The most obvious way to tell whether or not a rock is sedimentary is to look at its texture. Remember, sedimentary rocks are formed when sediments, fossils, shells, etc. are weathered and then lithified together. The lithification of those materials creates somewhat of an eclectic mix of particles. For instance, coquina looks as if someone cemented a bunch of shells together. Sedimentary rocks will have varying grain sizes, ranging from the larger gravel-sized grains to the microscopic microcrystalline grain sizes. These grains will vary in shape, from angular to well-rounded. Additionally, the grains will be arranged in varying manners, from being poorly sorted (a mix of different sizes) to well sorted (all generally the same size). When compared side by side with metamorphic or igneous rocks, the textural differences presented by sedimentary rocks become very clear.
Residual parent material is the weathered bedrock that is found beneath the soil layer. It is the unconsolidated material from which the soil has developed over time through the process of weathering and erosion.
Some examples of sedimentary rocks formed by chemical precipitation from seawater are limestone, dolomite, and evaporites such as rock salt and gypsum. These rocks form when minerals in seawater precipitate out and accumulate over time to create solid rock formations.
Rocks vary in mineral composition, texture, and origin. Igneous rocks are formed from magma or lava, sedimentary rocks are made from weathered materials or organic debris, and metamorphic rocks are altered by heat and pressure. Each type has distinct characteristics that result from their formation processes.
Sedimentary rocks form through the accumulation and compression of sediments such as sand, mud, and organic matter. Over time, these sediments are deposited in layers and compacted by the weight of overlying material, eventually hardening into rock through processes like lithification. Sedimentary rocks can also form from the remains of living organisms like shells or plants.
Sedimentary rocks are formed through the deposition and compression of sediments, such as sand, silt, and clay, over time. These sediments are compacted and cemented together to create layers of sedimentary rock, often by the pressure of overlying layers or through chemical processes. Examples of sedimentary rocks include sandstone, limestone, and shale.
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because they are
What do sedimentry rocks have to do with water
In the desert
sedimentry
sedimentry rocks can vary depending of the rock. But most sedimentry are between 12-100cm
yes because it is sedimentry isnt it ]
Cementation.
i mean in the rock cycle
it is the materials on the periodic table and rocks such as ignous rocks sedimentry and metamorphic rocks and many many more!
Conglomerate, Sandstone, Shale, Coal Seams, Limestone and Gypsum rock are Sedimentary rocks.
Sedimentary rocks change under great pressure and temperature condition to form metamorphic rocks