To represent the geological boundaries between the three beds of conglomerate, sandstone, and shale, you can create a stratigraphic column that illustrates the vertical arrangement of these layers. Since all beds have the same dip, you would typically depict them as parallel layers inclined at the same angle. Additionally, you can use a geological cross-section to show how these beds interact laterally, emphasizing any contacts or transitions between the different rock types. It's also important to indicate the thickness and extent of each bed to provide a clear geological context.
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