Chapter 4 - Rocks What can be learned by studying rocks… We can learn mo better about earth. So...
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Transcript of Chapter 4 - Rocks What can be learned by studying rocks… We can learn mo better about earth. So...
Chapter 4 - Rocks
What can be learned by studying rocks…
We can learn mo better about earth.
So what is a rock???
It’s a mixture of 1 or more minerals. Easy.
The Rock Cycle
• Shows how any rock may be transformed from one type into another.
• It’s a continuous process that causes rocks to change.
Vocab terms
• Magma – underground molten rock
• Lava – above ground molten rock
• Crystallization – formation of minerals from cooling magma/lava
• Weathering – any process that breaks down rocks into smaller pieces (sediment)
Vocab terms
• Erosion – transportation of sediment
• Deposition – accumulation of sediment
• Metamorphism – changing one type of rock into another by heat/pressure/chemicals
• Lithification – compaction and cementation of sediment
Igneous Rocks…from fire
• 2 main types
– Intrusive (large crystals)
• From magma
• Underground
• Cools and forms slowly
– Extrusive (small crystals)
• From lava
• Above ground
• Cools and forms quickly
Igneous Rocks Classification
• 2 ways to classify igneous rocks
1 = Texture 2 = composition
1. Texture (3 types)
a) Coarse grained – slow cooling, large crystals
b) Fine grained – fast cooling, small crystals
c) Glassy – super fast cooling, glassy
Porphyritic – slow and fast cooling, has both large and small crystals
Course-Grained Igneous Texture
Fine-Grained Igneous Texture
Obsidian Exhibits a Glassy Texture.
• 2. Composition
• Granitic (felsic)
– High in silica (SiO4), light colored, lower density
• Basaltic (mafic)
– Low in silica, dark colored, high in iron and magnesium higher density
• Andesitic (intermediate)
• Ultramafic
Sedimentary Rocks
Your teacher rocks!
Sedimentary Rocks
• From (Latin) sedimentum = settling
• Made from sediments of any type
• 4 agents of erosion (transportation)
1. Water
2. Wind
3. Glaciers
4. Gravity
3 Types Sedimentary Rock
1. Clastic = formed from sediment
2. Chemical = formed from precipitation or evaporation…dried up soda on a table
3. Biochemical (organic) = formed from remains of once living organisms
1) Clastic Sedimentary Rocks
• Conglomerate – rounded pebble sized
• Breccia – angular pebble sized
• Sandstone – sand sized
• Siltstone – silt sized
• Shale – clay sized
Conglomerate
2) Chemical Sedimentary Rocks
• Crystalline limestone – precipitates from ocean water
• Gypsum – precipitates from oceans, too
• Travertine – precipitates in caves
• Chert/flint – quartz
• Rock salt – evaporated salt water
3) Biochemical Sedimentary Rx
• Fossil limestone – fossil remains
• Coquina – shells and shell fragments
• Chalk – microscopic shells and clay
• Bituminous coal (B coal) – plant remains
Metamorphic Rocks
• Means to change form
• 2 types of metamorphism
1. Contact
- small areas from toughing hot magma
2. Regional
- large areas from the pressures of mountain building
Agents of Metamorphism
1. Heat (temperature)
2. Pressure (stress)
3. Reactions in hot solutions (chemicals)
Metamorphic Rock Classification
• 2 textures
1. Foliated - layered
2. Nonfoliated – not layered
1. Foliated Metamorphic Rx
A) Slate – very thin layers from shale
B) Phyllite – thin layers, sheen, wavy, from slate
C) Schist – medium layers,shiny, micas, from phyllite
D) Gneiss – distinct black & white layers, from schist or granite
2. Nonfoliated Metamorphic RX
A) Marble – shiny, fizzes in acid, H = 3, from limestone
B) Quartzite – shiny, won’t fizz, H = 6 – 7, from sandstone
C) Anthracite coal – shiny, black, from bituminous coal
The carbon cycle…see page 85
TREE
1. Igneous Rx
A) Intrusive