Body of rock strata possessing unifying characteristics usually indicative of the environment in which the rocks were formed. The term is also used to describe the environment of formation itself or unifying features of the rocks that comprise the facies.
Features that define a facies can include collections of fossils, sequences of rock layers, or the occurrence of specific minerals. Sedimentary rocks deposited at the same time, but representing different facies belong to a single
chronostratigraphic unit (see
stratigraphy). But these same rocks may belong to different
lithostratigraphic units. For example, beach sand is deposited at the same time that mud is deposited further offshore. The beach sand eventually turns to
sandstone while the mud turns to
shale. The resulting sandstone and shale
strata comprise two different facies, one representing the beach environment and the other the offshore environment, formed at the same time; the sandstone and shale belong to the same chronostratigraphic unit but distinct lithostratigraphic units.
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