Title: Rocks: Materials of the Solid Earth Chapter 2
1Rocks Materials of the Solid EarthChapter 2
- Earth Science, 6e
-
- Modified by Dr. Kane
2What is a Rock?
- How would you define a rock and a mineral?
3What 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
4The rock cycle (page 45)
5PART I IGNEOUS ROCKS
- FEEDBACK
- From what process igneous rocks from?
6Origin of Magma (page 228)
- Magma forms at three major geological settings
- Divergent (mid ocean ridge)
- Convergent (subduction zone)
- Intra plate (hotspot)
7Origin of Magma (page 148)
8Mid Ocean Ridge (divergent)
9Subduction Zone (Convergent)
10Causes 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)
11Types 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
12Classification of Igneous rocks
- When identifying Igneous rocks look for
- Grain Size (TEXTURE)
-
- and
- Rock color (CHEMICAL COMPOSITION)
13Rate 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
14Feedback
- The slower the rate of cooling, the smaller /
larger the crystals?
15Types 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)
16Types 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
17Photomicrograph
18Photomicrograph
19 Whats the texture?
20Whats the texture?
21 Whats the texture?
22Whats the texture?
23Whats the texture?
24Chemical 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)
26Feedback
- Which mineral crystallizes first?
- Which mineral crystallizes last?
27Question
- Can Olivine and Quartz be found together in the
same rock? - Why?
28Naming 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)
29Naming 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)
30Texture? Mafic or Felsic?
31 Texture? Mafic or Felsic?
32Naming 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
33Naming 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)
34Classification of igneous rocks
35PART II Sedimentary rocks
- FEEDBACK
- From what geological process sedimentary rocks
form?
36Weathering
- 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)
38Joint-controlled weathering in igneous rocks
39Unloading and exfoliation of igneous rocks
40Weathering
- 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
41Factors of weathering
- Important factors
- Climate (heat and moisture)
- Chemical weathering is most effective in areas of
warm temperatures and abundant moisture
42Chemical Weathering
- Weathering of granite minerals
- Weathering of potassium feldspar produces clay
43Sedimentary Rocks
- Lithification
- Compaction of loose sediment through confining
pressure of overlying rocks - Cementation of loose sediment by
- Calcite
- Silica
- Iron Oxide
44Classifying 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)
45Classification of sedimentary rocks (page 59)
46Shale with plant fossils
47Sandstone
48Conglomerate
49Classifying sedimentary Rocks
- Chemical Sedimentary rocks
- Derived from material that was once in solution
and precipitates to form sediment. Two groups
50A 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
52B - Chemical Inorganic rocks
- Chemical Sedimentary Rocks
- From precipitating solutions
- Evaporites Salt or gypsum rocks,
- Through increase in concentration
- Hematite, chert, flint, jasper, or agate
53Rock salt
54Features 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
55PART III Metamorphic Rocks
- FEEDBACK
- What process forms metamorphic rocks?
- Where would you expect to find metamorphic rocks?
- Florida or Georgia? Why?
56Metamorphic 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
57Causes 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
59Metamorphic Grades
- Degrees of metamorphism
- Low-grade (where shale becomes slate)
- Medium-grade (where granite becomes gneiss)
- High-grade (rock partially melts ? migmatite)
60Metamorphic 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
64Classification of metamorphic rocks
65Resources 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)
66End of Chapter 3
671 - The Texture of an igneous rock is
- Shape of the crystals
- Size and arrangement of crystals
- How hard of soft the rock feels
- All of the above
- I have no idea
682 Texture of igneous rocks is determined by
- Pressure and temperature
- Amount of sulfur in the magma
- Rate of cooling of magma
- Depth of cooling of magma
- c and d only
693 - The slower the rate of cooling, the
- Smaller the crystals of the rock formed
- Larger the crystals
- No relation whatsoever
704 - 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
715 - Name the volcanic rock (s)
- Granite
- Basalt
- Rhyolite
- Gabbro
- b and c
726 - Is this rocka Plutonic? Or b Volcanic?
737 Porphyritic-aphanitic is what type of rock?
- Plutonic with two rates of cooling
- Volcanic with two rates of cooling
- None of these
748 Where to find a basaltic magma?
- On the continental crust mainly
- On the Oceanic crust
- At the mid-ocean ridge
- At subduction zone
- b and c
759 Which texture indicates a magma rich in gases?
- Phaneritic
- Aphanitic
- Porphyritic
- Pyroclastic
- None of these
7610 Which texture indicates two rates of cooling?
- Phaneritic
- Aphanitic
- Vesicular
- Pyroclastic
- None of these
7711 Where to find a felsic magma?
- At mid ocean ridge
- On the ocean floor
- On the continental crust
- At subduction zone
7812 Which term means fine-grained texture?
- Aphanitic
- Phaneritic
- Porphyritic
- Vesicular
- None of these
7913 - Texture?a Glassy Or b Pophyritic
8014 - Which texture means all coarse-grained rock?
- Aphanitic
- Porphyritic
- Phaneritic
- Glassy
- Vesicular
8116 - Quartzite is what type of metamorphic rock?
- Regional metamorphism
- Contact metamorphism
- Not a metamorphic rock
8217 In what type of metamorphism do pressure
and temperature work together?
- Contact metamorphism
- Regional metamorphism
- All of the above
- None of the above
8318 - What is the parent rock of limestone?
- Quartzite
- Granite
- Marble
- Basalt
- This does not make sense
8419 Which one of these is a foliated metamorphic
rock?
- Marble
- Granite
- Mica-schist
- Basalt
- Shale
8520 -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
8621- What type of weathering is oxydation?
- a. Chemical weathering
- b. Mechanical weathering
- c. Soil sampling
- d. a and b
- e. None of the above
8722 - Exfoliation results from
- a. Frost wedging
- b. Oxidation
- c. Unloading
- d. Thermal expansion
- e. None of the above
8823 - Which one is the metamorphic rock?
- Do not take
- SANDSTONE for
- GRANITE (granted)!
- Have a
- c. GNEISS (nice) day!
89THE END
- THATS ALL FOLKS!
- THANK YOU!!!