mechanical chemical biological rocks eventually form sediment rocks - stationary

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Page 1: Mechanical  Chemical  Biological  Rocks eventually form sediment  Rocks - stationary
Page 2: Mechanical  Chemical  Biological  Rocks eventually form sediment  Rocks - stationary
Page 3: Mechanical  Chemical  Biological  Rocks eventually form sediment  Rocks - stationary

MechanicalChemicalBiological

Rocks eventually form sedimentRocks - stationary

Page 4: Mechanical  Chemical  Biological  Rocks eventually form sediment  Rocks - stationary

Definition Mechanisms

Produces finer particles by fracturing rock

Mineral composition remains the same

Abrasion (grinding)

Crystallization (frost shattering)

Thermal fracturing (rapid heat change)

Hydration (Expansion of water)

Exfoliation (pressure release jointing)

Page 5: Mechanical  Chemical  Biological  Rocks eventually form sediment  Rocks - stationary
Page 6: Mechanical  Chemical  Biological  Rocks eventually form sediment  Rocks - stationary

Definition Processes

Chemical reactions transform rocks and minerals into new chemical combinations that are stable under prevailing conditions at or near the Earth's surface.

Rock disintegrates

Hydrolysis & Hydration (involve water)

Oxidation & Reduction (combines with O or loss of O)

Solution/Dissolution (carbonates & carbon dioxides combine with form carbonic acid)◦ CO2 + H2O = H2CO3  

Page 7: Mechanical  Chemical  Biological  Rocks eventually form sediment  Rocks - stationary

Chemical weathering Not all minerals are prone to chemical weathering

Faster in warmer climates HeatWater

Page 8: Mechanical  Chemical  Biological  Rocks eventually form sediment  Rocks - stationary

Definition Photo Examples

Biological weathering can be considered special types of mechanical or chemical weathering

Action of living organism Plants & Animals Bacteria, algae and lichens

Secrete acids, chemicals

Page 9: Mechanical  Chemical  Biological  Rocks eventually form sediment  Rocks - stationary

Definition Agents

Removal and movement of earth materials by natural agents.

Some of these agents include glaciers, wind, water, earthquakes, volcanoes, tornadoes, hurricanes, mud flows, and avalanches.

Water Wind Glaciers

Page 10: Mechanical  Chemical  Biological  Rocks eventually form sediment  Rocks - stationary

http://www.bbc.co.uk/learningzone/clips/3079.bb.rm

Chandeleur Islands

Page 11: Mechanical  Chemical  Biological  Rocks eventually form sediment  Rocks - stationary

Weathering 2 processes No movement

Mass WastingMovement of rock particle – gravity

ErosionFlowing Agent

Page 12: Mechanical  Chemical  Biological  Rocks eventually form sediment  Rocks - stationary

Splash erosion Sheet erosion Fluvial erosion Waves Glacial erosion

AbrasionPlucking

Page 13: Mechanical  Chemical  Biological  Rocks eventually form sediment  Rocks - stationary

Waves in oceans and other large bodies of water cause coastal

erosion. The power of ocean waves is awesome; large storm waves can produce 2000 pounds of pressure per square foot. The pure energy of waves along with the chemical content of the water is what erodes the rock of the coastline. Aeolian Erosion

Page 14: Mechanical  Chemical  Biological  Rocks eventually form sediment  Rocks - stationary

Wave action in Calvert County Maryland

Page 15: Mechanical  Chemical  Biological  Rocks eventually form sediment  Rocks - stationary

Aeolian Erosion – Wind erosion, sand dunes

Page 16: Mechanical  Chemical  Biological  Rocks eventually form sediment  Rocks - stationary

Effects of mechanical weathering http://www.classzone.com/books/earth_science/terc/content/visualizations/es1201/es1201page01.cfm?chapter_no=visualization

Effects of chemical weathering http://www.classzone.com/books/earth_science/terc/content/visualizations/es1202/es1202page01.cfm?chapter_no=visualization

Landscape formed by erosion http://www.classzone.com/books/earth_science/terc/content/visualizations/es1205/es1205page01.cfm?chapter_no=visualization

Sediment transfer – flowing water http://www.classzone.com/books/earth_science/terc/content/visualizations/es1303/es1303page01.cfm?chapter_no=visualization

Channels in meandering river http://www.classzone.com/books/earth_science/terc/content/visualizations/es1306/es1306page01.cfm?

chapter_no=visualization

Waterfalls and chasms http://www.classzone.com/books/earth_science/terc/content/visualizations/es1305/

es1305page01.cfm?chapter_no=visualization

Glacial erosion of bedrock http://www.classzone.com/books/earth_science/terc/content/visualizations/es1502/es1502page01.cfm?

chapter_no=visualization

Example of wave erosion◦ http://www.classzone.com/books/earth_science/terc/content/visualizations/es1606/es1606page01.cfm?

chapter_no=visualization