Abstract
An excellent correlation is found between K+Ca:Ti ratios in rock varnishes and radiometric ages of K-Ar-dated basalt flows in the Cima volcanic field and accelerator-radiocarbon-dated varnishes from nearby sites in the east-central Mojave Desert of California. This calibration extends from about 1 million to about 100 years BP, allowing the chronometric dating of geomorphic and archaeologic surfaces in the eastcentral Mojave Desert. There are significant differences between this curve and the cation-leaching curve developed for the Coso Range, southestern California. Therefore, this curve cannot be used to determine the ages of rock varnishes in areas far beyond the east-central Mojave Desert.
Original language | English (US) |
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Pages (from-to) | 72-81 |
Number of pages | 10 |
Journal | Physical Geography |
Volume | 8 |
Issue number | 1 |
DOIs | |
State | Published - 1987 |
Externally published | Yes |
Keywords
- California
- Cima volcanic field
- Geomorphology
- Mojave Desert
- Quaternary dating methods
- Rock varnish
ASJC Scopus subject areas
- Environmental Science(all)
- Atmospheric Science
- Earth and Planetary Sciences (miscellaneous)
- Earth and Planetary Sciences(all)