How Rivers Get Across Mountains: Transverse Drainages

  • Larson, Phillip H.; 
  • Meek, Norman; 
  • Douglass, John; 
  • Dorn, Ronald I.; 
  • Seong, Yeong Bae
Citations

WEB OF SCIENCE

17
Citations

SCOPUS

15

초록

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: antecedencethe river maintains its course during mountain building (orogeny); superimpositiona river erodes across buried bedrock atop erodible sediment or sedimentary rock, providing a route across what later becomes an exhumed mountain range; piracy or capturewhere a steeper gradient path captures a lower gradient drainage across a low relief interfluve; and overflowa 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.

키워드

antecedence; overflow; piracy; superimposition; transverse drainage; COLORADO RIVER; GRAND-CANYON; TECTONIC CONTROLS; BOUSE FORMATION; AFTON CANYON; EVOLUTION; ORIGIN; SYSTEM; UPLIFT; REARRANGEMENT
제목
How Rivers Get Across Mountains: Transverse Drainages
저자
Larson, Phillip H.; Meek, Norman; Douglass, John; Dorn, Ronald I.; Seong, Yeong Bae
DOI
10.1080/24694452.2016.1203283
발행일
2017
유형
Article
저널명
Annals of the American Association of Geographers
권
107
호
2
페이지
274 ~ 283