Stable and radioactive isotope studies provide insight into the geochemical evolution of rock units. The geology of an area changes through time as rock units are deposited and inserted, and deformational processes change their shapes and locations. Geologists also use methods to determine the absolute age of rock samples and geological events. These dates are useful on their own and may also be used in conjunction with relative dating methods or to calibrate relative methods. The principle of cross-cutting relationships pertains to the formation of faults and the age of the sequences through which they cut. Finding the key bed in these situations may help determine whether the fault is a normal fault or a thrust fault.
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A. Strike-slip faults occur when rock units slide past one another. Optically stimulated luminescence and cosmogenic radionuclide dating are used to date surfaces and/or erosion rates. Dendrochronology can also be used for the dating of landscapes. Radiocarbon dating is used for geologically young materials containing organic carbon.
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Even higher pressures and temperatures during horizontal shortening can cause both folding and metamorphism of the rocks. This metamorphism causes changes in the mineral composition of the rocks; creates a foliation, or planar surface, that is related to mineral growth under stress. This can remove signs of the original textures of the rocks, such as bedding in sedimentary rocks, flow features of lavas, and crystal patterns in crystalline rocks.
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The principle of inclusions and components states that, with sedimentary rocks, if inclusions are found in a formation, then the inclusions must be older than the formation that contains them. For example, in sedimentary rocks, it is common for gravel from an older formation to be ripped up and included in a newer layer. A similar situation with igneous rocks occurs when xenoliths are found.