In geomorphology, a col is the lowest point on a mountain ridge between two peaks. It may also be called a notch, a gap or a saddle, although the last-named usually has a wider meaning and may contain a mountain pass. Moreover, the term col tends to be associated more with mountain, rather than hill, ranges.
The height of a summit above its highest col (called the key col) is effectively a measure of a mountain's prominence, an important measure of the independence of its summit. Cols lie on the line of the watershed between two mountains, often on a prominent ridge or arête.
Particularly rugged and forbidding cols in the terrain are usually referred to as notches. They are generally unsuitable as mountain passes, but are occasionally crossed by mule tracks or climbers' routes.
For example, the highest col in Austria, the Obere Glocknerscharte ("Upper Glockner Col", 3,766 m (AA)), lies between the Kleinglockner (3,783 m above sea level (AA)) and Großglockner (3,798 m above sea level (AA)) mountains, giving the Kleinglockner a minimum prominence of 17 metres. The notch is about 8 metres wide and links the two peaks with a usually corniced, often only two-foot-wide, narrow, snow-covered ridge. The col is on the normal climbing route from the Adlersruhe to the summit of the Großglockner; it acts as the exit from the Pallavicini Couloir (Pallavicini-Rinne) (an ice gully lying at up to 55 ° to the horizontal) from the north and has never been climbed from the south. Hardly anyone has ever considered crossing the Glockner massif via this col.