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To review our principles of relative dating as applied to such geologic cross-sections, we will make use of a neat learning tool available on the Internet."Athro Limited" is a private company which provides education modules on the Internet.Applying the principles of relative dating to these rock exposures (also called "outcrops"), we can reconstruct the sequence of events that created the geologic features which we see.Events can be the deposition of a sedimentary layer, the eruption of a lava flow, the intrusion of magma to form a batholith, a fault (break) in the rock that shifts one side relative to the other side (and causes an earthquake), a fold that bends and distorts rock layers, or any number of other geologic processes.

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Remember when we drew a topographic profile for lab manual exercise #1 (page 18) on Topographic Maps?Students begin by observing a photograph and a diagram of rock layers near Whanganui, watch an animation about how the layers were formed, then use an interactive labelling diagram to work out the order in which the rocks were created.