introtoweathering
DESCRIPTION
Introductory lecture to weathering for AS/A2 GeographyTRANSCRIPT
![Page 1: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/1.jpg)
The Wonderful World of
Rock WeatheringMdm Masayu Mahmud
Department of HumanitiesInnova Junior College,
Singapore
![Page 2: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/2.jpg)
What geologic processes causes these rocks to weather?
![Page 3: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/3.jpg)
Dairy Farm Estate Granite Outcrop, Singapore
![Page 4: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/4.jpg)
Describe this landform
![Page 5: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/5.jpg)
Denudation
Includes all processes of wearing down of the rocks on the earth’s surface and their removal resulting in the lowering of the land surface.Major processes.1. Weathering.
2. Mass movement/mass wasting. 3. Erosion. 4. Transportation. 5. Deposition
![Page 6: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/6.jpg)
Weathering
Weathering refers to the process of disintegration (physical breakdown) and decomposition (chemical decay) of rock in situ at or near the earth’s surface by climatic or biological elements.
![Page 7: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/7.jpg)
Erosion
Erosion refers to the wearing away of weathered rock material by agents such as running water (rivers), tornadoes, mudflows, moving ice (glaciers), waves and wind.Movement of loose rock material involved.
![Page 8: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/8.jpg)
![Page 9: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/9.jpg)
Why Do Rocks Weather?
Formed at depthUnder pressureNo exposure to oxygen, carbon dioxide,water, temperature changesComposition of rocks – reaction?Weathering as a response to atmospheric and surface conditions?Slow process
![Page 10: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/10.jpg)
Types of Weathering
Physical (Mechanical)
Chemical
Biological
![Page 11: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/11.jpg)
Mechanical Weathering( MW)
Disintegration of rock into smaller particles by mechanical processes but without any change in the chemical composition of the rockWhere is it likely to occur?- devoid of vegetation
- deserts, high mountains, arctic regionsEnd product- sands
![Page 12: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/12.jpg)
Chemical Weathering(CW)
Decomposition of rock resulting from chemical changeVarious components of rock – iron, mica, feldspar, calcium carbonate reacting with water, acids, heat etcDominant Location- warmer climates with vegetationEnd product- clay
![Page 13: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/13.jpg)
Biological Weathering(BW)
Physical or chemical breakdown of rocks due to action of plants, trees, animals,algae, bacteria etc.
Root pry, animals burrowing, humic acids reacting with rock.
![Page 14: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/14.jpg)
Products of Weathering
Type of weathering
Product of weathering and erosion
Type of sediment ultimately deposited
Mechanical weathering
Fragments containing the same minerals as the original rock (e.g. grains of quartz from a granite) Clastic sediments and
sedimentary rocks (e.g. sand and sandstone)
Chemical weathering
New solid mineral particles formed by chemical reactions during weathering (e.g. Clay minerals)
Material dissolved in water (e.g. Calcium ions)
Chemical and biological sediments (e.g. limestone and rock salt)
![Page 15: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/15.jpg)
A Point to Note
Different types of weathering
- dominant in certain regions
- DO NOT occur in isolation
![Page 16: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/16.jpg)
Factors Influencing Rate of Weathering
1. Climatic factor2. Rock Types3. Relief/
Topography/Slope4. Vegetation5. Impact of human
activities
![Page 17: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/17.jpg)
1. Climatic Factor
Main influences- air temperature, humidity and rainfallCW dominant in hotter, wetter climatesHydrolysis, oxidation and solution common in equatorial regionsMW dominant in regions with extreme temperature fluctuations- Which ones?Deserts, Temperate regions and mountainous areas
![Page 18: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/18.jpg)
2. Rock Types
Refers to
1. Chemical composition (constituents minerals) –determines resistance
2. physical structure
3. Presence of joints
4. Bedding planes
5. Permeability of rocks
![Page 19: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/19.jpg)
Jointed Structures
![Page 20: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/20.jpg)
Hard Rock Not?
Rocks composed of cemented particles less resistant compared to?
Rocks consisting of mainly carbonates?
Rocks of massive structure vs bedded structures
Presence of joints (naturally occurring cracks in rocks), cracks, fissures?
![Page 21: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/21.jpg)
Jointing in Granite
![Page 22: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/22.jpg)
![Page 23: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/23.jpg)
3. Relief, Topography and Slope
Aspect- slopes exposed to wind, rain and heat vs. sheltered slope
- Slopes facing sun in high altitudes vs. cold and sunless slopesSlope
- high, steep slopes lead to down slope washing and prone to runoff and erosion of materialsElevation- Higher elevation > opportunity for water movement
- Flat terrain; slow removal of weathered material. Why? How does this affect weathering rates?
![Page 24: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/24.jpg)
4. Effect of Vegetation
Dense vegetation- retains more water; aids CW
Decaying vegetation provides moisture and humic acids- aids CW
Roots of trees and plants pry rocks and joints- increase MW
![Page 25: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/25.jpg)
5. Impact of human activities
Expose the rocks and accelerate weathering
1. Clearing forests
2. Road construction
3. Industrial development
4. Mining/quarrying
5. Trampling
![Page 26: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/26.jpg)
Results of Weathering Processes
Joint blocks
Boulder fields
Exfoliated Rocks
Spheroidal boulders
Sand
Clay
Laterite
![Page 27: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/27.jpg)
Boulder fields
![Page 28: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/28.jpg)
Exfoliated Rocks and Spheroidal Boulders
![Page 29: Introtoweathering](https://reader035.vdocuments.mx/reader035/viewer/2022070316/555881fcd8b42a5d328b4bee/html5/thumbnails/29.jpg)
Lateritic Soil
A Laterite soil cross section in Brazil. The deep red color is due to Fe3+ hydroxide minerals in the soil.