Deposition, compaction, and cementation are the three steps needed to create a clastic rock formation. Clastic rock is made out fragments of other rocks.
The three processes are deposition of the particles or clasts, compaction from overburden and lithostatic pressure, and cementation of the particles by the precipitation of minerals out of the solution which surrounds the particles.
Clastic Rocks, Organic Rocks, and Chemical Rock
1. Mode of formation. 2. Chemical composition. 3. Origin.
it is when the process goes up and down and forms more of the it and goes thourgh the same process over and over again
Sandstone and shale Actually it is Organic, Clastic, and Chemical
The three processes are deposition of the particles or clasts, compaction from overburden and lithostatic pressure, and cementation of the particles by the precipitation of minerals out of the solution which surrounds the particles.
The three basic steps are erosion (weathering), transport (carrying silt), and deposition (carried load settles out).
The three basic steps are erosion (weathering), transport (carrying silt), and deposition (carried load settles out).
the three steps of hemostasis are :- (1) vasoconstrictiion (2) blood platelet plug formation (3) coagulation of blood
Shale, sandstone, and conglomerate are examples of clastic sedimentary rock.
The three basic types of unconformities:angular unconformities, disconformities, and nonconformities.
Clastic Rocks, Organic Rocks, and Chemical Rock
The mechanism of urine formation takes place by three steps. they are glomerular filtration, tubular reabsorption and tubular secretion.
The three most common clastic sedimentary rocks are: - conglomerate-sandstones-shale
Conglomerate, Sandstone and Shale are the three most common clastic sedimentary rocks.
Rocks are classified into the three categories, based on the method of their formation: Three main categories - igneous (solidified from magma/lava) metamorphic (undergone change from applied heat/pressure) sedimentary (deposited- can be clastic, biochemical and precipitated)
Clastic, Chemical, and Organic