essay

Raw materials and sources

ancient chalcatzingoAustin • Published In 1987 • Pages: 336-386

By: Grove, David C..

Abstract
Judging from some rather inconclusive sourcing studies done previously, Grove suggests that at the Olmec-influenced highland site of Chalcatzingo iron ores for pigment manufacture probably come from local sources, while mirrors mostly would have been imported in finished form. Through some new studies, it is strongly indicated that all obsidian used during the Formative period in Morelos State came from the Otumba and Paredon sources in the Teotihuacan Valley area, first passing through the Valley of Mexico; a distribution network probably largely separate from that for the Olmec core area on the Gulf Coast. Chalcatzingo could have functioned as the local importation, processing, and distribution center. The same is likely true of greenstone as described in Thomson: 1987 (Document 20) and Thomson: 1987 (Document 37). Kaolin, chert, and lime are not so readily sourced, but sources are near the site and could have been important in exchange. Granodiorite is available at the site and probably was used only there, for carving monuments.
Subjects
Laboratory analysis of materials other than dating methods in archaeology
Mineral resources
Special deposits
Lithic industries
External trade
tradition
Olmec
HRAF PubDate
2000
Region
Middle America and the Caribbean
Sub Region
Central Mexico
Document Type
essay
Evaluation
Creator Type
Archaeologist
Document Rating
5: Excellent Primary Data
Analyst
Leon G. Doyon ; 2007
Field Date
1972-1976
Coverage Date
3500 BP-2500 BP
Coverage Place
central-south highlands and Gulf Coast, Mexico
Notes
David C. Grove
For bibliographical references see Grove: 1987 (Document 3)
LCCN
85022673
LCSH
Olmecs