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how can geologists organize past geological events by using relative age dating relative age dating allows scientists to determine the sequence of past geological events by comparing the order of rock layers there are five principles of relative age dating superposition original horizontality lateral continuity inclusions and cross-cutting relationships lets take a look at each principle imagine sediment deposits becoming thicker over time younger sediment layers bury older sediment layers over time more and more horizontal layers form on top of each other and turn into rock ing to the principle of superposition the rocks that were deposited first are the oldest notice how sediment is usually deposited in flat level layers this is due to the force of gravity over time layers of rock may fold or tilt even though the rock layers are disturbed you can still assume the layers were originally deposited horizontally the principle of lateral continuity states that the sediments are deposited