1. Weathering breaks down materials on or near Earth’s surface.
Section 1: Weathering
Weathering breaks down materials on or near Earth’s surface. K
What I Know W
What I Want to Find Out L
What I Learned

2. Essential Questions How do mechanical and chemical weathering differ?
What are the different factors that affect mechanical and chemical weathering?
What variables affect the rate of weathering?
Weathering
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3. Vocabulary Review New acid weathering mechanical weathering
frost wedging
exfoliation
chemical weathering
oxidation
Weathering
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4. Mechanical Weathering
Weathering is the process in which materials on or near Earth’s surface break down and change.
Mechanical weathering is a type of weathering in which rocks and minerals break down into smaller pieces. It does not change a rock’s composition.
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Weathering

5. Mechanical Weathering
Effect of temperature
When water freezes, it increases in volume. If the temperature drops to the freezing point, water that has collected in the cracks of rocks or rock layers freezes, expands, and exerts pressure on the rocks, which can cause the cracks to widen slightly.
When the temperature increases, ice melts in the cracks of rocks and rock layers. The freeze-thaw cycles of water in the cracks of rocks is called frost wedging.
Weathering
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6. Add link to Animation from p. 164 here.
Ice Wedging
Concepts In Motion
FPO
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Weathering
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7. Mechanical Weathering
Effect of pressure
On a small scale, plant or tree roots wedged in the cracks of rocks exert pressure as they grow and expand, which often causes the rocks to split.
On a larger scale, when overlying rock layers are removed by processes such as erosion or even mining, the pressure on the bedrock is reduced. The bedrock surface that was buried expands, and long, curved cracks can form.
Weathering
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8. Mechanical Weathering
Effect of pressure
Exfoliation is a mechanical weathering process in which outer rock layers are stripped away, often resulting in dome-shaped formations.
Weathering
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9. Chemical Weathering
Chemical weathering is the process by which rocks and minerals undergo changes in their composition.
Agents of chemical weathering include water, oxygen, carbon dioxide, and acid precipitation
Weathering
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10. Chemical Weathering
The composition of a rock determines the effects that chemical weathering will have on it.
Temperature is a significant factor in chemical weathering because it influences the rate at which chemical reactions occur.
Weathering
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11. Chemical Weathering Effect of water
Water is an important agent in chemical weathering because it can dissolve many kinds of minerals and rocks. Water serves as a medium in which chemical reactions can occur, and it can also react directly with minerals in a chemical reaction.
Weathering
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12. Chemical Weathering Effect of oxygen
The chemical reaction of oxygen with other substances is called oxidation.
Iron in rocks and minerals combines with oxygen to form minerals with the oxidized form of iron. Hematite is a common example.
Weathering
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13. Chemical Weathering Effect of carbon dioxide
When carbon dioxide combines with water in the atmosphere, it forms a very weak acid called carbonic acid that falls to Earth’s surface as precipitation. The slight acidity of precipitation can cause it to dissolve certain rocks, such as limestone.
When slightly acidic water from precipitation seeps into the ground, it combines with carbon dioxide in the soil, and becomes a stronger acid. Carbonic acid slowly reacts with minerals such as calcite in limestone to dissolve rocks.
Weathering
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14. Chemical Weathering Effect of acid precipitation
Sulfur dioxide, carbon dioxide, and nitrogen oxides are released into the atmosphere by human activities. When these gases combine with water and oxygen in the atmosphere, sulfuric, carbonic, and nitric acids form and cause acid precipitation.
Weathering
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15. Chemical Weathering Effect of acid precipitation
Because strong acids can be harmful to many organisms and destructive to human-made structures, acid precipitation often creates problems, such as making forests more vulnerable to disease.
Weathering
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16. Rate of Weathering
The natural weathering of Earth materials occurs slowly. However, certain conditions and interactions can accelerate or slow the weathering process.
Weathering
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17. Rate of Weathering Effects of climate on weathering
The interaction between temperature and precipitation in a given climate determines the rate of weathering in a region.
Weathering
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18. Rate of Weathering Rates of chemical weathering
Warm, lush areas such as the tropics experience the fastest chemical weathering.
Weathering
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19. Rate of Weathering Rates of physical weathering
Physical weathering can break down rocks more rapidly in cool climates. Conditions in such climates do not favor chemical weathering because cool temperatures slow or inhibit chemical reactions.
Weathering
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20. Rate of Weathering Rock type and composition
Not all the rocks in the same climate weather at the same rate. The effects of climate on the weathering of rock also depend on the rock type and composition.
Weathering
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21. Rate of Weathering Surface area
Mechanical weathering breaks rocks into smaller pieces. As the pieces get smaller, their surface area increases, resulting in more total surface area available for chemical weathering.
Weathering
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22. Rate of Weathering Topography
The slope of a landscape helps determine the rate of weathering. Steep slopes promote erosion and continually expose more rocks to weathering.
Weathering
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23. Add link to Animation from ConnectED here.
Weathering
BrainPOP
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Add link to Animation from ConnectED here.
Weathering
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24. Review Essential Questions Vocabulary
How do mechanical and chemical weathering differ?
What are the different factors that affect mechanical and chemical weathering?
What variables affect the rate of weathering?
Vocabulary
weathering
mechanical weathering
frost wedging
exfoliation
chemical weathering
oxidation
Weathering
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