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A gap is a land form that is a low point or opening between hills or mountains or in a ridge or mountain range. It may be called a col, notch, pass, saddle, water gap, or wind gap, and geomorphologically are most often carved by water erosion from a freshet, stream or a river. Gaps created by freshets are often, if not normally, devoid of water through much of the year, their streams being dependent upon the meltwaters of a snow pack. Gaps sourced by small springs will generally have a small stream excepting perhaps during the most arid parts of the year.
Water gaps of necessity often cut entirely through a barrier range and Riverine gaps may create canyons may expose millennia of strata in the local rock column writing the geologic record. Such cuttings