Newport daily independent., 1905-10-06
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 molybdeuum 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 2o0, 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 nolybdeuum of this locality He was not permitted to visit the mine, but the observations he made at the surface furnished him sufficient data for a consideration of the character and origin of the deposit.
 The town of Cooper Is tn washing ton county. in the extreme southeaStern part of Maine, and is the fourth town ship west of Calais. The nearest rail- road station is Marion, in the second township south. Prospecting for mo- Iybdeulrs has been carried on at sev- sral points in this locality, but the only important development thus far is that on the property of the American Mo lybdenum company.
 The molybdenite occurs both In 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 molybden1te occurs in lead gray hexagonal crystals of short prismatic habit or as less reg uIar foliated masses, often with radlate structure. The moiybdenite Is found also iu small flakes or larger nests of flakes disseminated throughout the granite mass.
 Molybdenite occurs at several other localities in Maine, as well as In the other New England states. IL IS usu- ally found in small flakes dissem1nated through the granite or gneiss. so that the Cooper occurrence is of special interest by reason of the light IL throws on the origin of this mineral, The uegmatite dykes are probably approximately contemporaneous With the granite intrusion. representing the latest capitalization of the gran itic magma, and therefore lntrudlng the consolidated granite In this pegmatite magma mOlybdenum d1Sui- 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 pegmatltlc intrusion or it may be an original con- stituent. The former view is support ed by the apparently larger amount in the granite near the dykes.
 The ores of molybdenum have been in greater demand since molybdenum has been used in the manufacture of stee! to increase it's hardness and tougnness The comparative rarity and high cost of the ores. have, however. limited it's use.
 The economic value of such deposit as the Cooper molybdenite is partly con iecturai. The conditions for quarrying and mining both the pegmatite and the wall rock appear favorable. and con- siderable work of this kind has been done The rock lying on the dump contained varying proportions of mo iy odenite. but it seemed that most ot the crude ore could be readily distin- guished 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 methods 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