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sedimentary rock layers begin by being horizontal but under stress they will fold into anticlines and synth lines geologists want to describe the amount of folding and tilting and to do so they use the term dip and strike here we have a tilted rock layer the rock layers dipping at 45 degrees a very easy way to remember what the dip is is to imagine that itamp;#39;s raining out and that water is dripping down the rock the direction in which water is dripping is the dip and the dip is measured from a horizontal surface here we have a horizontal surface represented by the top of body of water and you can see that the angle from that horizontal surface and the tilting rock layers is 30 degrees so once again the dip is the angle from the horizontal that our rock layer tilts if the rock were vertical it would have a dip of 90 degrees whereas horizontal rock wouldnamp;#39;t dip at all itamp;#39;s dip would be zero geologists also want to describe the direction in which the rock layer tilti
