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Rocks

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Rocks Rocks, Part 3 Sedimentary Rocks Sedimentary From Latin sedimentum = settling Formed when sediments are compacted and cemented together Create a Sedimentary Rock ... – PowerPoint PPT presentation

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Title: Rocks


1
Rocks
2
Whats a Rock?
  • A solid chunk of one or more minerals (or
    sometimes mineral-like matter)

3
The Rock Cycle
4
A Quick Quiz
  • The type of rock that starts it all!
  • IGNEOUS!
  • A rock formed by squeezing and heating.
  • METAMORPHIC
  • A rock formed from smaller rocks and material
    being compacted together.
  • SEDIMENTARY

5
More Questions!
  • A rock formed from cooling magma or lava
  • IGNEOUS
  • A sedimentary rock might have originally been one
    of this(these) kind of rock(s)
  • IGNEOUS, METAMORPHIC, or SEDIMENTARY
  • A metamorphic rock might have originally been one
    of this(these) kind of rock(s)
  • IGNEOUS or SEDIMENTARY

6
Rocks, Part 2
  • Igneous Rocks

7
Igneous
  • From Latin ignis FIRE!
  • Formed when lava or magma cools and hardens

8
Examples of Igneous Rocks
9
Several Ways to Classify Igneous Rocks
  1. Intrusive vs. Extrusive
  2. Texture
  3. Composition

10
2. Texture
  1. Coarse Grain Texture
  2. Fine Grain Texture
  3. Glassy Texture

11
Coarse Grain Texture
  • Relatively Large Crystals
  • Formed by slow cooling of magma in Earth

12
Fine Grain texture
  • Smaller Crystals
  • Formed by rapid cooling of magma or lava

13
Glassy Texture
  • Crystals so tiny the rock looks like glass
  • Formed by extremely fast cooling of lava

14
3. Composition
  1. Granitic Composition
  2. Basaltic Composition

15
Granitic Composition
  • Lots of light-colored silicates, esp. quartz and
    feldspar
  • Usually speckled with about 10 dark silicates
  • Make up most of continental crust

16
Basaltic Composition
  • Mainly dark silicates
  • Darker and denser than granite
  • Make up most of ocean floor (formed at ocean
    ridges)

17
Rocks, Part 3
  • Sedimentary Rocks

18
Sedimentary
  • From Latin sedimentum settling
  • Formed when sediments are compacted and cemented
    together

19
Create a Sedimentary Rock in Only 3 Steps!
  • Step 1 Weather/erode parent rock and deposit
    sediment.
  • Step 2 Compact sediment.
  • Step 3 Cement sediment.
  • Voila! Your sedimentary rock is complete.

20
Step 1 Weather/erode parent rock and deposit
sediment.
Table Mountain, South Africa
21
Step 2 Compact sediment.
  • As sediments are buried, the increasing weight of
    sediments above them squishes them together and
    removes most water.

22
Step 3 Cementation.
  • Finally, dissolved minerals are deposited in the
    spaces between the sediments. The minerals
    solidify and cement the particles together (like
    mortar).

23
Examples of Sedimentary Rocks
Rounded, Gravel-sized Sediment
Conglomerate
24
Another Example
Angular Gravel-sized Sediment
Breccia
25
And Another
Sand-sized Sediment Grains
Sandstone
26
Sandstone in Architecture
The Treasury Petra, Jordan
And Its Still Used Today!
27
And Another Example
Fine-grained Sediment
Shale
28
More Sedimentary Rocks
Siltstone
Chalk
Limestone
29
A Special Word About Limestone
  • Very common
  • Main mineral Calcite (CaCO3)
  • Often used as building material
  • Often formed from marine organisms

30
Indiana Limestone in Buildings
AND 35 of 50 Statehouses made of Indiana
Limestone!
National Holocaust Museum
31
Why Studying Sedimentary Rocks is Useful
  • Formed by adding successive layers
  • Contents of layers tell a story of that time
  • Fossils of organisms, floods, volcanoes,
    earthquakes, climate

Limestone from Indiana???
A Trilobite Fossil
32
Rocks, Part 4
  • Metamorphic Rocks

33
Metamorphic
  • To change form due to heat and pressure
  • Formed from either igneous or sedimentary rocks

34
The Role of Heat
  • Provides energy to drive reactions between
    minerals
  • Existing minerals may be re-crystallized into a
    different form or new minerals may be formed
  • Source of heat
  • Contact with magma itself
  • Increasing depth (temperature increases 20-30oC
    per kilometer)

35
Role of Pressure
  • Farther down a rock is buried, the greater the
    pressure
  • Increased pressure smooshes minerals together or
    causes them to re-crystallize
  • Under high temp and pressure, rocks flow
    instead of fracturing

36
Foliated vs. Nonfoliated Metamorphic Rocks
  • Foliated striped
  • Nonfoliated not striped

Gneiss
Marble
37
More Metamorphic Rocks
Slate
Shale
38
Another Meta
Gneiss
Granite
39
And Another
Marble
Limestone
40
One More
Quartzite
Sandstone
41
And Lastly
  • Hornfels
  • No specific composition
  • Was baked by magma in contact the parent rock
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