The Formation Of Sedimentary Rocks

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Sedimentary rocks are formed by a process called deposition. This is the process of the layering of dirt over time. One way sedimentary rocks are formed by this layering process happens when silt builds up over time. This often happens at the bottom of a source of water, or as pebbles and various other minerals are worn down by the elements, and then compressed into a rock form. There are three categories of sedimentary rocks; clastic, chemical, and biogenic. Clastic sedimentary rocks are generally formed from the pieces of other rocks that have been weathered or eroded. They are characterized by the size of the grains that make up these rocks, as well as their structure. Some of the types of rocks that are categorized under the title of clastic sedimentary include breccia. This rock is often not rounded, and therefore can be easier to distinguish from other rocks.There is another form of clastic rock formed by volcano clasts. These are named pyroclasts, and form from the eruptions of a volcano. Clastic rocks are where those rocks such as conglomerates, sand and mud stone, and shale fined their home. Chemical sedimentary rocks are formed by dissolved minerals in water. These minerals are then subjected to the process of lithification. This can happen when plants and animals change the balance of chemicals in the water. An inland sea that has been exposed to increasing temperatures can also form this chemical change, forming evaporites. This is often due to a lack of incoming fresh water. One of the best examples of this is the Dead Sea in Jordan. This lake has many chemical sedimentary rocks surrounding it, and more forming every day. These rocks are most generally made from one particular mineral, such as gypsum. The most sought after kind of chemical sedimentary rock is a banded iron formation. These formations are where a significant amount of iron is mined
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