Characteristics
Typically, a stratum is generally one of a number of parallel layers that lie one upon another to form enormous thicknesses of strata. The bedding surfaces (bedding planes) that separate strata represent episodic breaks in deposition associated either with periodic erosion, cessation of deposition, or some combination of the two.Davies, N.S., and Shillito, A.P. 2021, ''True substrates: the exceptional resolution and unexceptional preservation of deep time snapshots on bedding surfaces.'' ''Sedimentology.'' published online 22 May 2021, doi: 10.1111/sed.12900.Davies, N.S., and Shillito, A.P. 2018, ''Incomplete but intricately detailed: the inevitable preservation of true substrates in a time-deficient stratigraphic record.'' ''Geology'', 46, 679–682. Stacked together with other strata, individual stratum can form composite stratigraphic units that can extend over hundreds of thousands of square kilometers of the Earth's surface. Individual stratum can cover similarly large areas. Strata are typically seen as bands of different colored or differently structured material exposed in cliffs, road cuts, quarries, and river banks. Individual bands may vary in thickness from a few millimeters to several meters or more. A band may represent a specific mode of deposition: river silt, beach sand, coalTypes of stratum
In the study of rock and sediment strata, geologists have recognized a number of different types of strata, including ''bed'', ''flow'', ''band'', and ''key bed''. A bed is a single stratum that is lithologically distinguishable from other layers above and below it. In the classification hierarchy of sedimentary lithostratigraphic units, a bed is the smallest formal unit. However, only beds that are distinctive enough to be useful for stratigraphic correlation and geologic mapping are customnarily given formal names and considered formal lithostratigraphic units. The volcanic equivalent of a bed, a flow, is a discrete extrusive volcanic stratum or body distinguishable by texture, composition, or other objective criteria. As in case of a bed, a flow should only be designated and named as a formal lithostratigraphic units when it is distinctive, widespread, and useful for stratigraphic correlation. A band is a thin stratum that is distingushiable by a distinctive lithology or color and is useful in correlating strata. Finally, a key bed, also called a ''marker bed'', is a well-defined, easily identifiable stratum or body of strata that has sufficiently distinctive characteristics, such as lithology or fossil content, to be recognized and correlated during geologic field or subsurface mapping.Murphy, MA., and Salvador, A., 1999Gallery
See also
* Archaeological horizon * Bed (geology) * Geological formation ** List of rock formations *References
External links
