This document discusses weathering and erosion. It defines weathering as the breakdown of rocks into smaller pieces through physical or chemical processes. Physical weathering breaks rocks down mechanically through processes like frost wedging or plant roots. Chemical weathering uses chemical agents like water, oxygen, carbon dioxide and acids to break rocks down chemically over time. One example of chemical weathering discussed is how carbon dioxide dissolves in water to form carbonic acid, which easily weathers limestone. The document also defines erosion as the movement of rock and soil by agents such as water, ice, wind or gravity. Specific types of erosion mentioned include water erosion through rivers/streams and runoff, ice erosion through glaciers, and wind erosion
4. Physical Weathering
• Process by which rocks are broken down
into smaller pieces by external conditions.
• Types of Physical weathering
– Frost heaving and Frost wedging
– Plant roots
– Friction and impact
– Burrowing of animals
– Temperature changes
11. Chemical Weathering
• The process that breaks down rock
through chemical changes.
• The agents of chemical weathering
– Water
– Oxygen
– Carbon dioxide
– Living organisms
– Acid rain
16. Acid Rain
• Compounds from burning coal, oil and gas
react chemically with water forming acids.
• Acid rain causes very rapid chemical
weathering
17. Karst Topography
• A type of landscape in rainy regions where
there is limestone near the surface,
characterized by caves, sinkholes, and
disappearing streams.
• Created by chemical weathering of
limestone
24. Learning Targets
I can:
-define erosion.
-enumerate the different agents of erosion.
-discuss how erosion happens.
-differentiate erosion from weathering
25. Erosion
• The process by which water, ice, wind or
gravity moves fragments of rock and soil.