sand is usually well compacted during deposition, and resists additional compaction during burial. grain-to-grain contact in sand form a supporting framework that helps maintain open spaces between grains.
Lithification is a diagenetic process in which loose sediment is converted to hard rocky compaction and cementation.
So sediments (sand) are buried the increase in pressure from the weight of the overlaying material pushes the grains closer together. The volume of sediment is reduced and the fluids between the grains are also squeezed out. This leaves the sandstone tightly compressed together this is lithification.
Sandstone is a sedimentary rock formed from layer upon layer of deposited sand which undergoes lithification.
Lithification processes, collectively referred to as "diagenesis," include: compaction (example: clay to shale), cementation (example: sand to sandstone), and partial recrystallization (example: lime mud to limestone). Note: Pressure by itself does not by compaction lithify sand to sandstone. Sandstone diagenesis is mostly by cementation and also, sometimes, by partial recrystallization and crystal overgrowths. The same is so of gravel that lithifies to conglomerate.
Shale, because sand and other coarse sediments compress little.
The formation of sandstone involves two principal stages. First, a layer or layers of sand accumulates as the result of sedimentation, and then the sand becomes sandstone when it is compacted by pressure of overlying deposits.
A clump. Unless they have undergone compaction and cementation in a process known as lithification. Then they would be classified as a sedimentary rock, maybe conglomerate, breccia, or sandstone.
Sandstone is formed from compaction and cementation of sand sized particles of rock.
Lithification is the compaction of materials into a sedimentary rock, such as sandstone.
Weathering and erosion from an existing rock, transportation and deposition, compaction and cementation.
Sandstone is a sedimentary rock formed from layer upon layer of deposited sand which undergoes lithification.
You call them 'sequence of events'.
Lithification processes, collectively referred to as "diagenesis," include: compaction (example: clay to shale), cementation (example: sand to sandstone), and partial recrystallization (example: lime mud to limestone). Note: Pressure by itself does not by compaction lithify sand to sandstone. Sandstone diagenesis is mostly by cementation and also, sometimes, by partial recrystallization and crystal overgrowths. The same is so of gravel that lithifies to conglomerate.
2,1,3,4
Shale, because sand and other coarse sediments compress little.
it is a sequence of events in a story or how to
In this expert the sequence of events creates suspense by ?
historyA record of events told in sequence is called a Chronicle.
time lines are basically a sequence of events in order.