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Weathering and Erosion

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Presentation on theme: "Weathering and Erosion"— Presentation transcript:

1 Weathering and Erosion

2 Weathering The breakdown of Earth’s crust into smaller pieces.

3 Mechanical (Physical) Weathering
Process by which rocks are broken down into smaller pieces by external conditions. Types of Mechanical weathering Frost heaving and Frost wedging Plant roots Impact of wind and water Abrasion Burrowing of animals Temperature changes

4 Frost Wedging

5 Frost Heaving

6 Plant Roots

7 Friction and Repeated Impact

8 Burrowing of Animals

9 Temperature Changes

10 Chemical Weathering The process that breaks down rock through chemical changes. The agents of chemical weathering Water Oxygen Living organisms Acid Rain Carbon Dioxide

11 Water Water weathers rock by dissolving it

12 Oxygen Iron combines with oxygen in the presence of water in a processes called oxidation The product of oxidation is rust

13 Living Organisms Lichens that grow on rocks produce weak acids that chemically weather rock

14 Acid Rain Compounds from burning coal, oil and gas react chemically with water forming acids. Acid rain causes very rapid chemical weathering

15 Carbon Dioxide CO2 dissolves in rain water and creates carbonic acid
Carbonic acid easily weathers limestone and marble

16 Karst Topography Karst is created by chemical weathering of limestone
A type of landscape in rainy regions where there is limestone near the surface, characterized by caves, sinkholes, and disappearing streams.

17 Features of Karst: Sinkholes

18 Features of Karst: Caves

19 Features of Karst: Disappearing Streams

20

21 Erosion The process by which water, ice, wind or gravity moves fragments of rock and soil.

22 Water Erosion Rivers, streams, and runoff

23 Ice Erosion Glaciers

24 Wind Erosion

25 Mass Movements Landslides, mudslides, slump and creep
landslide clip.mpeg

26

27 What have you learned? What is erosion?
2. How are weathering and erosion connected? Give 2 examples of weathering. 3. 4. Give 2 examples of erosion. 5. 6.


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