Newport daily independent., 1905-08-07
MOLYBDENITE MINE.
ORE USED IN MANUFACTURE OF
 STEEL FOUND IN MAINE.
Deposits Are of Rare Occurrence and the Value of Those Located Is Partly Conjec-
 tural.

One of the principal deposits Of molybdenum ore in this country is at Cooper. Me. It was visited in Sep tember. 1904, by Dr. George Otis Smith. of the United States geological survey, who tells in bulletin 26O, the surveys annual publication on it's ex- ploits in economic geology, how the American Molybdenum company pre- vented him from having more to say about the mOlybdenum of this locality. He was not permitted to visit the mine, but the observations he made at the surface furnished him sufficient data for consideration of the character ana origin of the deposit.
 The town of Cooper is in Washing ton county. in the extreme southeastern Dart of Maine, and is the fourth town ship west of Calais. The nearest rall- road station is Marion, in the second township south Prospecting for mo lybdenite has been carried on at seV- eral points in this locality, but the only important development thus far IS that on the property of the American Mo- lybdenum company.
 The moIybdenite occurs both tn peg matite dykes and in the granite cut by these dykes A number of distinct peg matite dykes were seen on this property, varying in width from a few inches to several feet In these the molybden!tte occurs in lead gray hexagonal crystals of short prismatic habit, or as less reg uiar foliated masses, often with radiate structure. The moly ybdenite is found also in small flakes or larger nests or flakes disseminated throughout the granite mass.
 MOlybdanite occurs at several other localities in Maine, as we'll as in the other New England states. It is usu- ally found in small flakes disseminated through the granite or gneiss, so that the Cooper occurrence is of special interest by reason of the light 1t throws on the origin of this mineral. The pegmatite dykes are probably approximately contemporaneou with the granite intrusion, representing the latest specialization of the gran tic magma, and therefore intrudlng the consolidated granite. In this pegmatite magma molybdenum dlsul- phide appears to have been a proml- nent constituent and to have crystal liZed early in the consolidation of the dykes. The molybdenite in the gran ite may be either the result of impreg- nation at the time of the pegmatitlc intrusion or 1t may be an original con stituent The former view is support ed by the apparently larger amount III the granite near the dykes.
 The ores of molybdenum have been in greater demand since molybdenum has been used in the manufacture ot steel to increase it's hardness and toughress. The comparative rarity and high cost of the ores, have, however, limited its use.
 The economic value of such deposit as the Cooper molybdenite is partly con jectural The conditions for quarrying and mining both the pegmatite and the wall rock appear favorable, and con- s3orable work of this kind has been done The rock lying on the dump contained varying proportions of mo- ly yodenite, but it seemed that most of the crude ore could be readily distin- Suished and separated from the barren rock by hand picking. The crucial test of the successful working of such de- posit is doubtless connected with the milling process, rather than with the mining me thods A compact plant for treating the molybdenite ore has been erected by this company, but the de tails as to cost of crushing the rock and of concentrating and cleansing the sep arated mineral could not be ascertained