The Thermal Emission Spectrometer spectra of low albedo surface materi
als suggests that a four to one mixture of pyroxene to plagioclase, to
gether with about a 35 percent dust component provides the best fit to
the spectrum. Qualitative upper limits can be placed on the concentra
tion of carbonates (<10 percent), olivine (<10 percent), clay minerals
(<20 percent), and quartz (<5 percent) in the limited regions observe
d. Limb observations in the northern hemisphere reveal low-lying dust
hazes and detached water-ice clouds at altitudes up to 55 kilometers.
At an aerocentric longitude of 224 degrees a major dust storm develope
d in the Noachis Terra region, The south polar cap retreat was similar
to that observed by Viking.