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Sediment sorting refers to the uniformity of grain size within a deposit, layering refers to the horizontal stratification of sediment, texture describes the size, shape, and arrangement of grains within a sediment, and grain roundness indicates the relative smoothness or angularity of sediment grains.
Sediment sorting refers to the uniformity of grain sizes in a sediment deposit, with well-sorted sediments having similar-sized grains. Layering refers to the stratification of sediment deposits into distinct layers. Texture refers to the size, shape, and arrangement of grains within a sediment. Grain roundness indicates the degree of abrasion a sediment particle has undergone, with well-rounded grains being smoother and more spherical.
The process that creates sedimentary rock from sediment is called lithification. This process involves compaction, where the weight of overlying sediments squeezes the sediment grains together, and cementation, where minerals in the groundwater crystallize and bind the sediment grains together to form solid rock.
The rounding and sorting of the sediment grains can be indicative of the energy of sediment transport. Higher energy environments tend to result in more rounded and well-sorted grains, while lower energy environments lead to more angular and poorly-sorted grains.
Pressure from above removes excess water and air from sediment, allowing mineral grains to compact and bind together more tightly. This process helps to form sedimentary rocks by cementing the sediment grains together.
Terrigenous
hydrates
Amorphous sediment is sediment that lacks a defined crystalline structure. It can consist of disorganized mineral grains, organic matter, or other materials that do not exhibit a regular geometric arrangement. Examples include volcanic glass shards and organic debris in marine sediments.
its actually a suspension
A sedimentary rock is formed.
Grain Roundness
Sediment rocks
Detrital- made of sediment grains Orgains- Made of fossils Chemical- from due to chemical reactions I hope this helped you enough :)
Sediment sorting refers to the uniformity of grain size within a deposit, layering refers to the horizontal stratification of sediment, texture describes the size, shape, and arrangement of grains within a sediment, and grain roundness indicates the relative smoothness or angularity of sediment grains.
Sediment sorting refers to the uniformity of grain sizes in a sediment deposit, with well-sorted sediments having similar-sized grains. Layering refers to the stratification of sediment deposits into distinct layers. Texture refers to the size, shape, and arrangement of grains within a sediment. Grain roundness indicates the degree of abrasion a sediment particle has undergone, with well-rounded grains being smoother and more spherical.
pressure or cementing
Grains can move closer together through a process called compaction, where external pressure is applied to sediment layers, squeezing out excess water and air between the grains. This results in the grains packing more closely together, increasing the density and reducing the volume of the sediment.