Want this question answered?
The force is created by the self weight of the overlying material.
pp
The process where grains are pressed together by the weight of sediments above is called compaction. It is one of the processes of lithification.
The particles in the sediments are cemented as pressure squeezes out water. The dissolved minerals in the water, usually silica or calcite, then become solid (crystallize), tying the particles together.
Usually weight from above, whether from a body of water or from additional sediments.
The main force is weight of overlying rocks , called overburden, which puts overburden pressure on sediments and make them compress and compacts
The process is called compaction.
The force is created by the self weight of the overlying material.
pp
Sediments (sand, clay, boulders etc) are derived from the erosion of preexisting rocks by snow, ice, water and wind. Eventually these sediments settle and are covered by more sediments. As the weight of overlying sediments builds up the pressure and minerals dissolved in and carried by groundwater cement the sediment particles together to form a new rock layer. This new rock is called a sedimentary rock.
As fluids and spaces between particles are squeezed out by the weight of overlying sediments, the particles become closer to each other, thus flattening the thickness of the strata.
The process where grains are pressed together by the weight of sediments above is called compaction. It is one of the processes of lithification.
Metamorphic
Pressure from weight of overlying rock.
Metamorphic
Metamorphic
Aquifers can't support the weight of overlying structures.