+ All Categories
Home > Documents > Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills”...

Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills”...

Date post: 29-Jan-2016
Category:
Upload: kathlyn-montgomery
View: 221 times
Download: 0 times
Share this document with a friend
Popular Tags:
57
Rock Cycle
Transcript
Page 1: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Rock Cycle

Page 2: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Why Study Rocks?

Page 3: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Rock Study

Page 4: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Rock Study

Ancient Societies

Page 5: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Rock StudyCultural History

Legends & Sacred Places

Mato Tipila“Bear Lodge”

Paha Sapa“Black Hills”

Badlands

Page 6: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

3 Stages of Rocks

Categorized by the way they form

1. IGNEOUS

2. SEDIMENTARY

3. METAMORPHIC

Page 7: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Rock Cycle

SedimentaryIgneous

Metamorphic

Page 8: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Rock Cycle Simulator

http://www.classzone.com/books/earth_science/terc/content/investigations/es0602/es0602page01.cfm?chapter_no=investigation

Interactive Rock Cycle Animation

Page 9: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Magma

Gasses in Magma

SilicaIronSodiumPotassiumAluminumMagnesium

Water VaporOxygenCarbon DioxideNitrogenHydrogenSulfur Dioxide

Elements in Magma

8 Basic Rock Forming Minerals

OlivinePyroxeneAmphiboleOrthoclasePlagioclaseMuscoviteBiotiteQuartz

Page 10: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

IGNEOUS ROCKSRock-Forming Process: Lava or Magma Cooling

ExtrusiveCools Quickly: PlutonicFine-Grained Crystals

IntrusiveCools Slowly: AphaniticLarge-Grained Crystals

Page 11: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

IGNEOUS ROCKS

Andesite is a gray to black volcanic rock. It is generally erupted from stratovolcanoes as thick lava flows.

Basalt Lava - Basalt is a hard, black volcanic rock. Basaltic lava flows quickly and which allows volcanic gases to escape without explosive events.

Page 12: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

IGNEOUS ROCKSObsidian is usually black in color though it can also be red or have a greenish tint. Obsidian is formed when the lava cools so quickly that crystals do not have time to grow. Obsidian fractures with very sharp edges. Native Americans use it to make knives, arrowheads, and other tools where sharp edges were important. Extrusive

Granite is a common intrusive igneous rock. Because it cools slowly crystals have time to form. The name granite comes from the Latin word granum which means “a grain” for the coarse grain crystalline structure of the rock.

Page 13: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

IGNEOUS ROCKS - TEXTUREVesicles: Gas Pockets

Glassy:No Visible Crystals

Fine:Crystals < 1mm

Coarse:Crystals 1-10 mm

Very Coarse:Crystals > 10 mm

Page 14: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

IGNEOUS ROCKS - COLOR

Felsic90% Light10% Dark

Mafic90% Dark10% Light

Andesitic50% Light50% Dark

UltramaficGreen

Page 15: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Igneous Rock Review

What is the Rock-Forming Process?

Page 16: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Igneous Rock Review

Rock-Forming Process Lava or Magma Cooling

Page 17: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Igneous Rock Review

Rock-Forming Process Lava or Magma Cooling

Two Types of Igneous Rocks?

Page 18: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Igneous Rock Review

Rock-Forming Process Lava or Magma Cooling

Two Types of Igneous Rocks 1. Extrusive 2. Intrusive

Page 19: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Igneous Rock Review

Rock-Forming Process Lava or Magma Cooling

Two Types of Igneous Rocks 1. Extrusive 2. Intrusive

2 Igneous Rocks?

Page 20: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Igneous Rock Review

Rock-Forming Process Lava or Magma Cooling

Two Types of Igneous Rocks 1. Extrusive or Plutonic 2. Intrusive or Aphanitic

4 Igneous Rocks1. Andesite 2. Basalt3. Obsidian 4. Granite

Page 21: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

SEDIMENTARY ROCKSThree Unique Processes Results in Three Main Groups

Clastic Chemical Organic

Page 22: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Clastic Sedimentary RocksRock-forming Process: Erosion & Compaction - Cementation

