Describe weathering processes operating on an open expanse of bedrock. How does regolith develop? How is sediment derived?

Short Answer

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Weathering processes on bedrock mainly include physical and chemical weathering. Regolith develops as an outcome of the weathering of bedrock and comprises dust, soil, and broken-down rock. Sediment is derived from weathered and eroded material that has been transported and deposited.

Step by step solution

01

Identification of Weathering Processes

There are several weathering processes that operate on an open expanse of bedrock. The major ones include physical weathering and chemical weathering. Under physical (or mechanical) weathering, we have freeze-thaw (where water gets into rock cracks, freezes and expands, thus breaking the rock), salt crystal growth, and biological activity (roots of plants breaking rocks). In chemical weathering, we have processes such as oxidation, hydration and carbonation where rocks are broken down through reactions with substances in the environment.
02

Understanding the Development of Regolith

Regolith is a layer of loose, heterogeneous material covering solid rock. It includes dust, soil, broken rock, and other related materials and is present on Earth, the Moon, Mars, some asteroids, and other terrestrial planets and moons. This layer forms as a result of the weathering of bedrock, with the accumulation and breaking down of materials through erosion, transportation, and deposition.
03

Explaining the Derivation of Sediment

Sediment is typically derived from the process of weathering and erosion. As rock breaks down, the resultant material is transported by agents of erosion such as water, wind or ice. This transported material, when deposited, is known as sediment. Sediment can further be transported and deposited across different landscape elements, contributing to landform development and dynamics.

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