
40
Weathering
  • Two kinds of weathering
  • 2. Chemical weathering
  • Alters the internal structures of minerals by
    removing or adding elements
  • Most important agent is water
  • Oxygen dissolved in water oxidizes materials
  • Carbon dioxide (CO2) dissolved in water forms
    carbonic acid and alters the material

41
Factors of weathering
  • Important factors
  • Climate (heat and moisture)
  • Chemical weathering is most effective in areas of
    warm temperatures and abundant moisture

42
Chemical Weathering
  • Weathering of granite minerals
  • Weathering of potassium feldspar produces clay

43
Sedimentary Rocks
  • Lithification
  • Compaction of loose sediment through confining
    pressure of overlying rocks
  • Cementation of loose sediment by
  • Calcite
  • Silica
  • Iron Oxide

44
Classifying sedimentary rocks
  • Two groups based on the source of the material
  • Detrital rocks (Residual solid material)
  • Common rocks include
  • Shale (fine grained)
  • Sandstone (medium grained)
  • Conglomerate (Coarse grained)

45
Classification of sedimentary rocks (page 59)
46
Shale with plant fossils
47
Sandstone
48
Conglomerate
49
Classifying sedimentary Rocks
  • Chemical Sedimentary rocks
  • Derived from material that was once in solution
    and precipitates to form sediment. Two groups

50
A Chemical Organic Rocks
  • From biochemical processes the most common
    sedimentary rocks
  • Example Limestone is the most abundant
    chemical rock .
  • Coal from plants-peat-bituminous
    coal-lignite-anthracite

51
Fossiliferous limestone
52
B - Chemical Inorganic rocks
  • Chemical Sedimentary Rocks
  • From precipitating solutions
  • Evaporites Salt or gypsum rocks,
  • Through increase in concentration
  • Hematite, chert, flint, jasper, or agate

53
Rock salt
54
Features of Sedimentary rocks
  • Features of sedimentary rocks
  • Strata, or beds (most characteristic)
  • Bedding planes separate stratas
  • Fossils
  • Are traces or remains of prehistoric life
  • Are the most important inclusions
  • Help determine past environments
  • Are used to determine age of sedimentary rocks
  • Are used for rock correlation

55
PART III Metamorphic Rocks
  • FEEDBACK
  • What process forms metamorphic rocks?
  • Where would you expect to find metamorphic rocks?
  • Florida or Georgia? Why?

56
Metamorphic rocks
  • Are changed from other rocks, including other
    metamorphic rocks
  • Every metamorphic rock has a parent rock
  • Metamorphism occurs between 200C 800C at
    several kms depth

57
Causes and Types of metamorphism?
  • Heat from magma ? Contact metamorphism
  • Pressure (stress) ? Regional metamorphism
  • Confining pressure from burial
  • Differential stress during mountain building
  • Chemically active fluids
  • Water and other volatiles (Hydrothermal fluids)

58
Types of pressure (stress) in metamorphism
59
Metamorphic Grades
  • Degrees of metamorphism
  • Low-grade (where shale becomes slate)
  • Medium-grade (where granite becomes gneiss)
  • High-grade (rock partially melts ? migmatite)

60
Metamorphic Textures
  • Nonfoliated from contact metamorphism
  • Typical rocks Marble and Quartzite
  • Resembles a coarse-grained igneous rock
  • Is localized around intrusion

61
Marble a Nonfoliated metamorphic rock
62
Development of foliation due to directed
pressure
63
Gneiss typically displays a banded
appearance
64
Classification of metamorphic rocks
65
Resources from rocks and minerals
  • Nonmetallic mineral resources
  • Make use of the materials
  • Nonmetallic elements
  • Physical or chemical properties
  • Two broad groups
  • Building materials (e.g., limestone, gypsum)
  • Industrial minerals (e.g., fluorite, corundum,
    sylvite)

66
End of Chapter 3
67
1 - The Texture of an igneous rock is
  1. Shape of the crystals
  2. Size and arrangement of crystals
  3. How hard of soft the rock feels
  4. All of the above
  5. I have no idea

68
2 Texture of igneous rocks is determined by
  1. Pressure and temperature
  2. Amount of sulfur in the magma
  3. Rate of cooling of magma
  4. Depth of cooling of magma
  5. c and d only

69
3 - The slower the rate of cooling, the
  1. Smaller the crystals of the rock formed
  2. Larger the crystals
  3. No relation whatsoever

70
4 - Which terms characterize a basalt?
  • Felsic/Light colored/silica rich
  • Mafic/dark colored/silica poor
  • Felsic/dark colored/silica rich
  • Mafic/light colored/silica poor

71
5 - Name the volcanic rock (s)
  1. Granite
  2. Basalt
  3. Rhyolite
  4. Gabbro
  5. b and c

72
6 - Is this rocka Plutonic? Or b Volcanic?
73
7 Porphyritic-aphanitic is what type of rock?
  1. Plutonic with two rates of cooling
  2. Volcanic with two rates of cooling
  3. None of these

74
8 Where to find a basaltic magma?
  1. On the continental crust mainly
  2. On the Oceanic crust
  3. At the mid-ocean ridge
  4. At subduction zone
  5. b and c

75
9 Which texture indicates a magma rich in gases?
  1. Phaneritic
  2. Aphanitic
  3. Porphyritic
  4. Pyroclastic
  5. None of these

76
10 Which texture indicates two rates of cooling?
  1. Phaneritic
  2. Aphanitic
  3. Vesicular
  4. Pyroclastic
  5. None of these

77
11 Where to find a felsic magma?
  1. At mid ocean ridge
  2. On the ocean floor
  3. On the continental crust
  4. At subduction zone

78
12 Which term means fine-grained texture?
  1. Aphanitic
  2. Phaneritic
  3. Porphyritic
  4. Vesicular
  5. None of these

79
13 - Texture?a Glassy Or b Pophyritic
80
14 - Which texture means all coarse-grained rock?
  • Aphanitic
  • Porphyritic
  • Phaneritic
  • Glassy
  • Vesicular

81
16 - Quartzite is what type of metamorphic rock?
  1. Regional metamorphism
  2. Contact metamorphism
  3. Not a metamorphic rock

82
17 In what type of metamorphism do pressure
and temperature work together?
  1. Contact metamorphism
  2. Regional metamorphism
  3. All of the above
  4. None of the above

83
18 - What is the parent rock of limestone?
  1. Quartzite
  2. Granite
  3. Marble
  4. Basalt
  5. This does not make sense

84
19 Which one of these is a foliated metamorphic
rock?
  1. Marble
  2. Granite
  3. Mica-schist
  4. Basalt
  5. Shale

85
20 -What type of weathering is frost wedging?
  • a. Chemical weathering
  • b. Mechanical weathering
  • c. Soil sampling
  • d. a and b
  • e. None of the above

86
21- What type of weathering is oxydation?
  • a. Chemical weathering
  • b. Mechanical weathering
  • c. Soil sampling
  • d. a and b
  • e. None of the above

87
22 - Exfoliation results from
  • a. Frost wedging
  • b. Oxidation
  • c. Unloading
  • d. Thermal expansion
  • e. None of the above

88
23 - Which one is the metamorphic rock?
  • Do not take
  • SANDSTONE for
  • GRANITE (granted)!
  • Have a
  • c. GNEISS (nice) day!

89
THE END
  • THATS ALL FOLKS!
  • THANK YOU!!!
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