Geology and ground water of the Azapa valley, province of tarapaca, Chile
Economic Geology
By: George C. Taylor
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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.
Suggested Citation
Taylor, G., 1949, Geology and ground water of the Azapa valley, province of tarapaca, Chile: Economic Geology, v. 44, no. 1, p. 40-62, https://doi.org/10.2113/gsecongeo.44.1.40.
Study Area
| 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 |
| Publication Date | January 01, 1949 |
| 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 |