Earth: An Introduction to Physical Geology (12th Edition)

Published by Pearson
ISBN 10: 0134074254
ISBN 13: 978-0-13407-425-2

Chapter 7 - Section 7.1 - An Introduction to Sedimentary Rocks - Concept Checks - Page 214: 3

Answer

To transform an exposure of granite in the mountains into various sedimentary rocks, several steps are involved. Here is an outline of the general processes and steps that would take place: 1. Weathering: The first step is the weathering of the exposed granite. Weathering can occur through physical, chemical, or biological processes. Physical weathering includes the breakdown of rocks into smaller fragments through mechanical forces like temperature changes, frost action, and abrasion. Chemical weathering involves the chemical alteration of minerals in the granite due to interactions with water, oxygen, and other substances. Biological weathering occurs through the actions of plants, animals, and microorganisms that can contribute to rock fragmentation. 2. Erosion and Transport: Once the granite is weathered, the resulting fragments and particles are then subjected to erosion. Erosion refers to the removal and transportation of the weathered material by various agents such as water, wind, ice, or gravity. Water, in the form of rivers, streams, or rainfall, is often the primary agent responsible for transporting sediment. The eroded particles are carried away from the source area and transported to new locations. 3. Deposition: After being transported, the eroded sediment undergoes deposition. Deposition occurs when the transporting agent loses energy and is no longer capable of carrying the sediment. As a result, the sediment settles and is deposited in basins, river deltas, lakes, or ocean floors. The deposition process can lead to the formation of layers or beds of sediment, known as stratification, as the sediment accumulates over time. 4. Lithification: Once deposited, the sediment undergoes lithification, which involves compaction and cementation. Compaction occurs when the weight of the overlying sediment compresses the lower layers, reducing pore space and causing the particles to become more tightly packed. Cementation refers to the precipitation and deposition of minerals in the pore spaces, binding the sediment particles together and forming solid rock. 5. Diagenesis: Diagenesis refers to the changes that occur within the sedimentary rock after lithification. These changes include further compaction, recrystallization of minerals, and the formation of new minerals. Diagenesis may also involve the introduction of fluids, such as groundwater, which can dissolve and transport minerals and precipitate new ones, contributing to the transformation of the sedimentary rock. 6. Burial and Metamorphism (optional): In some cases, if the sedimentary rocks undergo burial under increased heat and pressure, they may undergo metamorphism. Metamorphism involves the transformation of the rock through recrystallization and the growth of new minerals, resulting in the formation of metamorphic rocks. However, this step is optional and depends on the specific geological conditions. Overall, the transformation of granite into various sedimentary rocks involves weathering, erosion, transportation, deposition, lithification, and potentially diagenesis and metamorphism. These processes take place over a long period, driven by geological forces and environmental conditions.

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