The intensely brilliant luster present on artifacts that were long subjecte
d to waterflow is herein referred to as river patina. This condition is fre
quently attributed to water flow tumbling of the artifact and abrasion resu
lting from the movement of water-borne materials. Although abrasion is a co
ntributing factor its contribution to the artifact's remarkable brilliance
is indirect.,It is suggested that chemical dissolution of the artifact's su
rface is more directly responsible. Dissolution processes remain active whe
n natural precipitation maintains water silica content below saturation lev
els. The possible presence of a submicron layer of amorphous silica gel on
the dissolving surface may be an additional factor in the brilliance of aff
ected artifacts.