Obsidian is natural glass that forms when volcanic lava with
high silica content cools rapidly. Although it only occurs at specific sites, obsidian
was valued by ancient civilizations for its various properties – translucency,
sharpness, workability. The obsidian from each volcanic site exhibits a unique
assemblage of trace elements, which allows scientists and archaeologists to
pinpoint the original source of excavated obsidian through instrumental
analysis. Determining where materials originate from helps researchers
understand ancient trade routes. Most of the obsidian analyzed from Kaman-Kalehöyük
comes from Nenezi Dag, Tulce,
and Komurcu sites in Central Anatolia, modern-day
Turkey. See http://www.busitu.numazu-ct.ac.jp/mochizuki/english/stattk.htm
Conserving obsidian is much like conserving other archaeological glass. The
surface is cleaned with ethanol or a solution of water and ethanol. While
treating obsidian conservators must be careful of the sharp and delicate edges
because obsidian fractures under mechanical pressure with the characteristic
conchoidal pattern typical of pure silicates.