Respuesta :
(1)
Sediments are squeezed together by the weight of overlying sediments on top of them. This is called compaction. Cemented, non-organic sediments become clastic rocks. If organic material is included, they are bioclastic rocks.
(2)
Fluids fill in the spaces between the loose particles of sediment and crystallize to create a rock by cementation.
Sediments are squeezed together by the weight of overlying sediments on top of them. This is called compaction. Cemented, non-organic sediments become clastic rocks. If organic material is included, they are bioclastic rocks.
(2)
Fluids fill in the spaces between the loose particles of sediment and crystallize to create a rock by cementation.
Answer:
Sedimentary Rock Formation
Two important steps are needed for sediments to lithify. Sediments are squeezed together by the weight of overlying sediments on top of them. ... Cemented, non-organic sediments become clastic rocks. If organic material is included, they are bioclastic rocks.