How Rivers Get Across Mountains: Transverse Drainages

Phillip H. Larson, Norman Meek, John Douglass, Ronald I. Dorn and Yeong Bae Seong

Annals of the American Association of Geographers, 2017, vol. 107, issue 2, 274-283

Abstract: Although mountains represent a barrier to the flow of liquid water across our planet and an Earth of impenetrable mountains would have produced a very different geography, many rivers do cross mountain ranges. These transverse drainages cross mountains through one of four general mechanisms: antecedence—the river maintains its course during mountain building (orogeny); superimposition—a river erodes across buried bedrock atop erodible sediment or sedimentary rock, providing a route across what later becomes an exhumed mountain range; piracy or capture—where a steeper gradient path captures a lower gradient drainage across a low relief interfluve; and overflow—a basin fills with sediment and water, ultimately breaching the lowest sill to create a new river. This article reviews research that aids in identifying the mechanism responsible for a transverse drainage, notes a major misconception about the power of headward eroding streams that has dogged scholarship, and examines the transverse drainage at the Grand Canyon in Arizona.

Date: 2017
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DOI: 10.1080/24694452.2016.1203283

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