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.
Deposition, compaction, and cementation are the three steps needed to create a clastic rock formation. Clastic rock is made out fragments of other rocks.
Clastic Rocks, Organic Rocks, and Chemical Rock
1. Mode of formation. 2. Chemical composition. 3. Origin.
Sandstone and shale Actually it is Organic, Clastic, and Chemical
its cow dumpings
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 basic types of unconformities:angular unconformities, disconformities, and nonconformities.
The three basic steps are erosion (weathering), transport (carrying silt), and deposition (carried load settles out).
cementation recrystallization compaction
Shale, sandstone, and conglomerate are examples of clastic sedimentary rock.
Clastic Rocks, Organic Rocks, and Chemical Rock
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)
Organic, Chemical and clastic.
Clastic, Chemical, and Organic
clastic organic chemical