Observations On Certain Types Of Chalcocite And Their Characteristic Etch Patterns (431e5bd6-3bfb-4646-8585-52bda243cbc4)

Discussion of the paper of C. F. TOLMAN, JR., presented at the New York meeting, February, 1916, and printed in Bulletin No. 110, February, 1916, pp. 401 to 433. Louis C. GRATON, Cambridge, Mass.-Of particular interest at this time is any paper that deals with chalcocite, the characteristic product of secondary enrichment and the copper mineral of greatest commercial importance, and that seeks to aid in the distinction between primary and secondary chalcocite-a distinction of much scientific and practical importance but one which thus far it has proved difficult to draw. The present paper on this subject by Professor Tolman, like the ,many preceding it which he and his colleagues at Stanford have published in the last couple of years, contains much of interest and suggestiveness. Without endeavoring at this time to review or comment upon Professor Tolman's conclusions in detail, I may say that many of them are in accord with the findings that my associates and I have been accumulating in the course of studying secondary enrichment in many of the copper deposits of the country. On the other hand, it goes without saying that in this comparatively new field of research or, at least, a field in which