Material from field firing experiments using a 2,700-year old Formative kil
n at Batan Grande, Peru, was studied by X-ray diffraction and Mossbauer spe
ctroscopy. The experiments explore the technology involved in producing the
gray and black reduced ware for which Cupisnique and other Formative ceram
ics are justly known. During firing, the iron-bearing compounds in clays un
dergo characteristic changes which depend on kiln temperature and atmospher
e. These changes can be observed in the Mossbauer spectra. By comparing spe
ctra of an appropriate clay fired in field experiments and in the laborator
y with the spectra of ancient ceramics, a description of Formative firing t
echniques in a reducing environment is attempted.