Bed (geology)

From Wikipedia, the free encyclopedia
Jump to navigation Jump to search
Tilted sedimentary bedding in shales of the Cretaceous Salto del Fraile Formation, Peru.

Beds are the layers of sedimentary rocks that are distinctly different from overlying and underlying subsequent beds of different sedimentary rocks. Layers of beds are called strata. They are formed from sedimentary rocks being deposited on the Earth's solid surface over long periods of time.[1] The strata are layered in the same order that they were deposited, permitting discrimination as to which beds are younger and which ones are older (the law of superposition).[2] The structure of a bed is determined by its bedding plane, the surface that separates two layers.[3] Beds can be differentiated in various ways, such as by particle size or rock or mineral type. The term is generally applied to sedimentary strata, but may also be used for volcanic flows or ash layers.

Types of beds include cross-beds and graded beds. Cross-beds, or "sets," are not layered horizontally and are formed by a combination of local deposition on the inclined surfaces of ripples or dunes, and local erosion. Graded beds show a gradual change in grain or clast sizes from one side of the bed to the other. A normal grading occurs where there are larger grain sizes on the older side, while an inverse grading occurs where there are smaller grain sizes on the older side. By determining the type of beds, geologists are able to determine the relative ages of the rocks.[4]

Bed thickness[edit]

Thickness of bed and laminae sizes in centimeters

A bed is the smallest lithostratigraphic unit, usually ranging in thickness from 1 cm to several meters, and distinguishable from the beds above and below it. A bedding layer is distinct to a lamina, which is commonly defined as a sedimentary layer with a thickness of less than 1 cm.[5]

Classifications of Thickness of Stratification[6]
Bedding class Thickness (cm)
Very thick 100 – 300
Thick 30 – 100
Medium 10 – 30
Thin 3 – 10
Very thin 1 – 3

Engineering considerations[edit]

In geotechnical engineering a bedding plane often forms a discontinuity that may have a large influence on the mechanical behaviour (strength, deformation, etc.) of soil and rock masses in tunnel, foundation, or slope construction.

Geologic principles[edit]

Law of Superposition, Law of Original Horizontality, Law of Lateral Continuity, Cross-Cutting Relationship

There are geologic principles that the beds normally follow. Even though there can be cases where the principles do not apply mostly due to faults, they are true for most cases.

  • Law of Superposition states that the oldest rocks are deposited first and the younger layers are deposited last, as long as the beds have not been overturned through tectonic activities. This is used to date the stratigraphy and their relative ages.[2]
  • Law of Original Horizontality states that if the beds are not horizontal, then the layers were caused to either fold or tilt through tectonic activities and were deposited horizontally due to gravity.[7]
  • Law of Lateral Continuity states that the bed deposits extend in all lateral directions. This implies that two places separated by erosional features with similar rocks may have originally been continuous.[2]
  • Cross-Cutting Relationship states that a fault is younger than the rock layers that it goes through. This is used to find the relative ages of the rocks.

See also[edit]


  1. ^ Einsele, Gerhard (2000). "Sequences, Minor Cycles, and Event Stratigraphy". Sedimentary Basins. Berlin: Springer-Verlag. pp. 291–384. doi:10.1007/978-3-662-04029-4_7. ISBN 978-3-642-08544-4.
  2. ^ a b c Steno, Nicolaus (1671). The Prodromus to a Dissertation Concerning Solids Naturally Contained within Solids: Laying a Foundation for the Rendering a Rational Attempt both of the Frame and the several Changes of the Masse of the Earth, as also of the various Productions in the same. Translated by Oldenburg, Henry (2nd ed.). London: F. Winter – via Biodiversity Heritage Library.
  3. ^ Boggs, Jr., Sam (2006). Principles of Sedimentology and Stratigraphy (PDF) (4th ed.). Upper Saddle River, NJ: Prentice Hall. ISBN 0-13-154728-3.
  4. ^ Lyell, Charles (1830). Principles of Geology: Being an Attempt to Explain the Former Changes of the Earth's Surface, by Reference to Causes Now in Operation. 1. London: John Murray – via Smithsonian Libraries.
  5. ^ Campbell, Charles V. (February 1967). "Lamina, Laminaset, Bed and Bedset". Sedimentology. 8 (1): 7–26. doi:10.1111/j.1365-3091.1967.tb01301.x – via Wiley Online Library.
  6. ^ McKee, Edwin D.; Weir, Gordon W. (1953). "Terminology for Stratification and Cross-Stratification in Sedimentary Rock". Bulletin of the Geological Society of America. Geological Society of America. 64 (4): 381–390. Bibcode:1953GSAB...64..381M. doi:10.1130/0016-7606(1953)64[381:TFSACI]2.0.CO;2 – via GeoScienceWorld.
  7. ^ Levin, Harold L. (2009). The Earth Through Time. John Wiley & Sons, Inc. p. 15. ISBN 978-0-470-38774-0.