| a long, low ridge with a relatively steep face or escarpment on one side and a long, gentle slope on the other. |

cuesta
physical feature that has a steep cliff or escarpment on one side and a gentle dip or back slope on the other. This landform occurs in areas of tilted strata and is caused by the differential weathering and erosion of the hard capping layer and the soft underlying cliff maker, which erodes more rapidly. Cuestas with dip slopes of 40-45 are usually called hogback ridges.
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