Abstract
Abstract An only slightly weathered olivine-ronzite chondrite weighing approximately 25 pounds was found in 1950 seven miles southeast of the town of Densmore. Its external form and internal composition and structure are briefly described. The meteorite is cut by a thin veinlet of Ni-Fe, evidently formed by replacement. The name Densmore (1950) is proposed in contradistinction to Densmore (1879), which refers to three heavily-weathered fragments of an olivine-hypersthene chondrite found four miles to the NNW in Norton County.
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