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The Topaz Basin archaeological obsidian source in the transition zone of central Arizona
Abstract
The Classic Period Migration Project involves the analysis of archaeological sites at Perry Mesa in central Arizona and resulted in the discovery of several small marekanite1 obsidian artifacts that signaled a previously unlocated source. The source was eventually located in the Topaz Basin area of the upper Cienega Creek stream basin, southwest of Camp Verde, Arizona.2 While this locality solves the “unknown” sources in the Perry Mesa archaeological assemblage, it has not appeared in the archaeological record of Arizona with any frequency. The glass itself is an excellent medium for tool production, so its near absence in the archaeological record is likely attributable to social/territorial causes as well as limited secondary deposition, and along with other “minor” sources points to the archaeological utility of understanding these smaller sources. © 2009 Wiley Periodicals, Inc.
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Following Shackley (2009), rocks with relatively limited archaeological distributions provide an opportunity to learn on different levels of human organization of technology, mobility, and landscape use.
“Following Shackley (2009), we suggest that rocks with relatively limited archaeological distributions provide an opportunity to learn on different levels of human organization of technology, mobility, and landscape use.”
From Geographic vectors of human mobility in the andes (34–36° S): comparative analysis of ‘minor’ obsidian sources (2016) · cites this paper as Shackley, 2009
Laguna del Diamante and Cerro Huenul can be described as 'minor' obsidian sources based on the intensity of human use recorded on a macro-regional scale.
“in this paper we present a comparative analysis of the human use of two Andean obsidian sources that, based on the intensity of human use recorded on a macro-regional scale, can be described as 'minor' sources (sensu Shackley, 2009)”
From Geographic vectors of human mobility in the andes (34–36° S): comparative analysis of ‘minor’ obsidian sources (2016) · cites this paper as Shackley, 2009
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Research works printed but not linked: 25
- Arizona Bureau of Mines, 1958, Geologic map of Yavapai County, Arizona
- Bennet V.C., 1987, Proterozoic crustal history of the western United States as determined by Neodymium isotopic mapping, Geological Society of America Bulletin, 99, 674, 10.1130/0016-7606(1987)99<674:PCHOTW>2.0.CO;2 · DOI
- Bouška V., 1993, Natural glasses
- Burt D.M., 1981, Garnet and topaz bearing rhyolites from near Burro Creek, Mohave County, Arizona: Possible exploration significance, Arizona Geological Society Bulletin, 13, 1
- 10.1002/1520-6548(200010)15:7<649::AID-GEA2>3.0.CO;2-F · DOI
- Fink J.H., 2000, Encyclopedia of volcanoes, 307
- 10.1130/SPE212-p77 · DOI
- 10.1130/SPE283-p79 · DOI
- Lewis R.E.(1983).Geology of Hackberry Mountain volcanic center Yavapai County Arizona. Unpublished Ph.D. dissertation California Institute of Technology Pasadena.
- Menges C.M., 1989, Geological evolution in Arizona, 649
- Moyer T.C.(1982).The volcanic geology of the Kaiser Spring area SE Mohave County Arizona. Unpublished master's thesis Department of Geology Arizona State University Tempe.
- Moyer T.C.(1986).The Pliocene Kaiser Spring (AZ) bimodal volcanic field: Geology geochemistry and petrogenesis. Unpublished Ph.D. dissertation Department of Geology Arizona State University Tempe.
- 10.1029/JB094iB06p07841 · DOI
- Nealy L.D., 1989, Geological evolution in Arizona, 609
- 10.2307/281117 · DOI
- Shackley M.S.(1990).Early hunter‐gatherer procurement ranges in the Southwest: Evidence from obsidian geochemistry and lithic technology. Unpublished Ph.D. dissertation Arizona State University Tempe.
- 10.1002/gea.3340070403 · DOI
- 10.2307/282264 · DOI
- 10.1006/jasc.1998.0274 · DOI
- 10.1007/978-1-4757-9276-8_4 · DOI
- Shackley M.S., 2005, Obsidian: Geology and archaeology in the North American Southwest
- 10.1080/00231940.2001.11758437 · DOI
- Wilcox D.R., 2007, The archaeology of Perry Mesa and its world
- Wilcox D.R., 2001, Deadly landscapes: Case studies in prehistoric Southwestern warfare, 109
- Wittke J.H.(1984).Geochemistry and isotope geology of basalts of the Arizona Transition Zone (Yavapai County) and their tectonic significance. Unpublished Ph.D. dissertation University of Texas Austin.
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Cortegoso, V., Barberena, R., Durán, V., & Lucero, G. (2016) · Quaternary International · doi:10.1016/j.quaint.2015.11.133 · Cited by 38
Cortegoso, V., Yebra, L., Durán, V., Barberena, R., Lucero, G., Cornejo, L., Giesso, M., MacDonald, B. L., & Glascock, M. D. (2020) · Archaeological and Anthropological Sciences · doi:10.1007/s12520-019-01009-w · Cited by 20
Metadata
- Authors
- Shackley, M. S.
- Venue
- Geoarchaeology
- Publisher
- Wiley
- Published
- 2009-04-16
- Volume
- 24
- Issue
- 3
- Pages
- 336-347
- ISSN
- 0883-6353
- 1520-6548
- Cited by
- 8
- References
- 0
- Language
- en
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