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Geology and ground water of the Azapa valley, province of tarapaca, Chile

October 26, 1949

In the Azapa valley, Chile, Pleistocene and Recent alluvial fill, composed of intercalated lenses of clay, silt, sand, and gravel, contains a zone of saturation that is sustained by infiltration from floods of the San Jose river, from December through March.

Publication Year 1949
Title Geology and ground water of the Azapa valley, province of tarapaca, Chile
DOI 10.2113/gsecongeo.44.1.40
Authors George C. Taylor
Publication Type Article
Publication Subtype Journal Article
Series Title Economic Geology
Index ID 70215622
Record Source USGS Publications Warehouse