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17.4 Weathering and Erosion

To do:
• Class reading: page 583 – 588.
•    Individual Silent Work: Vocabulary starting page 583
17.4 Weathering and Erosion

Weathering – The change in the physical form or
chemical composition 0f rock materials exposed at
Earth’s surface.

Two types of the Weathering process:
  1. Physical or mechanical – it is a kind of
      weathering that breaks rocks into smaller pieces
      but does not alter the rocks’ chemical
      composition.
17.4 Weathering and Erosion

Two types of the Weathering process:
  1. Physical or mechanical – it is a kind of
      weathering that breaks rocks into smaller pieces
      but does not alter the rocks’ chemical
      composition.
     a. Ice (frost wedging) – occurs when water seeps
        into cracks or joints in rocks and then freezes.
        When water freezes, its volume increase by
        about 10% pushing the rock apart.
17.4 Weathering and Erosion

  a. Ice (frost wedging) – occurs when water seeps
     into cracks or joints in rocks and then freezes.
     When water freezes, its volume increase by
     about 10% pushing the rock apart.
  b. Plants (plant wedging) – occurs when roots
     grow into cracks in the rocks. As the plant
     grows, the roots exert a constant pressure on
     the rock. The crack continues to deepen and
     widen, eventually causing a piece of the rock
     to break off.
17.4 Weathering and Erosion

   b. Plants (plant wedging) – occurs when roots
      grow into cracks in the rocks. As the plant
      grows, the roots exert a constant pressure on
      the rock. The crack continues to deepen and
      widen, eventually causing a piece of the rock
      to break off.

2. Chemical Weathering- kind of weathering that
   breaks down rocks by changing its chemical
   composition.
17.4 Weathering and Erosion

2. Chemical Weathering- kind of weathering that
   breaks down rocks by changing its chemical
   composition.

   a. Oxidation – When certain elements, specially
      metals, react with oxygen, they become
      oxides and their properties change.
17.4 Weathering and Erosion

  a. Oxidation – When certain elements, specially
     metals, react with oxygen, they become
     oxides and their properties change.
     - Oxidation in minerals causes minerals to
        decompose or form new minerals causing
        both chemical and physical appearance of
        the rock to change.
  b. Carbon dioxide – carbon dioxide in the air
     dissolves in rainwater resulting to a carbonic
     acid.
17.4 Weathering and Erosion

  b. Carbon dioxide – carbon dioxide in the air
     dissolves in rainwater resulting to a carbonic
     acid.
     - Although carbonic acid is a weak acid, it
        reacts with minerals, seeps into the ground
        and weather rocks underground.
     - Acid rain – slowly dissolves minerals caused
        burning fossil fuels in cars, power stations,
        factories
17.4 Weathering and Erosion

    - Although carbonic acid is a weak acid, it
      reacts with minerals, seeps into the ground
      and weather rocks underground.
    - Acid rain – slowly dissolves minerals caused
      burning fossil fuels in cars, power
      stations, factories.
    - Acid rain damages both living organisms
      and non-living matter.
17.4 Weathering and Erosion

        - Acid rain damages both living organisms
           and non-living matter.

How does pollution contribute to acid rain?
- Coal, oil and gasoline – release gases including
  sulfur dioxide reacting with water in the air and
  clouds to form nitric acid or nitrous acid and sulfuric
  acid.
17.4 Weathering and Erosion

How does pollution contribute to acid rain?
- Coal, oil and gasoline – release gases including
   sulfur dioxide reacting with water in the air and
   clouds to form nitric acid or nitrous acid and sulfuric
   acid.
 - US Act of 1970 (Clean Air Act) – reduced the release
   of chemicals that cause acid rains. Acidity of rain is
   greatly reduced.
17.4 Weathering and Erosion

 - US Act of 1970 (Clean Air Act) – reduced the release
   of chemicals that cause acid rains. Acidity of rain is
   greatly reduced.

Erosion – removal and transportation of weathered
   and non-weathered materials by agents of erosion.
   Agents of Erosion:
   • running water
   • Wind
17.4 Weathering and Erosion

Erosion – removal and transportation of weathered
   and non-weathered materials by agents of erosion.
   Agents of Erosion:
   • running water
   • Wind
   • Waves
   • Ice
   • underground water
   • gravity.
17.4 Weathering and Erosion

   •   Ice
   •   underground water
   •   gravity.

