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Soils, Weathering, and Erosion

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Title: Mapping the earth Author: UNC Last modified by: Coble Created Date: 1/24/2010 4:19:26 PM Document presentation format: On-screen Show (4:3) Company – PowerPoint PPT presentation

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Title: Soils, Weathering, and Erosion


1
Soils, Weathering, and Erosion
  • Where the geosphere and the biosphere meet

2
Learning Targets
  1. Define mechanical and chemical weathering
  2. Discuss agents of weathering
  3. Give examples of each type of weathering

3
Soil Forming Processes
  1. Weathering process that changes solid rock into
    sediments
  2. Erosion process that moves sediments
  3. Sedimentation depositing of rock pieces

4
Weathering
5
Erosion
6
Sedimentation
7
Weathering
  • Large rocks and mountains ? sediment
  • Sediment sizes
  • Boulders
  • Gravel
  • Sand
  • Silt
  • Clay
  • What processes act on weathered sediments?
  • Erosion (movement)
  • Sedimentation (deposition)

8
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9
Weathering
  • Weathering only happens at the surface
  • Occurs in 2 forms
  • Mechanical change in shape or size
  • Also known as physical weathering
  • Chemical change in composition

10
Mechanical Weathering (Physical Weathering)
11
Chemical weathering
12
Mechanical Weathering (Physical Weathering)
  • 3 main types
  • Ice wedging
  • Cycles of freezing and thawing
  • Abrasion
  • Physical contact and friction
  • Biological weathering
  • Roots, burrowing animals, fungi, lichens, humans

13
Ice wedging
14
Abrasion
15
Biological weathering
16
Mechanical Weathering
  • Increases surface area
  • Increased surface area leads to quicker
    weathering. Why?
  • More rock is exposed to the atmosphere less rock
    is protected from water and oxygen

17
Increasing surface area
18
Chemical weathering
  • Creates new minerals or compounds
  • Different composition not just different size
  • Different minerals are stable at surface than at
    depth
  • Mainly caused by
  • Water dissolves minerals
  • Oxygen combines to form oxides
  • Carbon Dioxide makes water acidic

19
Oxidation
20
Hydrated obsidian
21
Oxidized ultramafic rock
22
Rust chemical weathering of Iron
23
Chemical Weathering
  1. Some organisms release chemicals that break down
    rocks and minerals
  2. Fungi and bacteria are very important parts of
    chemical weathering

24
Lichens colonizing a lava flow
25
Differential weathering
  • Weather rates speed up based on
  • Rock and Mineral Type
  • Sedimentary rocks weather fastest
  • Climate type
  • Temperature increases Chemical reactions more
    rapid
  • Precipitation increases More water allows more
    chemical reactions
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