| Abstract: | Travertine deposits in eastern Grand Canyon National Park, Arizona, are inferred to have formed under conditions of effective wetness that were greater than present. Uranium-series dating of 17 samples indicates that the deposits formed at about 15,000, 71,000, 111,000, 171,000, and 338,000 yr B.P. Intervals of travertine deposition are essentially contemporaneous with dated high paleolake levels, montane glacial maxima, and high paleowater-table levels from several Great Basin localities. ?? 1990. |
| Genre: | Article |
| ProdID: | 70016360 |
| Citation Author: | Szabo, B. J. |
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| Citation End Page: | 32 |
| Citation Issue: | 1 |
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| Citation Language: | English |
| Citation Larger Work Title: | Quaternary Research |
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| Citation Number Of Pages: | 9 |
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| Citation Publisher: | Elsevier |
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| Citation Search Results Text: | Ages of travertine deposits in eastern Grand Canyon National Park, Arizona; 1990; Article; Journal; Quaternary Research; Szabo, B. J. |
| Citation Start Page: | 24 |
| Citation Volume: | 34 |
| Citation Year: | 1990 |
| Type: | citation/reference |
| Text: | Ages of travertine deposits in eastern Grand Canyon National Park, Arizona; 1990; Article; Journal; Quaternary Research; Szabo, B. J. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| URL (DIGITAL OBJECT IDENTIFIER): | http://dx.doi.org/10.1016/0033-5894(90)90070-2 |
| Date Other: | Mon, 1 Jan 1990 00:00 -0600 |
| Publisher: | Elsevier |
