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Why is sediment size alone not enough to classify clastic rock?
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.
How does one clastic detrital sedimentary rock have a texture and composition different than another?
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.
Sediment composition in a clastic rock is determined by all of the following EXCEPT?
The type of plant that grew near a river.
What is gravel sand and mud are called what sediment?
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 flint chemical clastic or organic?
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.
What is sediment composition in clastic rock determined by?
The type of plant that grew near a river. Apex.
Why is sediment size alone not enough to classify clastic rock?
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.
How does one clastic detrital sedimentary rock have a texture and composition different than another?
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.
Sediment composition in a clastic rock is determined by all of the following EXCEPT?
The type of plant that grew near a river.
What type of clastic sediment has the largest particle?
gravel
What is form when sediment is lithified?
Clastic sedimentary rock.
How are clastic rocks grouped?
Clastic rocks are grouped based on the size of the grains of sediment contained within them.
What clastic sedimentary rock is made from finest sediment?
Metamorphic rock
Would texture or composition be more important to classify a clastic sedimentary rock?
composition
What is gravel sand and mud are called what sediment?
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.
What is a brief summary of the section charateristics of clastic sediment in the Earth space science book?
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.
Is flint chemical clastic or organic?
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.
