The meteorite is a carbonaceous chondrite of the ALH85085 grouplet. Cecilia Satterwhite Small, dull patches of fusion crust remain on QUE93001 but are gone from 93002. The overall color of the exterior of these two specimens is red-brown. Large and small pyroxene crystals, both green and black in color, are visible on the exterior surfaces. The largest crystal noted in 93001 was 3 x 2 cm in dimension.
Numerous fractures penetrate the interior of the specimens making the meteorite easy to break apart.
The sections are identical and evidently represent a single meteorite. Most of the pyroxene is hypersthene, with composition Wo3Fs24, but a few grains of pigeonite were analyzed. Plagioclase compositions are in the range An90-96. The exterior color of 93004 is greenish-gray. Evaporite deposit is present on 93006.