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A col in geomorphology is the lowest point on a mountain ridge between two Summit.Whittow, John (1984). Dictionary of Physical Geography. London: Penguin, 1984, p. 103. . It may also be called a gap or mountain pass. Particularly rugged and forbidding cols in the terrain are usually referred to as notches. They are generally unsuitable as , but are occasionally crossed by mule tracks or climbers' routes. Derived from the French col ("collar, neck") from Latin collum, "neck", "col", in Trésor de la langue française informatisé Digitized, 2012. the term tends to be associated more with mountain than hill ranges.Chambers 21st Century Dictionary'', Allied. The distinction with other names for breaks in mountain ridges such as saddle, wind gap or notch is not sharply defined and may vary from place to place. Many are separated by prominent cols.
The height of a summit above its highest col (called the key col) is effectively a measure of a mountain's topographic prominence.
Cols lie on the line of the drainage divide between two , often on a prominent ridge or arête. For example, the highest col in Austria, the Obere Glocknerscharte ("Upper Glockner Col", ) lies between the Kleinglockner () and Grossglockner () mountains, giving the Kleinglockner a minimum prominence of 17 metres.Willi End, Hubert Peterka (1990). Alpenvereinsführer Glockner- und Granatspitzgruppe. Munich: Bergverlag Rudolf Rother. .
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