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Presented By:
        M Sajjad (907)
            Ph# +923346544625
οƒ’   Introduction
        οƒ’   Definition
        οƒ’   Weathering vs. erosion
οƒ’   Types of weathering
        οƒ’   Mechanical weathering
        οƒ’   Agents of Mechanical weathering
              οƒ’   Frost Action
              οƒ’   Pressure Release (Exfoliation)
              οƒ’   Insulation
              οƒ’   Some minor Agents of Mechanical weathering
        οƒ’   Chemical weathering
        οƒ’   Main process of Chemical Weathering
              οƒ’   Hydrolysis
              οƒ’   Oxidation
              οƒ’   Carbonation
              οƒ’   Acidic Rain
              οƒ’   Solution
        οƒ’   Biological weathering
οƒ’   Mechanical weathering vs. chemical weathering
οƒ’   Factors af fecting weathering
οƒ’   Significance of weathering
οƒ’   β€œWeathering is the process of disintegration and
          decomposition of rocks of the earth’s surface”.

οƒ’   Weathering Vs. Erosion
οƒ’   Mechanical weathering
       οƒ’   Disintegration by physical agents
       οƒ’   Composition of rock does not change
οƒ’   Frost Action
       οƒ’   Weathering process by ice
       οƒ’   Water increases in volume by about 9% when it freezes
       οƒ’   Produces about 1890 metric tons pressure for every 1 ft2
       οƒ’   Common in high altitude zones
οƒ’   Pressure Release (Exfoliation)
       οƒ’   Metamorphic and intrusive igneous rocks are under
           pressure
       οƒ’   Upper layer is removed by erosion
       οƒ’   Due to pressure release the cracks are formed
οƒ’   Insolation
       οƒ’   Common in arid and desert regions
       οƒ’   Temperature is high in day time and low in night
       οƒ’   Disintegration due to expansion and contraction
            οƒ’   Block Disintegration
            οƒ’   Granular disintegration
οƒ’   Rainfall
οƒ’   Gravity
οƒ’   Salt wedging
οƒ’   Weathering process by chemical agents
οƒ’   Composition of rocks is changed
These weathered tombstones are from a burying ground in
Boston, Massachusetts. The marker on the left, carved in marble,
has been strongly weathered, weakening the lettering. The
marker on the right, made of slate, is much more resistant to
erosion.
οƒ’   Hydrolysis
         οƒ’   Addition of water
         οƒ’   When minerals are moistened, hydrolysis occurs.

                      H2O + CO2 + CaCO3 --> Ca+2 + 2HCO3-
οƒ’   water + carbon dioxide + calcite dissolve into calcium ion and bicarbonate ion
Feldspars to clay

         + H 2 CO 3 (acid)
οƒ’   Oxidation
       οƒ’   Iron combines with oxygen in the presence of water in a
           processes called oxidation
       οƒ’   The product of oxidation is rust
οƒ’   Carbonation
      οƒ’   Mostly in humid areas
      οƒ’   CO2 dissolves in rain water and creates carbonic acid
      οƒ’   Carbonic acid easily weathers limestone and marble
      CaCo3+H2CO3                           Ca2+ + 2HCO3
οƒ’   Acidic Rain
      οƒ’   Compounds from burning coal, oil and gas react chemically with
          water forming acids.
      οƒ’   Acid rain causes very rapid chemical weathering
οƒ’   Solution
       οƒ’   Rock salt and gypsum may be dissolved by water and
           then removed in solution
οƒ’   Can be both chemical and mechanical in
    nature.

    β€’   roots split rocks apart

    β€’   roots produce acids
        that dissolve rocks.
β€’   Animal And
    Insects
β€’   Vegetation
β€’   Human
    Activities
MECHANICAL WEATHERING                  CHEMICAL WEATHERING
 οƒ’   Rocks are disintegrated by         οƒ’   Rocks are decomposed by
     physical force                         chemical action
 οƒ’   There is no chemical change        οƒ’   Rocks undergo chemical change
                                        οƒ’   Prominent in hot and humid
 οƒ’   Prominent in dry and cool areas        areas
 οƒ’   Rocks are broken into great        οƒ’   Only surface rocks are affected
     depth                              οƒ’   Hard rock like quartz resist
 οƒ’   Hard rocks are weathered too           chemical weathering
οƒ’   Nature of rock
οƒ’   Slope of land
οƒ’   Joints
οƒ’   Vegetation cover
οƒ’   Climate
οƒ’   Landforms
οƒ’   Formation of sedimentary rocks
οƒ’   Mass wasting
οƒ’   Regolith formation
Niche habitation of native Americans wall of canyon de chelly
Arizona
This granite outcrop in Yosemite National Park, California, displays sheetlike joints, giving a
stepped appearance to the mountain slope.
οƒ’   Monolith
οƒ’   Buttes
οƒ’   Mesas
Monoli           Mesa
  th




         Butte
οƒ’   Bajwa.A.S, β€œModern Physical Geography” publishers emporium Urdu Bazar
    Lahore
οƒ’   Strahler.A β€œPhysical Geography” 2nd 2005
οƒ’   http://www.soils.wisc.edu/courses/SS325/weathering.htm
οƒ’   http://www.physicalgeography.net/fundamentals/10s.html

οƒ’   http://russiatrek.org/blog/nature/the-weathering-pillars-of-komi-republic-
    photos/
οƒ’   http://www.allrussiantours.com/natural-attractions/pillars-of-
    weathering.html
Presentation of geomorphology corrected

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Presentation of geomorphology corrected

