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In geology and related fields, a stratum (plural: strata) is a layer of sedimentary rock or soil with internally consistent characteristics that distinguish it from other layers. The "stratum" is the fundamental unit in a stratigraphic column and forms the basis of the study of stratigraphy.
Each layer is generally one of a number of parallel layers that lie one upon another, laid down by natural processes. They may extend over [[1 E11 m²|
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Weathering, Paleontology, Geologic time scale, Chronology, Alberta
Digital object identifier, Mars, Basalt, Hellas Planitia, Stratum