weathering
Weathering and Its Processes
Definition of Weathering:
Weathering is the collective term for the physical and chemical processes that occur at the Earth's surface, resulting in the breakdown of rocks.
The end products are sediments, which are materials used to create sedimentary rocks.
Sediments:
Comprise rock or mineral fragments and altered minerals such as clays and oxides, as well as elements in solution.
Erosion:
After rocks are weathered and broken down into sediments, these sediments are eroded, meaning they are removed from their source.
Agents of Transport:
Wind
Water
Ice
Gravity
Deposition:
Sediment fragments accumulate in various environments within sedimentary basins.
In the depositional environment, elements in solution can transform back into solid sediments through:
Chemical means
Biochemical means
Lithification:
The process by which buried sediments are converted into rock.
Consists of two main processes:
Compaction: The reduction of the volume of sediment due to pressure over time.
Cementation: The binding together of sediments by minerals precipitating from water that occurs between the sediment grains.
Categories of Sedimentary Rocks:
Based on the origins of the sediments, sedimentary rocks are classified as:
Detrital: Formed from the mechanical weathering debris.
Biochemical: Comprised of organic material and/or minerals precipitated from solution by biological processes.
Crystalline Chemical: Formed from the precipitation of minerals from solution.