Question:

The sedimentary structure formed by unidirectional current is

Updated On: Feb 10, 2025
  • trough cross-bedding
  • oscillation ripple
  • concretion
  • hummocky cross-stratification
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The Correct Option is A

Solution and Explanation

Trough cross-bedding is formed by unidirectional currents, typically in a fluvial or shallow marine environment. This structure is characterized by angled layers of sedimentary material that are deposited in a current-driven direction.

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