Thermal Expansion
Thermal expansion refers to the tendency of materials to increase in size or volume as their temperature rises. This phenomenon occurs because heat energy causes the atoms or molecules within a substance to move more vigorously, leading to increased spacing between them. As the particles move more, they push against each other and the material expands.
Mechanical Weathering
Mechanical Weathering, also known as Physical Weathering, is nature’s way of breaking rocks into smaller pieces. Imagine it as rock transformation through a series of natural actions. Factors like temperature, plants, and the rocks themselves play key roles in this process. Temperature takes center stage, causing rocks to expand and contract, slowly breaking them down over time. Plants contribute by sending their roots into rock crevices, applying pressure that eventually leads to rock crumbles. Even rocks, seemingly solid, yield to the wear and tear from wind-blown sand or the relentless force of waves along coastlines.
In this article we’ll discuss about Mechanical Weathering, Its Types, Factors, Process and so on. To know more, Stay Tuned!
Table of Content
- Mechanical Weathering
- What Is Mechanical Weathering?
- How Mechanical Weathering Works?
- Types Of Mechanical Weathering Process
- Stages Of Mechanical Weathering
- Factors Affecting Mechanical Weathering
- Freeze-Thaw Weathering Or Frost Wedging
- Exfoliation Weathering
- Thermal Expansion
- Abrasion Weathering
- Salt Weathering Or Haloclasty
- Difference Between Mechanical Weathering And Chemical Weathering
- Difference Between Mechanical Weathering And Physical Weathering
- Difference Between Mechanical Weathering And Biological Weathering