AChemical
BBiochemical
COrganic
DMechanical
Answer:
D. Mechanical
Read Explanation:
Sedimentary Rocks Classification
Mechanical Sedimentary Rocks (Clastic Rocks)
These rocks are formed from the accumulation and cementation of mineral and rock fragments (clasts) that have been weathered and eroded from pre-existing rocks.
The fragments are transported by wind, water, or ice and deposited in layers.
Sandstone is a prime example, composed primarily of sand-sized mineral grains or rock fragments, most commonly quartz. It forms from the lithification of sand.
Shale is another key example, formed from compacted clay-rich or silty sediment. It is characterized by its fine grain size and fissility (tendency to split into thin layers).
Other examples of mechanical sedimentary rocks include conglomerate (rounded pebbles), breccia (angular fragments), and siltstone (silt-sized grains).
Formation Process
Weathering: The breakdown of existing rocks into smaller pieces.
Erosion: The transport of these fragments by natural agents.
Deposition: The settling and accumulation of transported sediments.
Compaction: The weight of overlying sediments reduces pore space.
Cementation: Minerals dissolved in groundwater precipitate in the pore spaces, binding the sediments together into solid rock. Common cementing agents include silica, calcite, and iron oxides.
