what are the chemical sediments example?
An example would be salt. As seawater evaporates from a surface, what is left is salt.
There are four types of sediments that create sedimentary rocks. The fours types of rocks are sandstone, mudrocks, biochemical and chemical.
Chemical sediments are sedimentary rocks that form from the precipitation of minerals dissolved in water. These minerals accumulate on the ocean floor or in lakes through processes like evaporation or chemical reactions. Common examples of chemical sediments include limestone, gypsum, and halite.
The breaking up of rocks into sediments is called weathering. Weathering can be physical (mechanical) or chemical in nature, and it is a key process in the formation of sedimentary rocks.
Sedimentary rocks are formed through the accumulation and cementation of sediments or organic materials over time. These sediments can come from the erosion of pre-existing rocks, the remains of plants and animals, or chemical precipitation. Through processes like compaction and cementation, these sediments are eventually lithified into sedimentary rocks.
When sedimentary rock is weathered in nature by chemical or mechanical means, the particles that are produced can be eroded and deposited, becoming sediments.
1) Chemical and biological sedimentary rocks are produced by chemical weathering instead of the siliciclastic sediments which are created by physical weathering. Because physical weathering is much more often than the chemical weathering there are 10 times more clastic sediments in the earth's crust than chemical and biological sediments.
Some common chemical sediments created by organisms include calcium carbonate (by corals, shellfish), silica (by diatoms), and organic matter (by plants, algae). These sediments accumulate over time and can form rocks such as limestone, chert, and coal.
Not all rocks are, only sedimentary rocks are truly made up of sediments. Some metamorphic rocks do because they are formed when heat and pressure are applied to sedimentary rocks, which makes sediments the basis of these rocks as well
Fossils are nothing to do with weathering they are formed during the deposition of sediments before they become rocks.
Sedimentary rocks.
One interesting thing about sedimentary rocks is that since they are comprised of many different sediments, we are able to learn about where it was formed. For example, the sediments present in a conglomerate can tell us a little bit about the history of the rock.
Sedimentation