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. Graded beds refer to layers of sediment that vary in grain size, with coarser material at the bottom and finer material at the top. Horizontal and tilted beds refer to the orientation of the sedimentary layers themselves, rather than internal structures within the layers.

Consult the Figure Below