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Material that solidifies in such cracks remains behind as dikes. Precise dating of such dikes can reveal times of crustal rifting in the past. Rocks converted to new mineral assemblages because of changing temperatures and pressures are called metamorphic.

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Such regions of the crust may even undergo melting and subsequent extrusion of melt magma, which may appear at the surface as volcanic rocks or may solidify as it rises to form granites at high crustal levels. In wind-blown or water-lain sandstone , a form of erosion during deposition of shifting sand removes the tops of mounds to produce what are called cross-beds. Such hot circulating fluids can dissolve metals and eventually deposit them as economic mineral deposits on their way to the surface.

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Such hot circulating fluids can dissolve metals and eventually deposit them as economic mineral deposits on their way to the surface. Many of the criteria of top—bottom determination are based on asymmetry in depositional features.

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The source of ancient sediment packages like those presently forming off India can be identified by dating single detrital grains of zircon found in sandstone. Most methods for determining relative geologic ages are well illustrated in sedimentary rocks.

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