Weathering: Wind, Rain, Moving Water, Freezing Water Breaks Rocks Into Smaller Pieces

Erosion: Combination of Weathering & Movement of Sediment

Sediments: The Smaller Pieces of Weathered Rocks

Deposition: Sediment Settled Out of Wind, Moving Water or Due to Gravity

Lithification: The Process of Sediment Changing to Rock

Compaction: After sediments are deposited - The weight of the sediments squeezes the particles together. When more and more sediments are deposited on top, the weight on the sediments below increases.

Cementation: Dissolved minerals fill in the spaces between the sediment particles. These liquid minerals act as glue or cement to bind the sediments together.

Waterborne sediments squeeze so tightly together that most of the water is pushed out.

Page 23: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Clastic Sedimentary Rocks

Erosion

Page 24: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Clastic Sedimentary Rocks

Page 25: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Conglomerate is made up of rounded pebbles cemented together.

Breccia is made up of angular pebbles cemented together.

Sandstone is sand grains cemented together into solid stone.

Page 26: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Siltstone is made from silt particles cemented together.

Shale is made from silt particles cemented together. It is similar to siltstone but with even finer grain size.

Page 27: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Chemical Sedimentary Rocks

Positive & Negative atoms crystallize into solid mineral crystals. This process is called precipitation. Precipitation can occur within an ocean, a lake, a cave, or where a hot spring flows out onto Earth's surface.

Rock-Forming Process: Chemicals Reactions Form Minerals in Water

Carbonates: Composed mainly of carbonate minerals. Dolomite Limestone.

Dolomite

Page 28: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Chemical Sedimentary Rocks

Evaporites: Evaporation leaves water enriched with calcium, sodium, and chlorine atoms – Which then precipitate from the water Halite or rock salt Gypsum

Siliceous: Composed of an exceptionally high amount of crystalline siliceous material, mainly the mineral quartz Chert

Page 29: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Organic Sedimentary Rocks

Rock-Forming Process: Organic Matter (Plants)

Coal:

Lignite is black and has a crumbly consistency

Bituminous coal can be dull to shiny and black.

Page 30: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Sedimentary Rock Review

3 Main Groups of Sedimentary Rocks?

Page 31: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Sedimentary Rock Review

3 Main Groups of Sedimentary Rocks

Clastic Chemical Organic

Page 32: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Sedimentary Rock Review

3 Main Groups of Sedimentary Rocks

Clastic Chemical Organic

Rock-Forming Processes for each Main Group?

Page 33: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Sedimentary Rock Review

3 Main Groups of Sedimentary Rocks

Clastic Chemical Organic

Rock-Forming Processes for each Main Group?

Erosion & Compaction - Cementation

Page 34: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Sedimentary Rock Review

3 Main Groups of Sedimentary Rocks

Clastic Chemical Organic

Rock-Forming Processes for each Main Group?

Erosion & Compaction - Cementation

Chemicals Reactions Form Minerals in Water

Page 35: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Sedimentary Rock Review

3 Main Groups of Sedimentary Rocks

Clastic Chemical Organic

Rock-Forming Processes for each Main Group?

Erosion & Compaction - Cementation

Chemicals Reactions Form Minerals in Water

Organic Matter

Page 36: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Sedimentary Rock Review3 Main Groups of Sedimentary Rocks

Clastic Chemical Organic

Rock-Forming Processes for each Main Group?

Erosion & Compaction - CementationChemicals Reactions Form Minerals in Water

Organic MatterExamples from Each Main Group?

Page 37: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Sedimentary Rock Review3 Main Groups of Sedimentary Rocks

Clastic Chemical Organic

Rock-Forming Processes for each Main Group?

