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Cycle of Erosion : Complete Notes

The cycle of erosion is a natural process that occurs in the earth’s crust, which involves the gradual breakdown and reshaping of the land. This process has been ongoing for millions of years and is responsible for the formation of the world’s major landforms such as mountains, valleys, canyons, and plains. The cycle of erosion is a complex and continuous process that involves several stages, each of which plays an essential role in shaping the earth’s surface. In this article, we will take a closer look at the cycle of erosion and its different stages.

Cycle of Erosion
Cycle of Erosion

What is the cycle of erosion?

It is a natural process that involves the breakdown and reshaping of the earth’s surface. This process occurs due to several natural factors such as wind, water, ice, and gravity, which contribute to the erosion of the land. The cycle of erosion is a continuous process, and it involves four main stages, which are:

Stage 1: Weathering

Weathering is the first stage of the cycle of erosion, and it involves the breakdown of rocks and minerals on the earth’s surface. This process occurs due to several natural factors such as wind, water, ice, and temperature changes. Weathering can occur through several mechanisms such as physical, chemical, and biological weathering. Physical weathering occurs when rocks are broken down due to physical forces such as wind, water, and ice. Chemical weathering occurs when rocks are broken down due to chemical reactions such as oxidation and carbonation. Biological weathering occurs when rocks are broken down due to the actions of living organisms such as plant roots and burrowing animals.

Stage 2: Transportation

Transportation is the second stage of the cycle, and it involves the movement of weathered materials from their place of origin to another location. Transportation occurs due to several natural factors such as wind, water, ice, and gravity. The mechanism of transportation varies depending on the type of material being transported. For example, wind can transport small particles such as sand and dust, while water can transport larger particles such as rocks and boulders.

Stage 3: Deposition

The deposition is the third stage of the cycle, and it involves the settling of transported materials in a new location. Deposition occurs when the velocity of the transporting medium decreases, and it can occur in several locations such as rivers, oceans, and lakes. The materials that are deposited can vary in size and composition depending on the type of transportation mechanism.

Stage 4: Uplift

Uplift is the fourth and final stage of the cycle, and it involves the gradual rise of the earth’s crust due to tectonic activity. Uplift can occur due to several factors such as volcanic activity, plate tectonics, and geological folding. When the earth’s crust is uplifted, the materials that were deposited during the deposition stage are exposed to weathering and erosion once again, and the cycle of erosion begins anew.

Conclusion

The cycle of erosion is a natural process that has been ongoing for millions of years, and it plays an essential role in shaping the earth’s surface. The cycle of erosion involves four main stages, which are weathering, transportation, deposition, and uplift. Each of these stages is important in reshaping the land and creating the world’s major landforms such as mountains, valleys, canyons, and plains. Understanding this is crucial for geologists and environmental scientists who study the earth’s surface and its evolution over time.

The cycle of Erosion : Summary

  • The cycle of erosion is a natural process that involves the gradual breakdown and reshaping of the land.
  • It occurs due to natural factors such as wind, water, ice, and gravity.
  • The cycle of erosion involves four stages: weathering, transportation, deposition, and uplift.
  • Weathering is the breakdown of rocks and minerals on the earth’s surface.
  • Transportation is the movement of weathered materials from their place of origin to another location.
  • The deposition is the settling of transported materials in a new location.
  • Uplift is the gradual rise of the earth’s crust due to tectonic activity.
  • The cycle of erosion plays an essential role in shaping the earth’s surface and creating major landforms such as mountains, valleys, canyons, and plains.
  • Understanding the cycle of erosion is crucial for geologists and environmental scientists who study the earth’s surface and its evolution over time.

The cycle of Erosion: MCQ

Q. Which of the following is the first stage of the cycle of erosion?
A. Transportation
B. Deposition
C. Uplift
D. Weathering
Answer: D. Weathering is the first stage of the cycle of erosion. It involves the breakdown of rocks and minerals on the earth’s surface.

Q. What is the mechanism of transportation for the wind?
A. Carrying small particles such as sand and dust
B. Carrying larger particles such as rocks and boulders
C. Flowing downhill in rivers
D. Carrying materials in suspension and traction
Answer: A. Wind can transport small particles such as sand and dust.

Q. What is the process involved in chemical weathering?
A. Breaking down rocks due to physical forces such as wind and water
B. Breaking down rocks due to chemical reactions such as oxidation and carbonation
C. Breaking down rocks due to the actions of living organisms
D. None of the above
Answer: B. Chemical weathering occurs when rocks are broken down due to chemical reactions such as oxidation and carbonation.

Q. What is the final stage of the cycle of erosion?
A. Weathering
B. Transportation
C. Deposition
D. Uplift
Answer: D. Uplift is the final stage of the cycle of erosion. It involves the gradual rise of the earth’s crust due to tectonic activity.

Q. What is the role of the cycle of erosion?
A. To create new landforms such as mountains and valleys
B. To transport materials from one location to another
C. To cause destruction and erosion of the earth’s surface
D. All of the above
Answer: A. The cycle of erosion plays a crucial role in shaping the earth’s surface and creating new landforms such as mountains and valleys.

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