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16.3 g, 32 × 19.1 mm, 3.5 mm thick. A collector's proportion — narrower than QD189 and slightly heavier, so the section runs a little deeper through the piece.
The internal lattice is the accepted means of identifying an iron meteorite, and it is the reason these pieces are etched rather than polished. Polishing would produce a mirror; etching produces the record.







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