Erosion & Compaction - CementationChemicals (Elements) Dissolved in Water

Organic MatterConglomerateBrecciaSandstoneSiltstoneShale

Page 38: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Sedimentary Rock Review3 Main Groups of Sedimentary Rocks

Clastic Chemical Organic

Rock-Forming Processes for each Main Group?

Erosion & Compaction - CementationChemicals (Elements) Dissolved in Water

Organic MatterConglomerateBrecciaSandstoneSiltstoneShale

LimestoneDolomiteRock SaltGypsumChert

Page 39: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Sedimentary Rock Review3 Main Groups of Sedimentary Rocks

Clastic Chemical Organic

Rock-Forming Processes for each Main Group?

Erosion & Compaction - CementationChemicals (Elements) Dissolved in Water

Organic MatterConglomerateBrecciaSandstoneSiltstoneShale

LimestoneDolomiteRock SaltGypsumChert

Coal

Page 40: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Rock-Forming Process: Heat & Pressure

Heat - Gravity Pulls Crust Downward- Increases Further Downward

Pressure

Hydrothermal Solution- Hot Steam Escapes from Mantle Carrying Dissolved Minerals - Dissolves Existing Minerals in Rocks & Deposits New Minerals - Recrystallization Alters the Rock’s Composition

- Energy Source for Chemical Reactions- Mantle- Friction- Increases Further Downward

Page 41: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Rock-Forming Process: Heat & Pressure

Contact metamorphism

- Magma forces into existing rock- Heat bakes surrounding rock- Small, low-grade metamorphism

Metamorphic Rock Marble: Created from limestone that has been subjected to heat

Page 42: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Rock-Forming Process: Heat & Pressure

Regional metamorphism

- Affects Large Regions- High-grade Metamorphism- Mountain-Building

Black Canyon of The Gunnison

Gneiss

Pegmatite

Page 43: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.
Page 44: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Foliated Non-foliated

Bands or LayersProgressing Through Stages of Metamorphism

One Mineral

Two Main Groups

Page 45: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.
Page 46: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Shale

Slate

Schist

Gneiss

Page 47: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Shale, Mudstone, Siltstone (Very Fine Grained)

Slate (Fine Grained)

Schist (Medium – Coarse Grained)

Granite, Igneous Rocks

Gneiss (Medium – Coarse Grained)

Textures

Page 48: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Limestone

Marble (Medium – Coarse Grained)

Quartz Sandstone

Quartzite (Medium – Coarse Grained)

Page 49: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

What are the 2 groups?

Page 50: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

What are the 2 groups?

Foliated Non-Foliated

Page 51: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

What are the 2 groups?

Foliated Non-Foliated

What are the foliated stages?

Page 52: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

What are the 2 groups?

Foliated Non-Foliated

What are the foliated stages?

Shale – Slate – Schist – Gneiss

Page 53: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

What are the 2 groups?

Foliated Non-Foliated

What are the foliated stages?

Shale – Slate – Schist – Gneiss

What are the Non-Foliated rocks & why are they non-foliated?

Page 54: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

What are the 2 groups?

Foliated Non-Foliated

What are the foliated stages?

Shale – Slate – Schist – Gneiss

What are the Non-Foliated rocks & why are they non-foliated?

Marble & Quartzite – They are composed of single minerals

Page 55: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Rock Cycle

SedimentaryIgneous

Metamorphic

Page 56: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

Rock ReflectionCultural History

Legends & Sacred Places

Mato Tipila“Bear Lodge”

Paha Sapa“Black Hills”

Igneous Rock - Intrusive

Sedimentary – LimestoneMetamorphic - Granite

Sedimentary – Deposition & ErosionsFossils of Extinct MammalsMetamorphic - Shale

Badlands

Page 57: Rock Cycle Why Study Rocks? Rock Study Mato Tipila “Bear Lodge” Paha Sapa “Black Hills” Badlands.

References

http://www.rocksandminerals4u.com/igneous_rock_cycle.html


Recommended