Weathering - PowerPoint PPT Presentation

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  1. Weathering

  2. Weathering and Erosion • Weathering is the chemical or physicalbreakdown of a rock or mineral due to exposure to the atmosphere. • Erosion is the removalor transport of material by 5 possible agents: running water, glaciers, waves, wind, and gravity. • - wind, water, waves, gravity, glaciers • Humans and animals may also play a part in erosion.

  3. Types of Weathering • There are two major types of weathering: • 1. Physical (mechanical) – mechanical breakdown of rock or mineral. Just breaks it into smaller pieces, composition of the material is NOT changed!! • 2. Chemical – decomposition of material. The composition IS changed!!

  4. Mechanical Weathering – Video Clip

  5. Physical (Mechanical) Weathering • There are several different types of physical weathering: • 1. Frost or Ice Wedging – alternating freezing and thawing of moisture in rockopenings causing rock disintegration. • Water expands as it freezes, this breaks the rock into angular fragments. • Occurs A LOT in Western New York – causes most potholes!! • Will ONLY occur in areas where the temperature alternates above freezing and below freezing!!!

  6. Frost Wedging animation

  7. Physical (Mechanical) Weathering • 2. Exfoliation – Erosion of upper rock causes underlying rock to expand resulting in cracking and peeling of rock in slabs. • Think of onion skin layers and peeling them off!!

  8. Pictures of Stone Mountain, Georgia – exfoliation here has caused an overall rounded shape to the mountain.

  9. Physical (Mechanical) Weathering • 3. Organic Activity – plant roots or animals like burrowing worms can cause rock to breakdown.

  10. Physical (Mechanical) Weathering • 4. Wetting and Drying - addition of water to mineral structure causes structure to expand.

  11. Physical (Mechanical) Weathering • IMPORTANT!! • Physical weathering increasesthe surface area of rocks/minerals. • Taking a rock/mineral and breaking it up into smaller pieces causes it to take up more space (surface area) and will eventually increase the rate of chemical weathering to occur.

  12. Chemical Weathering – Video Clip

  13. Chemical Wethering • There are also several different types of chemical weathering: • 1. Hydrolosis – chemical reaction between waterand other substances. • Silicate minerals will often form clay from this process. Kaolin mine, central Georgia (feldspar weathered into clay by hydrolosis)

  14. Chemical Weathering • 2. Carbonic Acid – dissolving of substances by acids in water often leaving insoluble remains.

  15. Chemical Weathering • 3. Oxidation – chemical reaction of a substance with oxygen causing arust material to form.

  16. Weathering and Climate • Climate plays a very important role in weathering. • The temperature and amount of moisture influences the type of weathering that will occur. • Warm and wet climates produce mostly chemical weathering.Never any frost wedging. • Cool and slightly wet climates produce mostly physical weathering.

  17. Cleopatra’s Needle in Egypt – warm dry climate – little to no weathering occurs Cleopatra’s Needle was moved to New York and has weathered considerably in only 80 years due to the cold and wet climate.

  18. Weathering and Resistance • The harderthe rock or mineral is, the moreresistant it will be to weathering. • Any rock with quartz will be quite resistant due to quartz’s hardness. • What is quartz’s hardness?? • Rocks made mostly ofcalcite, a very soft mineral, will be easily weathered. • What is calcite’s hardness?? 7 3

  19. Porosity and Permeability • Porosity: The percentage of pore space in a material • Permeability: The ability of a material to let liquid (water) pass through it. • Impermeable:When something will not let liquids pass through it(usuallywateris the liquid).

  20. Does the grain size or the size of the sediment affect the porosity? • NO!!!!! • Smaller pieces have smaller gaps between them but there are lots of gaps. • Larger pieces have fewer gaps, but they are larger gaps. • So…the amount of pore space (porosity) does not change with grain size.

  21. MIXED grain sizes WILL affect the porosity though because the small pieces fill in the space between the big pieces. Sorted Unsorted

  22. Permeability • If something has Low Porosity, then permeability will be SLOW • If something has High Porosity, then permeability will be FAST