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Questions and Answers
What are the two types of weathering?
What are the two types of weathering?
Mechanical weathering and chemical weathering.
What is weathering?
What is weathering?
Weathering is the process of breaking down rocks into smaller particles like sand, clay, and gravel.
What are the agents of erosion?
What are the agents of erosion?
Water, wind, and glaciers.
What is erosion?
What is erosion?
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What are exogenic processes?
What are exogenic processes?
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What are some examples of mechanical weathering?
What are some examples of mechanical weathering?
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How does pressure contribute to mechanical weathering?
How does pressure contribute to mechanical weathering?
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How does temperature contribute to mechanical weathering?
How does temperature contribute to mechanical weathering?
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What is frost wedging?
What is frost wedging?
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How do plants contribute to mechanical weathering?
How do plants contribute to mechanical weathering?
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How do burrowing animals contribute to mechanical weathering?
How do burrowing animals contribute to mechanical weathering?
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What is chemical weathering?
What is chemical weathering?
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What is dissolution?
What is dissolution?
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What are some examples of minerals that are dissolved in water?
What are some examples of minerals that are dissolved in water?
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What is hydrolysis?
What is hydrolysis?
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What is oxidation?
What is oxidation?
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What is mass wasting?
What is mass wasting?
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What are some examples of mass wasting?
What are some examples of mass wasting?
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Erosion is a natural process that can be harmful to the environment.
Erosion is a natural process that can be harmful to the environment.
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How do animals contribute to erosion?
How do animals contribute to erosion?
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How do human activities affect the rate of erosion?
How do human activities affect the rate of erosion?
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Study Notes
Exogenic Processes
- Exogenic processes are the processes that shape Earth's surface.
- These processes include weathering and erosion.
- Weathering breaks down rocks into smaller pieces.
- Erosion carries away the weathered materials.
- Weathering and erosion are important for soil formation.
Learning Objectives
- Students will learn how rocks weather.
- Students will identify factors that cause erosion.
- Students will explain how the eroded materials are deposited.
Introduction
- Earth's surface is made up of water and landmasses.
- Rocks and minerals on the solid portion can undergo physical or chemical changes.
- Weathered materials are transported by factors like water, wind and ice.
- These progressions are called exogenic processes.
Weathering
- Weathering is the process of breaking down rocks into smaller particles.
- Two types of weathering are mechanical and chemical.
Mechanical Weathering
- Mechanical weathering breaks down rocks into smaller pieces without changing the composition.
- Causes include pressure, temperature changes (like frost wedging), abrasion, organic activities (roots), and human activities (digging, quarrying).
Pressure (Mechanical Weathering)
- Tectonic forces can lift rocks to high elevations.
- As the overlying rocks erode, pressure decreases.
- The decreasing pressure causes rock expansion.
- This can cause cracks and eventual breaking.
Temperature (Mechanical Weathering)
- Rocks expand when heated and contract when cooled.
- Repeated heating and cooling can weaken rocks, fracturing them.
- Frost wedging: Water seeps into cracks and freezes, expanding the crack, eventually breaking the rock.
Abrasion (Mechanical Weathering)
- Rocks collide with each other, wearing away edges.
- This occurs due to flowing water, wind, or waves.
- The rocks, sand, and silt result in sharp edges becoming rounded.
Organic Activities (Mechanical Weathering)
- Plant roots grow into cracks, widening them.
- The roots can push apart the rock by expanding as they grow.
Human Activities (Mechanical Weathering)
- Activities like digging, quarrying, or forest clearing can contribute to mechanical weathering.
Burrowing Animals (Mechanical Weathering)
- Animals like rats, rabbits, and squirrels make burrows, widening cracks and breaking rocks apart.
Chemical Weathering
- Chemical weathering changes the composition of rocks through chemical reactions.
- Dissolution, hydrolysis, and oxidation are examples.
Dissolution (Chemical Weathering)
- Minerals like Halite(NaCl) and Calcite (CaCO3) dissolve in water.
- Examples include caves formations (stalactites and stalagmites).
Hydrolysis (Chemical Weathering)
- Rock-forming minerals like amphibole, pyroxene, and feldspar react with water.
- The reactions change the composition of the minerals, eventually dissolving them into clay minerals.
Oxidation (Chemical Weathering)
- Oxygen reacts with minerals, altering their composition.
- Iron oxidation (rusting) is a common example.
- The reaction weakens the rock and causes decomposition.
Weathering (General Considerations)
- Weathering is crucial to soil formation.
- Soil is a mixture of grains, organic matter, water, and gases.
- Plants, animals, and humans also play roles in the process of erosion.
Erosion
- Erosion is the process of removing and transporting weathered materials.
- Water, wind, and glaciers are the primary agents.
Mass Wasting
- Mass wasting is the downslope movement of sediments under gravity.
- Common forms include falls, slides, avalanches, and flows.
Deposition
- Deposition is the process where eroded materials settle in new locations.
- It results in the creation of new landforms.
- Alluvial fans are an example of a resulting deposition feature.
Reflect Upon
- The presentation raises questions about animal and human impacts on erosion and the effects of soil erosion on communities.
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Description
Explore the concepts of exogenic processes that shape Earth's surface. This quiz covers the mechanisms of weathering and erosion, and their roles in soil formation. Understand how weathered materials are transported and deposited by natural forces.