The term was used by Abraham Gottlob Werner in his theory of the origin of the Earth, which was developed over the period from 1774 to his death in 1817.
[3] The concept became increasingly formalized over time and is now codified in such works as the North American Stratigraphic Code and its counterparts in other regions.
The lithology of a formation includes characteristics such as chemical and mineralogical composition, texture, color, primary depositional structures, fossils regarded as rock-forming particles, or other organic materials such as coal or kerogen.
[2] Geologic formations are typically named after a permanent natural or artificial feature of the geographic area in which they were first described.
Formations were at first described as the essential geologic time markers, based on their relative ages and the law of superposition.
The divisions of the geological time scale were described and put in chronological order by the geologists and stratigraphers of the 18th and 19th centuries.
[11] "Formation" is also used informally to describe the odd shapes (forms) that rocks acquire through erosional or depositional processes.