Name:
Weathering and Soil Formation
Rocks and Weathering
1. The Effects of Weathering
· Weathering is the process that breaks down rocks at Earth’s surface.
· Heat, cold, water, ice, oxygen and carbon dioxide in the atmosphere all contribute to weathering.
· Erosion is the movement of rock particles by wind, water, ice or gravity.
· Weathering and erosion work together.
· Two kinds of weathering: Mechanical & Chemical
2. Mechanical Weathering
· Weathering in which rock is physically broken into smaller pieces
· Rock is broken by freezing and thawing, release of pressure, growth of plants, and actions of animals
· Abrasion: the grinding away of rock by particles carried by water, ice, wind or gravity.
· Ice wedging – ice acts like a wedge to break rocks apart
3. Chemical Weathering
· Breaks down rocks through chemical change
· Agents of Chemical Weathering: Water, oxygen, carbon dioxide, living organisms and acid rain
· Chemical weathering creates holes or soft spots in rock, so the rock breaks apart more easily
A. Water
· Most important agent
· Water dissolves rock
B. Oxygen
· Rock that contains iron oxidizes or rusts
C. Carbon Dioxide
· Carbon Dioxide is dissolved in rainwater and in water that sinks through air pockets in the soil.
· Carbonic acid weathers limestone and marble easily
D. Living Organisms
· Seeds grow on rocks
· Lichens also produce weak acids that weather rocks
E. Acid Rain
· Burning fuels can pollute the air
· The result is acid rain that contributes to chemical weathering
4. Rate of Weathering
· The most important factors that determine the rate of weathering are type of rock and climate.
A. Type of Rock
· The minerals that make up a rock determine the rate of weathering
· Some rock weathers easily because it is permeable or has tiny air spaces
B. Climate
· The average weather conditions in an area
· Chemical and Mechanical weathering occurs faster in wet and hot weather