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Four basic processes are involved in the formation of a clastic sedimentary rock: weathering (erosion)caused mainly by friction of waves, transportation where the sediment is carried along by a current, deposition and compaction where the sediment is squashed together to form a rock of this kind.
The sediments begin to undergo diagenesis, which is an umbrella term for physical and chemical changes which turn sediment into sedimentary rocks. Physically, the primary change is compacting sediments and squeezing out fluid in the pores between sediment grains; imagine squeezing water out of a sponge.he sediments begin to undergo diagenesis, which is an umbrella term for physical and chemical changes which turn sediment into sedimentary rocks. Physically, the primary change is compacting sediments and squeezing out fluid in the pores between sediment grains; imagine squeezing water out of a sponge.