Through series of processes combinely known as Diagnesis.
Sedimentary
Strata (singular: stratum)
Cross-beds are horizontal units that are internally comprised of inclined layers. It is a sedimentary structure that forms during deposition on the inclined surfaces of bedforms.
The layers are formed by the deposition of sediments carried by wind, water, or ice.
sedimentary rock
Sedimentary Rock. Strata is layers of sedimentary rock that form from the deposition of sediment.
crustal movement occurring after deposition
erosion
Not exactly. Some metamorphic rocks have foliation, which can appear similar to the layers of sedimentary rock. Foliation develops from mineral grains being oriented by pressure, rather than the deposition of layers.
temperature and time or deposition and melting or collection and transportation or time and pressure
A gap in sedimentary layers is known as an unconformity, and occurs as a result of either erosion or a period of non-deposition.
Rocks formed from layers of materials that settle and get cemented together are Sedimentary Rocks.
Sedimentary
Strata (singular: stratum)
Cross-beds are horizontal units that are internally comprised of inclined layers. It is a sedimentary structure that forms during deposition on the inclined surfaces of bedforms.
Cross-beds are horizontal units that are internally comprised of inclined layers. It is a sedimentary structure that forms during deposition on the inclined surfaces of bedforms.
Sedimentary rocks are formed by the layering of materials, as new layers are added, they compress the lower layers which eventually physically adhere together.