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

Economic Geology
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Abstract

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.

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Publication type Article
Publication Subtype Journal Article
Title Geology and ground water of the Azapa valley, province of tarapaca, Chile
Series title Economic Geology
DOI 10.2113/gsecongeo.44.1.40
Volume 44
Issue 1
Year Published 1949
Language English
Publisher Society of Economic Geologist
Description 23 p.
First page 40
Last page 62
Country Chile
Other Geospatial Azapa Valley
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