Bouma sequence

The Bouma sequence (named after Arnold H. Bouma, 1932–2011) describes a classic set of sedimentary structures in turbidite beds deposited by turbidity currents at the bottoms of lakes, oceans and rivers. == Description == The Bouma sequence specifically describes the ideal vertical succession of structures deposited by low-density (i.e., low sand concentration, fine-grained) turbidity currents.

Source: Wikipedia — Bouma sequence (CC BY-SA 4.0)

Bouma sequence

The Bouma sequence (named after Arnold H. Bouma, 1932–2011) describes a classic set of sedimentary structures in turbidite beds deposited by turbidity currents at the bottoms of lakes, oceans and rivers. == Description == The Bouma sequence specifically describes the ideal vertical succession of structures deposited by low-density (i.e., low sand concentration, fine-grained) turbidity currents.

Source: Wikipedia "Bouma sequence" · CC BY-SA 4.0

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