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Dip slope
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A dip slope is a geological formation often created by erosion of tilted strata. It is seen in large ridges that have one side that is steep and irregular (an escarpment) and the other side, the dip slope, that is generally planar and tilting at a continuous angle. The orientation of the dip slope is referred to as the strike.
Some rocks (usually softer ones) erode more rapidly than others. For example, shale most frequently erodes faster than limestone. In situations like this, an entire layer of the more eroded rock can be weathered away while a layer of a more durable rock will not be as affected. This results in a nearly flat surface created by the top of the more durable layer. When this happens to beds that are not tilted mesas are formed. When this happens to tilted beds, structures called cuestas and hogbacks are formed. Mesas will have a flat top while cuestas and hogbacks will look like ridges, with one side that is a dip slope and another side that is eroded and generally more steep.
Dip slopes can also be formed by igneous structures such as sills. Any generally planar geological structure can form dip slopes, when it is tilted away from horizontal.
Dip slopes are quite prone to landslides, due to the dipping flat erosional surface. Large sheets of rock have a tendency to slide down dip slopes.
- Dip circle - old means of measuring slope dip
- Strike and dip
- Cuesta
- Escarpment