Consult the figure below.Here,distinct internal laminations are inclined at an angle to the boundary of the main sedimentary layers.These are termed

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The distinct internal laminations that are inclined at an angle to the boundary of the main sedimentary layers are known as cross beds. Cross beds are formed by the migration of ripples or dunes in response to the direction of the current or wind, resulting in inclined layers within the sedimentary rock.

Consult the Figure Below