Longitudinal valley

The Val de Travers which, despite its name, is a longitudinal valley

A longitudinal valley is an elongated valley found between two almost-parallel mountain chains in geologically young fold mountains, such as the Alps, Carpathians, Andes, or the highlands of Central Asia. They are often occupied and shaped by a subsequent stream.[1] The term is frequently used if a mountain range also has prominent transverse valleys, where rivers cut through the mountain chains in so-called water gaps.

  1. ^ Whittow, John (1984). Dictionary of Physical Geography. London: Penguin, p. 318. ISBN 0-14-051094-X.

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