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Geology; July 2004; v. 32; no. 7; p. 605-608; DOI: 10.1130/G20601.1
© 2004 Geological Society of America
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Groundwater-sapping origin for the giant quebradas of northern Chile

Gregory D. Hoke1, Bryan L. Isacks1, Teresa E. Jordan1 and Jennifer S. Yu1

1 Department of Earth and Atmospheric Sciences, Cornell University, Ithaca, New York 14853, USA

Northernmost Chile is home to a well-preserved disequilibrium landscape of great antiquity. Contrasting drainage patterns are developed on the western slope of the Altiplano plateau. The oldest of these patterns is a now-relict parallel-patterned drainage network. In places a younger pattern, comprising a series of deeply incised canyons, or quebradas, crosscuts the older parallel-patterned network. These canyons show strong evidence of a groundwater-sapping origin. We hypothesize that the initiation of the canyon network resulted from changes in the hydrological regime related to a drying out of climate of the forearc and to the uplift of the Altiplano plateau.

Key Words: Andes • geomorphology • rivers and streams • groundwater • groundwater sapping




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