Late-Wisconsin paleohydrology of the West-Central Amargosa Desert, Nevada, U.S.A.
Chemical Geology: Isotope Geoscience Section
By: H. C. Claassen
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Abstract
Studies of isotopes in groundwater using 14C, 2H (deuterium) and 18O have provided significant insight into the paleoclimate of middle and late Wisconsin age in a typical arid environment of southern Nevada, the west-central Amargosa Desert. Evidence indicates that recharge probably was through infiltration of runoff in paleostream channels and that this runoff was important only from ∼ 17,000 to ∼ 10,000 yr. B.P. Mean annual temperature at 17,000 yr. B.P. was ∼ 8°C less than present mean annual temperature; some summer moisture was effective in recharge. Winter (October–May) temperature at ∼ 10,000 yr. B.P. was ∼ 1°C less than present; summer moisture did not contribute to recharge.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Late-Wisconsin paleohydrology of the West-Central Amargosa Desert, Nevada, U.S.A. |
| Series title | Chemical Geology: Isotope Geoscience Section |
| DOI | 10.1016/0168-9622(86)90019-9 |
| Volume | 58 |
| Issue | 4 |
| Year Published | 1986 |
| Language | English |
| Publisher | Elsevier |
| Description | 13 p. |
| First page | 311 |
| Last page | 323 |
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