Cementation
Sandstone and shale Actually it is Organic, Clastic, and Chemical
Weathering, Erosion, Deposition, Compaction, & Cementation.
There are various processes that are involved in the formation of sedimentary rocks. This starts from weathering to deposition then erosion and finally there is lithification and compaction.
rock cools quickly from melted rockRock cools quickly from melted rock.
Sedimentary rocks require two processes to be formed. The first is weathering. Weathering is the disintegration/decomposition of rocks. Erosion is the process by which the weathered material is moved from one place to another. Erosion occurs when, for instance, a moving stream picks up a weathered pebble and moves it miles downstream to the mouth of a river. Erosion can also take place with ice, wind, etc.
Cementation
Sandstone and shale Actually it is Organic, Clastic, and Chemical
clastic organic chemical
Organic, Chemical and clastic.
Clastic, organic, and chemical rocks ~Isabelle (6th grader)
Weathering, Erosion, Deposition, Compaction, & Cementation.
Clastic sediments are sediments that have particles or pieces of rock (clasts) in them. The clasts can be of igneous, metamorphic or sedimentary rock. Non-clastic sediments are made up of dissolved minerals or organic matter.
Sedimentary rock formation begins with igneous, metamorphic, or other sedimentary rocks. When these rocks are exposed at the earth's surface they begin the long slow but relentless process of becoming sedimentary rock.
Melting.
The two major processes involved in the formation of sedimentary rock include deposition (in which sedimentary material is deposited in an area) and cementation (in which that material becomes glued together overtime).
The two major processes involved in the formation of sedimentary rock include deposition (in which sedimentary material is deposited in an area) and cementation (in which that material becomes glued together overtime).
The two major processes involved in the formation of sedimentary rock include deposition (in which sedimentary material is deposited in an area) and cementation (in which that material becomes glued together overtime).