5 Archaeological and Economic Geology (Posters)
Thursday, 27 March 2008
8:00 AM - 12:00 PM
GEOCHEMISTRY OF THE ALCA OBSIDIAN SOURCE, PERU
Paper number: 5-3
Program: Technical Sessions
Time: 8:00 AM – 12:00 PM
Authors
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Kurt RademakerUniversity of Maine, Orono, ME
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David GibsonUniversity of Maine - Farmington, Farmington, ME
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Martin YatesUniversity of Maine, Orono, ME
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Laure DussubieuxField Museum of Chicago, Chicago, IL
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Michael GlascockUniv of Missouri, Columbia, MO
Abstract
Field and laboratory investigations have identified up to six spatially and geochemically distinct Alca obsidian deposits over an area of ~1,000 km2 of the southern Peruvian highlands. The largest and most conspicuous of these is a ~412 ha. obsidian deposit at Cerro Condorsayana, located at the east rim of the Cotahuasi Canyon between 4,000 and 4,820 m elevation. We have used a suite of analytical techniques, including Electron Microprobe, Laser Ablation-Inductively Coupled Plasma Mass Spectrometry (LA-ICPMS), X-Ray Fluorescence (XRF), and Instrumental Neutron Activation Analysis (INAA), to provide the most high-resolution characterization of a Peruvian obsidian source to-date. Alca sub-sources are best discriminated by plotting sample concentrations of Rb vs. Sr, Rb/Sr ratios vs. Zn and Nb, and Mn vs. Ba. A substantial number of other element concentration differences also define these same geochemical groups. Our replicate sample analyses allow inter-technique and inter-laboratory comparisons.
These efforts have determined the spatial extent of Alca obsidian deposits and the patterning of geochemical variability within the Alca source region. We anticipate future non-destructive XRF analysis of Alca obsidian artifacts recovered from the full temporal sequence of prehistoric archaeological sites throughout Peru. Geochemical comparison of these artifacts with the new high-resolution Alca source fingerprint will allow us to better understand the evolution of prehistoric mobility and trade patterns over 13,000 years in the southern Peruvian Andes.