Clastic sedimentary rocks are formed from the compaction and cementation of rock particles of various sizes which have been transported and deposited by the processes of erosion. Examples of clastic sedimentary rocks are shale, sandstone, and conglomerate.
Here's the process from start to finish, which can take millions of years:
It begins with the weathering and erosion of bodies of sedimentary, igneous, or metamorphic rocks; larger rock is broken up into smaller particles which are transported by moving water, ice, gravity or wind, and deposited at the bottom of a lake, a river delta, an ocean, or similar location where further movement is restricted or slowed down. The rock particles can range in size from boulders to clay particles less than .002 mm in diameter. If these rock particles are covered by additional particles, eventually the weight from above will start the process of lithification. Lithification is the compaction and cementation of particles which form rock. Compaction squeezes out the fluids and space that exists between the particles, and cementation results when the fluids that are squeezed out are replaced with minerals that were in the fluids. Once cementation occurs, the new sedimentary rock has been formed.
Sediment compositions in classic rocks are determined based on the topgoraphy and georgraphy of the land from which they're found. The weather in any given area will determine the rocks composition.
Clastic rocks are classified by the size of the rock fragments, or particles, of which they are made along with their mineralogical composition..
By their size of the fragments in them, called clasts.
Clastic sedimentary rocks are composed of minerals and rock fragments that were transported by moving fluids and were deposited when these fluids came to rest.
The type of plant that grew near a river. Apex.
Clastic rocks are rocks composed of broken pieces of older weathered and eroded rocks. The sediment composition in a clastic rock is determined through its facies associations.
The difference would lie in the origin of the sediment and largely on the distance the sediment traveled.
becuse sediment alone is not enough to classify clastic rock because clastic rock is made up of more than just sediment
clastic
When rock sediment is lithified, a sedimentary rock is formed. The two processes involved in lithification are compaction and cementation.
Clastic or bioclastic sedimentary rock is formed in this manner.
The type of plant that grew near a river. Apex.
The difference would lie in the origin of the sediment and largely on the distance the sediment traveled.
becuse sediment alone is not enough to classify clastic rock because clastic rock is made up of more than just sediment
clastic
Clastic sedimentary rock.
gravel
Clastic rocks are grouped based on the size of the grains of sediment contained within them.
Metamorphic rock
composition
Clastics lol.
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.
When rock sediment is lithified, a sedimentary rock is formed. The two processes involved in lithification are compaction and cementation.