l^Jb- ^' Califorr\ia Art &^ Nature TOURMALINE. SCHORL—Black tourmaline; quite common in San Diego county and in The tourmaline is one of the most in- Baja California, disseminated through of but little teresting gems, yet known, quartz or feldspar. Crystals six inches especially under its true name, its di- in diameter have been observed. versity of color having enabled it to pass under a multitude of names. Black and brown tourmaline are usually opaque, and hence have no value as gems. The transparent stones available for gems are found in Maine, Connecticut and California, and in Brazil, Russia and Ceylon. The col- ored varieties are known correctly un- der the following names: ACHROITE (colorless tourmaline)— Of gem quality, has been discovered in San Diego county, California, associat- ed with other lithia tourmalines. BRAZILIAN EMERALD—The em- blem of the Brazilian clergy, is not an emerald proper, but a green colored tourmaline. A few green tourmalines have been found in San Diego county, A BRIGHT IDEA. in the lithia mine at Pala, and in sev- eral other localities, some of them of Dr. A. C. Hamlin published in 1873 the finest gem quality. One beautiful a small book, 'The Tourmaline,' of 107 specimen' showing a perfectly flat pages and 4 colored plates, devoted termination, is banded green at the mainly to the beautiful crystals of this end, then a band of achroite shading mineral as found in Maine. On page 62 into rubellite where fractured. An- he says: — other specimen is green at the center, 'It seems as though the light of with a thin outer crust of black. heaven was required in the production INDICOLITE—Blue tourmalines are of the gems, as it is for the marvellous reported as occuring in San Diego and varied hues of the flowers of vege- county. tation. Thus far, nearly all of our RUBELLITE—Beautiful radiations precious stones have been found on or and masses of crystals of pink tourma- near the surface of the .earth; and it line occur in the lepidolite at Pala. A appears as though the contact of the few crystals of gem quality, resembling air or a ray of sunlight was required those from the Isle of Elbe have been to build up their forms and perfect found in the county. The largest lines. Down in the thousand mines crystals measure two inches in di- along the slope of the Rocky Mountains ameter. the amethyst vanishes below the depth California Art & Nature. of 20 or 30 feet, while the same quartz A vein of feldspathic minerals, crystallizes in its beautiful and definite mostly decomposed, and lying on a but colorless forms in the depths of the granite foundation, contained masses deepest mines. The diamond and the of coarse, purple lepidolite, angular sapphire belong to superficial terrains; fragments of crystal quartz, and am- and we find that the rule of shallow blygonite, spodumene, and other min- deposit relates to most of the gems. erals. In this matrix were the beau- The topaz of Braz.il, the beryl of Si- tiful vari-colored crystals of tourma- beria, the chrysoprase of Silesia, the lines, and loose in the soil composed of turquoise of Thibet, or the opals of decomposed portions of the ledge, were Hungary, all occur near the surface of many of the finest gems ever found. the earth, and are never found below C. R. ORCUTT. a certain depth.' Oliver Cummings Farrington, in Birds and Nature for September, 1901, says: — 'The crystals are usually in the form of long, slender prisms; They often have the peculiarity of being differ- ently colored in different portions. Thus a crystal may be green at one end and red at the other, and in cross sec- tion may show a blue center, then a colorless zone, then one of red and then one of green. Some of the crystals from Paris, Me., change from white at one termination to emerald green, then lightl green, then pink, and finally colorless at the other termination. In some crystals again the red passes to blue, the blue to green and the green to black. Tourmalines of different colors have been known in the mountains near San Diego, California, for many years. At Pala the red crystals in lepidolite have been known since 1876, but not until 1898 was this remarkable deposit of lithia mica of known value, when the writer brought it to the attention of great chemical houses. The beautiful radiations of red tourmaline crystals in the delicate lilac lepidolite are sel- dom of gem value, but are now to be found in nearly every mineral cabinet in the world. At Mesa Grande, east of San Diego, OACTI AT one of the most remarkable deposits of HOME. tourmalines was brought to my notice in 1899. The locality had been known CASSITERITE — Tin stone from for nearly 20 years, but