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MINERAL RESOURCES.
and from orange yellow through ocher and drab to corn yellow. Some pieces have a suggestion of green in the yellow, giving an olive tint. These colors in the jasper are sometimes solid over areas of several square inches and then again are banded or irregularly mixed with other colors. The colored jaspers occur mixed with and in patches scattered through gray cherty chalcedony or through translucent gray chalcedony. Streaks and splotches of black jasper or flint lend contrast to the varied colors of the jaspers. The luster of some of the petrified wood is dull and cherty, though a part is brighter, and some even glassy. Occasionally amethyst and quartz crystals are found in cavities in the petrified trees or coating over limbs.
Many of the petrified forests of Arizona, especially those near Adamana and Holbrook, are protected by law against material being carried off. Visitors are generally allowed to take off a few pounds, however, as souvenirs or material from which to cut souvenir orna­ments or gems. Even if one does not procure such specimens, a visit to the petrified forests always proves of great interest, especially to one interested in mineral objects of natural beauty. A trip to the forests is not difficult, and two areas of petrified trees can be seen in half a day's drive from Adamana, on the Santa Fe Railway.
Petrified forests are known to exist in other regions of Arizona, and some of these are doubtless outside of the regular reservation and where they could be used to procure material for polishing. If it is not possible to find such areas, a small area might be set aside where petrified wood could be obtained for use in ornamental work. Petri­fied forests occur in the Navajo Indian Reservation between Ganado and Chin Lee and have been reported farther west in the Moqui Reservation.
CALIFORNIA.
Mrs. Gertrude S. McMullen, of the Southwest Turquoise Company, of Los Angeles, Cal., kindly sent in a specimen of jasper from near Hart, Shasta County. This material is from a deposit owned by Hart & McCullum. It is composed of layers of white, gray, yellow, and red jasper in peculiar straight and curved bands. It appears to be slightly granular though very fine grained and susceptible to a fair polish. The material will be used in jewelry under the name "creolite."
LABRADORITE.
OREGON.
Maynard Bixby, of Salt Lake City, Utah, reports the discovery of a new deposit of labradorite in southern Oregon. The labradorite ranges from a colorless glassy variety resembling quartz to dark, showing fine red, salmon, and green tints. Mr. Bixby states that the mineral would yield handsome gem material.
CANADA.
Dr. E. S. Ward, of Rochester, N. Y., reports an importation of several hundred pounds of labradorite from Nain, Labrador, for gem purposes. There is a considerable demand for a good grade of this stone for jewelry purposes, especially in the West.