Abstract
THE Allende (Chihuahua, Mexico) meteorite of February 8, 1969 (ref. 1 and unpublished report of R. S. Clarke, jun., E. Jarosewich, B. Mason and J. Nelen), is of great interest because it belongs to a group of relatively rare carbon containing meteorites known as the carbonaceous chondrites and because the amount of material collected so far already exceeds the total weight of all other carbonaceous chondrites in museum collections.
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