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704                       MINERAL RESOURCES, 1913—PART II.
a hard dense texture necessary for good gems. Brown stains of limo-nite coat the faces of some of the veinlets and have permeated cracks and seams in them. Such material furnishes attractive matrix gems with varied markings.
A little turquoise has been found in a prospect at the Maltby silver-copper mine, about 1 mile south of west of the Texas Turquoise Co.'s mine. Hardened black siliceous slate is the principal rock at the Maltby mine, but the turquoise occurs in a small dike or sill of white partly altered porphyry a few feet thick, which is inclosed in the slate. A few pieces of greenish-blue turquoise were seen. These were associated with brecciated porphyry rather heavily stained with limonite. The only work done for turquoise at this locality consisted of a small prospect pit 2 feet deep, and, until further work has been done, the discovery must be considered merely an indication of possible gem material.
MISCELLANEOUS.
ASTERIA QUARTZ.
Asteria quartz of exceptionally good quality has been applied to use in jewelry by Bell & Birknir, of New York. The source of the rough mineral has not been revealed. The gems are cut round cabochon and are sold as asteria or star stone. They show a fine bright 6-ray star in reflected light on a nearly colorless highly trans­lucent background. The cut stones are very pretty and may be mounted simply or in a girdle of small diamonds.
HELIODOR.
A species of beryl has been introduced to the gem world under the name of "heliodor." ' This material has been very scarce so far and most of it is in the possession of the Emperor of Germany. It comes from Rossing, German Africa. Heliodor differs from most beryl in containing a small percentage of uranium oxide and in being weekly radioactive. The color by day is golden yellow and by arti­ficial light a delicate bluish green.
HET AEROLITE.
A specimen of hetaerolite from Leadville, Colo., was sent in by Mr. W. C. Hart, of Manitou Springs. This mineral, containing zinc and manganese oxides, occurs m botryoidal and mammdlary deposits with radiated columnar structure. According to Dana, it has s hardness of 5 and a specific gravity of 4.93. The specimen sent by Mr. Hart was cut cabochon. It is a brilliant black and in certain fights the radiated structure can be seen.
ICELAND SPAR.
Prof. J. P. Rowe, of the University of Montana, at Missoula, reports the occurrence of crystallized calcite, of sufficient transpar­ency to be classed as "Iceland spar," in Sweet Grass County, Mont,
1 Houdelet, A., Deutsche Goidschmiede Zeitung, abstracted to JeweJers' Circular-WeeiJj-, Apr. 22,Mi. Bauser, Otto, and Herzield, H., Chem.-Zeitung, June 2,1914..