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Fetched 2026-10-26 (cache).

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Noun

  1. {{lb|en|geology}} A form of [[graded]] [[bedding]] that occurs at the bottom of a body of water. The principle says that smaller colloids ([[particle]]s) settle farther in the [[strata]] while larger particles settle closer to the source of water.

Source: Wiktionary · CC BY-SA 4.0 (Wiktionary dump) · cached copy, not a rewrite.