Date of Award

Spring 1985

Document Type

Thesis

Degree Name

Master of Science (MS)

Department

Ocean/Earth/Atmos Sciences

Program/Concentration

Geology

Committee Director

G. R. Whittecar

Committee Member

Dennis A. Darby

Committee Member

Harris B. Stewart

Abstract

Fluvial depositional processes along the Rio Magui in south-western Columbia are primarily controlled by localized uplift downstream of the mouth of the river, sediment sources that produce both coarse-and-fine-grained load, and numerous over-bank flows caused by torrential rainfall.

DOI

10.25777/6t6q-2049

Included in

Geology Commons

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