had previously Cornwall, England, is composed of 78.6 failed to attract attention. In 1900 the per cent tin, and 21.4 per cent oxygen. mine produced hundreds of crystals It occurs in the Black Hills, South Da- from 1 to 2 inches in diameter, gener- kota, at Temescal, Riverside county, ally 3 or 4 inches or more long, of California, and near San Diego. The nearly every shade and tint of color two latter localities may yield speci- that the world had yet known, except mens equal to that from Durango, some shades of blue and yellow. Mexico, which is polished as a gem. 429 TOURMALINE. OPyNieHT 1»01, BY A. W. HUUFOR^ Green Tourmaline (Brazil). Red Tourmaline or Rubelllte (Island of Elba). Black Tourmaline (Finland). Green Tourmaline (Haddam, Conn.) Brown Tourmaline (Gouverneur, N. Y.) Cross Section of Green Tourmaline (Cal.) Red Tourmaline or Rubellite in Lepldolite (Cal.) &c be o Plate 3.—Monstera deliciosa. 5 California Art & Nature 6 THE COLORADO DESERT. ber and water. Not so on the eastern declivity—the precipitous walls of rock, A vast triangular-depressed plain, hundreds, often thousands of feet in level of the sea for a below the large height, present small inducements for of its surface, with an ap- portion pi^^^^ growth, and the less precipitous area of twelve million proximate ^.^^^j^g ^j.^ ^^^ slightly less devoid of acres (about one-half of which lies botanical forms. in Mexican and territory), compara- jjj ^j^^ mighty chasms (or canyons), destitute of verdure or of am- lively eroded by the still active, tremendous is basin known as mal life, the great ^^rces of nature, the botanist finds the Colorado Desert. his richest harvest amid scenery This remarkable region lies bs- that for beauty and grandeur would tween the peninsular range of moun- rival even the Yosemite. Surround- tains and the Colorado river of the ed by walls three thousand feet or west, extending from the San Gor- more high, the queenly Washinst n gonio pass, at the base of the San palm (Washington flllfera) may b^ Bernardino mountains, on the north, found in groves, growing with tropi- to the shores of the Gulf of Califor- cal luxuriance beside quiet brooklets, nia, on the south, and forms one of rivalling in beauty and novelty the the most extensive and important giant Sequoia groves of California, portions of the arid regions of the Despite the large areas totally bar- United States. On the north and ren of vegetable life for the larger northeast it is separated from the portion of the year, the absolute lack more elevated plains of the Mohave of rain through long periods, whi h desert by a low range of denuded may extend over three or more years hills, extending from the San Bernar- of time, the Colorado desert posse ses dino mountains to near the junction in seasons of precipitation a flora that of the Gila and Colorado rivers. Simi- in variety and beauty of forms sur- lar arid conditions exist on the east- passes that of the Atlantic states. In ern borders of the Colorado river, in richness of variety and coloring, the Arizona, and south in Sonera, and flora of California is probably unsur- along the Gulf shores. passed, and the arid regions of tne From their rich chocolate-brown state are not one whit behind the color, the inhospitable barrier between more attractive western slopes. In the Colorado and the Mohave deserts springtime the stately lily of the des- is frequently indicated on maps as ert (Hesperocallis undulata) wastes the Chocolate mountains; but the its sweetness on the desert air; every range is better known to miners as dry and thorny bush produces its the Chuekawafla (Lizard) mountains, quota of beauty, and a wealth of bril- a peculiarly appropriate name, liant annuals spring into brief exist- from the great abundance and var- ance. lety of lizards, but probably given During June and July, 1888, the wri- from some fancied resemblance in the ter made his initial exploration in the outline of these hills to this nimble Colorado desert, the main object be- animal. ing the examination of various pros- The peninsula range of mountains, pects of gold, silver, lead and copper, with a varying altitude of four thou- which had been discovered in the sand to eleven thousand feet, rise in Chuckawalla mountains, for a gen precipitous abruptness from the tleman who was largely interested western borders of the plains. The in their development. A brief report crest of this mountain range forms on this region, named the Pacific min- a sharp and well-defined line of de- ing district, appeared in the tenth an- markation between the arid region nual report of the California state and the rich and fertile western slope, mineralogist.