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582                                 MINERAL RESOURCES.
that exhibits color. Undoubtedly better material exists in the locality ' where this was found.
Dumortierite.—About the same time that Messrs. Eiggs and Diller found that the blue mineral supposed to be indicolite was identical with dumortierite in Harlem, New York, masses of quartz were discov­ered in Yuma county, Arizona, heavily impregnated with dumortierite and of an indigo-blue color, and which when polished resembled the blue lapis lazuli, and would serve the same purpose in jewelry, as the quartz is harder than lapis lazuli.
Tourmaline.—Among some very interesting minerals found by Messrs. C. E. Beecher and S. A. Robinson, at Newcoinb, Essex county, New York, were some remarkable specimens of brown tourmaline. The crystals, although not so fine as those from Gouverneur, New York, were frequently sufficiently transparent to offer material for at least one hundred gems, weighing from 1 to 10 carats. They varied from golden brown to topaz-yellow in color.
Rhodonite.—This mineral, which has been known to occur in bowlders near Cummington, Massachusetts, has been traced to the ledge. Fine masses, weighing several hundred pounds, have been blasted out, and efforts will be made during the coming year to introduce this as an orna­mental stone, it being as beautiful as the Siberian variety, which is so ex­tensively used for table tops, mantel pieces, paper weights, etc., in Russia.
Turquois.—Considerable mining of a desultory character has been carried on at the turquois mines near Cerrillos, New Mexico, by the In­dians and hunters, who obtained the turquois in a primitive manner by building fires against the wall rock and then cracking off large masses by throwing water on it. This method, however, invariably destroys the color. Some of the material sent from this locality during the past year was in form of thin veins entirely free from rock. In color it was almost equal to the poorer Persian material, and should find a ready use as an ornamental or decorative stone. The recent releasing of the property is likely to prevent the existing method of working the locality. A new deposit of turquois was opened during the year in the Holy Cross mining district, 30 miles from Leadville, Colorado, which is very simi­lar to the variety from Arizona and New Mexico, the color being, if any­thing, a better blue. At this locality there was no evidence of prehis­toric mining. Until recently the impression in the vicinity was that the turquois was an ore of copper.
Gadolinite.—This stone admits of a high polish, and is of a deep velvet-black color. During the last year large quantities of it were ob­tained near Bluffton, in Llano county, Texas, 22 miles from Burnet. The occurrence of this gadolinite was somewhat similar to that of allanite in Amherst county, Virginia. It has more than ordinary interest from the fact that it contains from 40 to 50 per cent, of yttria. About 1,000 pounds were found in a single pocket, associated with xenotime, fergusonite, and euxenite. One crystal weighed 11 pounds, another 13 pounds, and a single group weighing 40 pounds was obtained. The pro-