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.
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.
The type of plant that grew near a river.
Gravel, sand, and mud are all types of sedimentary particles, with gravel being the largest size, followed by sand, and then mud being the smallest. Collectively, these sediments are referred to as clastic sediment.
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.
The type of plant that grew near a river. Apex.
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.
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.
The type of plant that grew near a river.
gravel
Clastic sedimentary rock.
Clastic rocks are grouped based on the size of the grains of sediment contained within them.
Metamorphic rock
composition
Gravel, sand, and mud are all types of sedimentary particles, with gravel being the largest size, followed by sand, and then mud being the smallest. Collectively, these sediments are referred to as clastic sediment.
Is determined by the way the sediments were transported to the place where they are deposited. Sediments have four main transported agents: Wind, Water, Gravity, and Ice. Sediments particles size can be carried and the distance is determined by the speed of that particle. Both the the distance of the sediments and the sediments agents determines the characteristics of that sediment.
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.