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cross-stratification

American  
[kraws-strat-uh-fi-kay-shuhn, krahs-] / ˌkrɔsˌstræt ə fɪˈkeɪ ʃən, ˌkrɑs- /

noun

  1. Geology. cross-bedding.


cross-stratification Scientific  
  1. An arrangement of sediment strata deposited at an angle to the main stratification. The most common type of cross-stratification is produced by the migration of sand dunes or ripples.

  2. ◆ Cross-stratification in which the individual strata are greater than 1 cm (0.39 inch) in thickness is called cross-bedding.

  3. ◆ Cross-stratification in which the individual strata are less than 1 cm (0.39 inch) in thickness is called cross-lamination.


Example Sentences

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See Examples For:

These beds are called hummocky cross-stratification and have a 3D architecture of hills and valleys, with inclined and declined layering that matches the dune shapes.

From Textbooks Jan. 1, 2017

These sediment layers are typically finely laminated and may contain hummocky cross-stratification.

From Textbooks Jan. 1, 2017

Two of their colleagues on the work have some particularly nice web resources related to cross-stratification.

From BBC May 8, 2013

Shaler is a classic example of cross-stratification - a process that produces thin, inclined layers of sediment.

From BBC May 8, 2013

They present frequent traces of cross-stratification, alternating with regularly stratified horizontal beds, with here and there an intervening layer of clay.

From The Atlantic Monthly, Volume 18, No. 105, July 1866 by Various

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