The type of plant that grew near a river. Apex.
The sediment composition in a clastic rock is determined by factors such as the rock's source material, transportation process, and depositional environment. It is not determined by the age of the rock formation.
Sediment size alone is not enough to classify clastic rock because other factors such as mineral composition, sorting, and rounding of the sediment particles also play a significant role in the classification of clastic rocks. These additional factors provide more detailed information about the rock formation processes and history.
Sediment composition in an elastic rock is determined by factors such as the source of the sediment, the processes of weathering and erosion, and the depositional environment. However, it is not determined by the age of the rock itself. The age may influence the degree of alteration or metamorphism but does not directly affect the sediment composition.
Different clastic sediments have different textures based on the size, shape, and sorting of the grains they are composed of. The composition of a clastic sedimentary rock will vary depending on the mineralogy of the grains present in the rock. Factors such as the source rock, transportation distance, and depositional environment can all contribute to the differences in texture and composition between clastic sedimentary rocks.
Clastic sedimentary rock.
Metamorphic rock
The type of plant that grew near a river.
Sediment composition in a classic rock is determined by factors such as the source material, transportation processes, and depositional environments. However, it is not influenced by the age of the rock itself. Instead, the age may provide context for the sedimentary processes but does not directly affect the composition of the sediments.
composition
Yes. Any rock can be weathered to form sediment.
Shale is a sedimentary rock formed from the compaction of fine-grained sediment such as mud or clay.
Flint is a chemical sedimentary rock that forms from the precipitation of silica-rich fluids, rather than from the accumulation and compaction of organic or clastic sediment particles.