Title: Rocks
1Rocks
2Whats a Rock?
- A solid chunk of one or more minerals (or
sometimes mineral-like matter)
3The Rock Cycle
4A 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
5More 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
6Rocks, Part 2
7Igneous
- From Latin ignis FIRE!
- Formed when lava or magma cools and hardens
8Examples of Igneous Rocks
9Several Ways to Classify Igneous Rocks
- Intrusive vs. Extrusive
- Texture
- Composition
102. Texture
- Coarse Grain Texture
- Fine Grain Texture
- Glassy Texture
11Coarse Grain Texture
- Relatively Large Crystals
- Formed by slow cooling of magma in Earth
12Fine Grain texture
- Smaller Crystals
- Formed by rapid cooling of magma or lava
13Glassy Texture
- Crystals so tiny the rock looks like glass
- Formed by extremely fast cooling of lava
143. Composition
- Granitic Composition
- Basaltic Composition
15Granitic Composition
- Lots of light-colored silicates, esp. quartz and
feldspar - Usually speckled with about 10 dark silicates
- Make up most of continental crust
16Basaltic Composition
- Mainly dark silicates
- Darker and denser than granite
- Make up most of ocean floor (formed at ocean
ridges)
17Rocks, Part 3
18Sedimentary
- From Latin sedimentum settling
- Formed when sediments are compacted and cemented
together
19Create 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.
20Step 1 Weather/erode parent rock and deposit
sediment.
Table Mountain, South Africa
21Step 2 Compact sediment.
- As sediments are buried, the increasing weight of
sediments above them squishes them together and
removes most water.
22Step 3 Cementation.
- Finally, dissolved minerals are deposited in the
spaces between the sediments. The minerals
solidify and cement the particles together (like
mortar).
23Examples of Sedimentary Rocks
Rounded, Gravel-sized Sediment
Conglomerate
24Another Example
Angular Gravel-sized Sediment
Breccia
25And Another
Sand-sized Sediment Grains
Sandstone
26Sandstone in Architecture
The Treasury Petra, Jordan
And Its Still Used Today!
27And Another Example
Fine-grained Sediment
Shale
28More Sedimentary Rocks
Siltstone
Chalk
Limestone
29A Special Word About Limestone
- Very common
- Main mineral Calcite (CaCO3)
- Often used as building material
- Often formed from marine organisms
30Indiana Limestone in Buildings
AND 35 of 50 Statehouses made of Indiana
Limestone!
National Holocaust Museum
31Why 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
32Rocks, Part 4
33Metamorphic
- To change form due to heat and pressure
- Formed from either igneous or sedimentary rocks
34The 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)
35Role 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
36Foliated vs. Nonfoliated Metamorphic Rocks
Gneiss
Marble
37More Metamorphic Rocks
Slate
Shale
38Another Meta
Gneiss
Granite
39And Another
Marble
Limestone
40One More
Quartzite
Sandstone
41And Lastly
- Hornfels
- No specific composition
- Was baked by magma in contact the parent rock