Abstract
The soil’s position in the material cycle of the lithosphere (Fig. 2.1) shows that a large number of processes are involved in the formation of rocks, lithogenesis , in the form of a cycle. At the beginning of lithogenesis, rocks are formed through crystallization when the molten magma cools down. They are subject to further diverse changes through the processes of weathering , erosion , transport , deposition , diagenesis , metamorphism and anatexis , which are connected to one another in a cycle. Soils are a significant station in this cycle. On the one hand, they are the result of the transformation of rock in contact with the atmosphere, hydrosphere and biosphere (pedogenesis ), and on the other, they deliver material for the formation of new rocks. For this reason, soils cannot be understood and classified without knowledge of the rocks; however, the same is true for many rocks without knowledge of the soils (Kittrick 1985).
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Blume, HP. et al. (2016). Inorganic Soil Components—Minerals and Rocks. In: Scheffer/SchachtschabelSoil Science. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-30942-7_2
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