Production and Techniques
Obsidian is relatively easy to work, aiding its prolific use throughout Mesoamerica. Obsidian is obtained by quarrying a source site. Pieces then are shaped by fracture as in the production of blades or knives. It may be also be formed by pecking and grinding, producing animal figurines, beads, labrets, ear ornaments, and other erratics. Pressure flaking blades from a prepared core was a common practice. Edge-rejuvenation or resharpening of blades was performed to prolong the lifespan of many pieces. Modern attempts to recreate production techniques are heavily based on Spanish records and accounts of obsidian knapping. Motolinia, a Spanish observer, left this account of pressure flaking: "It is in this manner: First they get out a knife stone (obsidian core) which is black like jet and 20 cm or slightly less in length, and they make it cylindrical and as thick as the calf of the leg, and they place the stone between the feet, and with a stick apply force to the edges of the stone, and at every push they give a little knife springs off with its edges like those of a razor."*
The widespread use of obsidian necessitated a large workforce to produce enough tools to supply an area. During Monte Alban's most populous period 900 to 1800 people were working obsidian. In Teotihuacan, a major contributor, if not possessing monopolistic control of obsidian trade and production, possessed more than 100 obsidian workshops within the city.
Trade
Obsidian sources are relatively easily identified through trace chemical element analysis, making obsidian an excellent medium for the study of long-distance trade in Mesoamerica. This pan-Mesoamerican trade industry is due to the limited number of quality sources; the low bulk of obsidian in transport, thus requiring less human effort in trade; and the large quantity of items that may be produced from that small amount. Two cultures are good examples of the source side of trading and the recipient side; Teotihuacan held significant control over major obsidian sources, and the Mayan culture did not control a single significant source. Evidence of Teotihuacan's trade strength is seen in the presence of obsidian artifacts originating from their controlled sources throughout Mesoamerica, even at a distance of over 350 miles. It is debated whether the rise of this culture's dominance came from obsidian trade or if the trade simply served as a mode for obtaining elite items or human labor. The Maya acquired their obsidian from long-distance trade arriving at central places such as Tikal, Uaxactan, and Palenque. These Maya centers then redistributed the obsidian to smaller settlements. This is seen by the lack debitage from core production, cortex flakes or large percussion flakes, in the more rural areas of Maya territory. The larger centers may have exported fully pre-formed cores to outlying regions. Evidence also points towards much coastal trade, with higher quantities of obsidian artifacts found in coastal sites than in those farther inland in areas such as Belize. Obsidian trade was far-reaching, allowing opportunities for contact and trade of a variety of other items and ideas during pre-Hispanic times.
Sources
Obsidian sources were limited in Mesoamerica. Principal sources in Mexico included Jalisco, Oyameles, Zaragoza, Guadalupe Victoria, Cerro de Minas, Cerro de las Navajas, and Ucareo, the post-classic source for the Toltec state. Sources in the Valley of Mexico and under Teotihuacan control were Pachuca, Otumba, and Chicoloapan. Pachuca was a notable source with its high quality green obsidian, which was traded widely throughout Mesoamerica. In Guatemala three sources were significant: El Chayal, Ixtepeque, and San Martin Jilotepeque. These highland Guatemalan sources served the Mayans through long-distance trade. The Olmec heartland and the Valley of Oaxaca are two significant locations that lack obsidian sources.
Chemical Analysis
Obsidian, a volcanic glass, comes from several geological sources in Mesoamerica, as listed above. Each of these sources has a distinctive “fingerprint” of trace elements of the chemicals in a particular obsidian sample. Neutron activity analysis and X-ray fluorescence are two methods of analysis to identify a sample's geological source. Dating analysis is also performed on obsidian artifacts. Hydration dating permits absolute or relative dating of a sample. The degree of hydration observed indicates how long it has been since an artisan exposed the obsidian surface. All of these analysis techniques are invaluable for obsidian production and trade studies in the region.
Cited Resource
- Hester, Thomas R., Jack, Robert N., and Heizer, Robert F. The Obsidian of Tres Zapotes, Veracruz, Mexico. University of California Archeology Research Facility. No. 13 pp. 65-131, 1971.