  • 1. Presented By: M Sajjad (907) Ph# +923346544625
  • 2. οƒ’ Introduction οƒ’ Definition οƒ’ Weathering vs. erosion οƒ’ Types of weathering οƒ’ Mechanical weathering οƒ’ Agents of Mechanical weathering οƒ’ Frost Action οƒ’ Pressure Release (Exfoliation) οƒ’ Insulation οƒ’ Some minor Agents of Mechanical weathering οƒ’ Chemical weathering οƒ’ Main process of Chemical Weathering οƒ’ Hydrolysis οƒ’ Oxidation οƒ’ Carbonation οƒ’ Acidic Rain οƒ’ Solution οƒ’ Biological weathering οƒ’ Mechanical weathering vs. chemical weathering οƒ’ Factors af fecting weathering οƒ’ Significance of weathering
  • 3. οƒ’ β€œWeathering is the process of disintegration and decomposition of rocks of the earth’s surface”. οƒ’ Weathering Vs. Erosion
  • 4. οƒ’ Mechanical weathering οƒ’ Disintegration by physical agents οƒ’ Composition of rock does not change
  • 5. οƒ’ Frost Action οƒ’ Weathering process by ice οƒ’ Water increases in volume by about 9% when it freezes οƒ’ Produces about 1890 metric tons pressure for every 1 ft2 οƒ’ Common in high altitude zones
  • 6.
  • 7. οƒ’ Pressure Release (Exfoliation) οƒ’ Metamorphic and intrusive igneous rocks are under pressure οƒ’ Upper layer is removed by erosion οƒ’ Due to pressure release the cracks are formed
  • 8.
  • 9. οƒ’ Insolation οƒ’ Common in arid and desert regions οƒ’ Temperature is high in day time and low in night οƒ’ Disintegration due to expansion and contraction οƒ’ Block Disintegration οƒ’ Granular disintegration
  • 10.
  • 11. οƒ’ Rainfall οƒ’ Gravity οƒ’ Salt wedging
  • 12. οƒ’ Weathering process by chemical agents οƒ’ Composition of rocks is changed
  • 13. These weathered tombstones are from a burying ground in Boston, Massachusetts. The marker on the left, carved in marble, has been strongly weathered, weakening the lettering. The marker on the right, made of slate, is much more resistant to erosion.
  • 14. οƒ’ Hydrolysis οƒ’ Addition of water οƒ’ When minerals are moistened, hydrolysis occurs. H2O + CO2 + CaCO3 --> Ca+2 + 2HCO3- οƒ’ water + carbon dioxide + calcite dissolve into calcium ion and bicarbonate ion
  • 15. Feldspars to clay + H 2 CO 3 (acid)
  • 16.
  • 17. οƒ’ Oxidation οƒ’ Iron combines with oxygen in the presence of water in a processes called oxidation οƒ’ The product of oxidation is rust
  • 18. οƒ’ Carbonation οƒ’ Mostly in humid areas οƒ’ CO2 dissolves in rain water and creates carbonic acid οƒ’ Carbonic acid easily weathers limestone and marble CaCo3+H2CO3 Ca2+ + 2HCO3
  • 19. οƒ’ Acidic Rain οƒ’ Compounds from burning coal, oil and gas react chemically with water forming acids. οƒ’ Acid rain causes very rapid chemical weathering
  • 20.
  • 21. οƒ’ Solution οƒ’ Rock salt and gypsum may be dissolved by water and then removed in solution
  • 22.
  • 23. οƒ’ Can be both chemical and mechanical in nature. β€’ roots split rocks apart β€’ roots produce acids that dissolve rocks.
  • 24. β€’ Animal And Insects β€’ Vegetation β€’ Human Activities
  • 25. MECHANICAL WEATHERING CHEMICAL WEATHERING οƒ’ Rocks are disintegrated by οƒ’ Rocks are decomposed by physical force chemical action οƒ’ There is no chemical change οƒ’ Rocks undergo chemical change οƒ’ Prominent in hot and humid οƒ’ Prominent in dry and cool areas areas οƒ’ Rocks are broken into great οƒ’ Only surface rocks are affected depth οƒ’ Hard rock like quartz resist οƒ’ Hard rocks are weathered too chemical weathering
  • 26. οƒ’ Nature of rock οƒ’ Slope of land οƒ’ Joints οƒ’ Vegetation cover οƒ’ Climate
  • 27. οƒ’ Landforms οƒ’ Formation of sedimentary rocks οƒ’ Mass wasting οƒ’ Regolith formation
  • 28.
  • 29.
  • 30. Niche habitation of native Americans wall of canyon de chelly Arizona
  • 31. This granite outcrop in Yosemite National Park, California, displays sheetlike joints, giving a stepped appearance to the mountain slope.
  • 32.
  • 33.
  • 34.
  • 35.
  • 36. οƒ’ Monolith οƒ’ Buttes οƒ’ Mesas
  • 37. Monoli Mesa th Butte
  • 38. οƒ’ Bajwa.A.S, β€œModern Physical Geography” publishers emporium Urdu Bazar Lahore οƒ’ Strahler.A β€œPhysical Geography” 2nd 2005 οƒ’ http://www.soils.wisc.edu/courses/SS325/weathering.htm οƒ’ http://www.physicalgeography.net/fundamentals/10s.html οƒ’ http://russiatrek.org/blog/nature/the-weathering-pillars-of-komi-republic- photos/ οƒ’ http://www.allrussiantours.com/natural-attractions/pillars-of- weathering.html