In the grand canyon, the same rock layers are visible on opposite sides of the canyon and were deposited simultaneously, which is an example of what?
directly continuity
width continuity
bilateral continuity
lateral continuity
Look at the Grand Canyon in Figure below . It’s a good example of lateral continuity. You can clearly see the same rock layers on opposite sides of the canyon. The matching rock layers were deposited at the same time, so they are the same age.