Notes on Erosion:
  • Water erosion shapes Earth’s surface
  • Water is by far the most effective physical
      weathering agent.
17.4 Weathering and Erosion

Notes on Erosion:
  • Water erosion shapes Earth’s surface
  • Water is by far the most effective physical
      weathering agent.
  • Rivers carry sediments that scrapes and scratch
      rocks and soil in riverbanks and river bottom
  • Deposition – the process of depositing
      sediments on the floor of calmer portions of
      rivers, lakes and sea.
17.4 Weathering and Erosion

Notes on Erosion:
  • Rivers carry sediments that scrapes and scratch
      rocks and soil in riverbanks and river bottom
  • Deposition – the process of depositing
      sediments on the floor of calmer portions of
      rivers, lakes and sea.
  • Glaciers erode mountains
  • Wind also shape landscapes
17.4 Weathering and Erosion

 Poster: figure 17-35 on page 588

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2.3c weathering and erosion

  • 1. 17.4 Weathering and Erosion To do: • Class reading: page 583 – 588. • Individual Silent Work: Vocabulary starting page 583
  • 2. 17.4 Weathering and Erosion Weathering – The change in the physical form or chemical composition 0f rock materials exposed at Earth’s surface. Two types of the Weathering process: 1. Physical or mechanical – it is a kind of weathering that breaks rocks into smaller pieces but does not alter the rocks’ chemical composition.
  • 3. 17.4 Weathering and Erosion Two types of the Weathering process: 1. Physical or mechanical – it is a kind of weathering that breaks rocks into smaller pieces but does not alter the rocks’ chemical composition. a. Ice (frost wedging) – occurs when water seeps into cracks or joints in rocks and then freezes. When water freezes, its volume increase by about 10% pushing the rock apart.
  • 4. 17.4 Weathering and Erosion a. Ice (frost wedging) – occurs when water seeps into cracks or joints in rocks and then freezes. When water freezes, its volume increase by about 10% pushing the rock apart. b. Plants (plant wedging) – occurs when roots grow into cracks in the rocks. As the plant grows, the roots exert a constant pressure on the rock. The crack continues to deepen and widen, eventually causing a piece of the rock to break off.
  • 5. 17.4 Weathering and Erosion b. Plants (plant wedging) – occurs when roots grow into cracks in the rocks. As the plant grows, the roots exert a constant pressure on the rock. The crack continues to deepen and widen, eventually causing a piece of the rock to break off. 2. Chemical Weathering- kind of weathering that breaks down rocks by changing its chemical composition.
  • 6. 17.4 Weathering and Erosion 2. Chemical Weathering- kind of weathering that breaks down rocks by changing its chemical composition. a. Oxidation – When certain elements, specially metals, react with oxygen, they become oxides and their properties change.
  • 7. 17.4 Weathering and Erosion a. Oxidation – When certain elements, specially metals, react with oxygen, they become oxides and their properties change. - Oxidation in minerals causes minerals to decompose or form new minerals causing both chemical and physical appearance of the rock to change. b. Carbon dioxide – carbon dioxide in the air dissolves in rainwater resulting to a carbonic acid.
  • 8. 17.4 Weathering and Erosion b. Carbon dioxide – carbon dioxide in the air dissolves in rainwater resulting to a carbonic acid. - Although carbonic acid is a weak acid, it reacts with minerals, seeps into the ground and weather rocks underground. - Acid rain – slowly dissolves minerals caused burning fossil fuels in cars, power stations, factories
  • 9. 17.4 Weathering and Erosion - Although carbonic acid is a weak acid, it reacts with minerals, seeps into the ground and weather rocks underground. - Acid rain – slowly dissolves minerals caused burning fossil fuels in cars, power stations, factories. - Acid rain damages both living organisms and non-living matter.
  • 10. 17.4 Weathering and Erosion - Acid rain damages both living organisms and non-living matter. How does pollution contribute to acid rain? - Coal, oil and gasoline – release gases including sulfur dioxide reacting with water in the air and clouds to form nitric acid or nitrous acid and sulfuric acid.
  • 11. 17.4 Weathering and Erosion How does pollution contribute to acid rain? - Coal, oil and gasoline – release gases including sulfur dioxide reacting with water in the air and clouds to form nitric acid or nitrous acid and sulfuric acid. - US Act of 1970 (Clean Air Act) – reduced the release of chemicals that cause acid rains. Acidity of rain is greatly reduced.
  • 12. 17.4 Weathering and Erosion - US Act of 1970 (Clean Air Act) – reduced the release of chemicals that cause acid rains. Acidity of rain is greatly reduced. Erosion – removal and transportation of weathered and non-weathered materials by agents of erosion. Agents of Erosion: • running water • Wind
  • 13. 17.4 Weathering and Erosion Erosion – removal and transportation of weathered and non-weathered materials by agents of erosion. Agents of Erosion: • running water • Wind • Waves • Ice • underground water • gravity.
  • 14. 17.4 Weathering and Erosion • Ice • underground water • gravity. Notes on Erosion: • Water erosion shapes Earth’s surface • Water is by far the most effective physical weathering agent.
  • 15. 17.4 Weathering and Erosion Notes on Erosion: • Water erosion shapes Earth’s surface • Water is by far the most effective physical weathering agent. • Rivers carry sediments that scrapes and scratch rocks and soil in riverbanks and river bottom • Deposition – the process of depositing sediments on the floor of calmer portions of rivers, lakes and sea.
  • 16. 17.4 Weathering and Erosion Notes on Erosion: • Rivers carry sediments that scrapes and scratch rocks and soil in riverbanks and river bottom • Deposition – the process of depositing sediments on the floor of calmer portions of rivers, lakes and sea. • Glaciers erode mountains • Wind also shape landscapes
  • 17. 17.4 Weathering and Erosion Poster: figure 17-35 on page 588