This Clovis biface—or two-faced point with a continuous
edge—is made of Green River Formation chert. Though
precisely when the Fenn artifacts were made is unknown, experts
used a process known as hydration analysis to get a rough idea of
when two obsidian points in the cache were created. When a newly
broken piece of obsidian is buried in soil it begins to absorb
water, forming a "hydration rind." Experts can use the thickness
of this rind to roughly determine age, which in the case of the
two obsidian points tested was thousands of years old.