  We present mid-infrared spectral mapping observations of the core-collapse
supernova remnant 1E 0102.2-7219 in the Small Magellanic Cloud using the
InfraRed Spectrograph (IRS) on the Spitzer Space Telescope. The remnant shows
emission from fine structure transitions of neon and oxygen as well as
continuum emission from dust. Comparison of the mid-IR dust emission with
observations at x-ray, radio and optical wavelengths shows that the dust is
associated with the supernova ejecta and is thus newly formed in the remnant.
The spectrum of the newly formed dust is well reproduced by a model that
includes 3x10^-3 solar masses of amorphous carbon dust at 70 K and 2x10^-5
solar masses of Mg2SiO4 (forsterite) at 145 K. Our observations place a lower
limit on the amount of dust in the remnant since we are not sensitive to the
cold dust in the unshocked ejecta. We compare our results to observations of
other core-collapse supernovae and remnants, particularly Cas A where very
similar spectral mapping observations have been carried out. We observe a a
factor of ~10 less dust in E 0102 than seen in Cas A, although the amounts of
amorphous carbon and forsterite are comparable.
