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HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

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Weathering Chemical and physical alteration of rock and minerals when exposed to air, moisture, and organic matter –Chemical weathering - minerals in a rock are chemically altered or dissolved –Physical weathering - solid rock fragmented by mechanical breaking University of Georgia Examples?

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Page 1: HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

HCDE-LPI Workshop onSedimentary Processes

Good Morning!!

Page 2: HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

WeatherinWeathering…g…Let’s break it Let’s break it

down…down…

Page 3: HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

Weathering• Chemical and physical alteration of rock

and minerals when exposed to air, moisture, and organic matter– Chemical weathering - minerals in a

rock are chemically altered or dissolved

– Physical weathering - solid rock fragmented by mechanical breaking

University of Georgia

Examples?

Page 4: HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

What Controls the Rate of Weathering?

• Parent Material (minerals and structure)• Climate (rainfall and temperature)• Biology• Slope• Presence / Absence of Soil • Exposure Time

Page 5: HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

Chemical Weathering• Chemical weathering - minerals in a rock

are chemically altered or dissolved • Minerals weather at different rates

because of differences in chemical stability; the resistance of a mineral to change

Page 6: HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

Which Minerals are More Stable?

Less?

Page 7: HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

Our Hero Bowen & His Reaction Series

Skinner and Porter, 1992

Page 8: HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

Physical Weathering• Physical weathering - solid rock

fragmented by mechanical breaking• Factors affecting:

– Slope – Zones of weakness - joints– Organisms - flora (and fauna)– Freeze/thaw (frost wedging)– Crystal growth – Heat / Cold

Page 9: HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

Slope• Things move downhill …. Why?• Gravity aids in the breakdown and transport of material• Slope starts it all!

Page 10: HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

Mass Movements (Mass Wasting)

• Mass movement is the down slope movement of earth materials under the influence of gravity

www.physicalgeography.net

Page 11: HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

Rock Mass Movements• Fall - fast; rocks break and fall

www.physicalgeography.net

Page 12: HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

www.geology.com

Page 13: HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

Rock Mass Movements

• Slide - (land slide) moderate; rocks slide as a unit

Source: USGS

Page 14: HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

Unconsolidated Mass Movements

• Creep - very slow flow downhill; top moves faster than base

Source: North Dakota State University

Page 15: HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

Unconsolidated Mass Movement

• Slump - moderate; slide of material as a unit along a lower surface (spoon-shaped)

Page 16: HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

Why Do We Care?• Human Impacts of mass wasting …

• Year Location Type Fatalities• 1916 It/Aust Landslide 10,000• 1920 China Earthquake triggered landslide 200,000• 1945 Japan Flood triggered landslide 1,200• 1949 USSR Earthquake triggered landslide 12-20,000• 1954 Austria Landslide 200• 1962 Peru Landslide 4,000-5,000• 1963 Italy Landslide 2,000• 1970 Peru Earthquake related debris avalanche 70,000• 1985 Columb Mudflow related to volcanic eruption 23,000• 1987 Ecuador Earthquake related landslide 1,000

• In a typical year in the United States, landslides cause over $1.5 billion in damages and 25 to 50 deaths

http://www.tulane.edu/~sanelson/geol204/masswastproc.htm

Page 17: HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

Joints

http://www.geo.duke.edu/geo41/st045.gif

Page 18: HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

http://www.geo.duke.edu/geo41/wea017.gif

Page 19: HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

Chemical Weathering Along Joints

….. Where the Water Goes …..

http://www.geo.duke.edu/geo41/wea017.gif

Spheroidal Surfaces

Page 20: HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

http://www.geo.duke.edu/geo41/wea003.gif

Roots and Critters

Page 21: HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

Crystal Growth

http://www.geo.duke.edu/geo41/wea001.gif

Page 22: HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

http://ww

w.usd.edu/esci/figures/150651.JPG

Frost Wedging

Page 23: HCDE-LPI Workshop on Sedimentary Processes Good Morning!!

In what environments will chemical weathering be

greatest?

Physical?