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 , 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 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 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- . 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 , 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. 1890 ("The Colorado Des- The summit is usually clothed with ert," by Charles Russell Orcutt. pages forests of oak and pine The western 899-919). slope is thickly overgrown with a va- Lyell says: —"Geology is the science rled vegetation, the valleys supplied which investigates the successive in a greater or less degree with tim- changes that have taken place in the Cafifornia Art & Nature organic and inorganic kingdoms of nature; it inquires into the causes of these changes, and the influsnce which they have exerted in modifying the surface and external structure of our planet." In the decade commencing with 1850 the more depressed part of the ColoradQ desert seems to have been known as the Cienega Grande, now hetter known perhaps as the Salton Sea.but more usually designated as the Dry Lake; in 1870 we are told by early emigrants of that period that the Colorado river was in the habit of annually overfTowing its banks during the time of summer freshets, when the snows melted in the mountains whence the river has its source. This "annual overflow" (as often omitted as other- wise, it is said) formed a channel through the deep alluvial bottom lands of the great basin, to which the name New River was applied by the earlier pioneers who crossed the des- ert on the old overland route from Ft. Yuma to San Diego. Along the course of New River, the CEffiEUS OHLOBANTHUS Eingelm. Cocopa and other tribes of Indians planted and raised magnificent crops consist of shales and clays of a light on the overflowed lands. Corn, melons, brown or pinkish color, forming hills of squashes, and other vegetables, and considerable magnitude at the base of grain, reached the rankest growth at- the mountains. Prom their soft and tainable, and some of these early pio- yielding texture they have been eroded neers spoke with wonder of the fer- into a great variety of fantastic and tility of the soil and the success imitative forms. This series of beds attending these Indians in their agri- have been greatly disturbed, in many cultural labors. These fertile lands places exhibiting lines of fracture and were formed of the sediment deposi- displacement. Where they are cut ted by the waters of the Colorado through In the bed of Carrizo creek, river, and as the soil increased in depth they contain concretions and bands of the overflow decreased; with the in- dark brown ferruginous limestone, creasing Jnfrequency of these overflows which include large numbers of fos- now of more rare occurrence, the In- sils, ostreas and anomias. These have dians were compelled to depart—the been described by Mr. Conrad, and are Cocopas retreating to the region of the considered of Miocene age. In the de- gulf, the Cahuillas to the mountains bris of these shale beds I found frag- around the northern arm of the desert. ments of the great oyster (Ostrea In 1890 the desert Indian huts might titan), characteristic of the Miocene yet be found among the mesquite beds of the California coast. A few groves of New river, and in 1892 I found miles north of this point, similar the Indians producing from the unfill- strata, probably of the same age, were ed soil crops of promise, after an over- noticed by Dr. Le Conte, but there they flow of some of the lands below the contain gnathodon, an estuary shell, United States boundary. showing that the portion of the desert "Approaching Carrizo creek, we saw where they are now found was once for the flrst time in many days, strata covered by brackish water."—J. S. of unchanged sedimentary rock. These Newberry. California Art & Nature lO

Dr. J. G. Cooper reports (in bulletin Diego, on the Pacific side, would seem 4, California state mining bureau, pages to indicate that thegreat changes which 58 and 59) the discovery by H. W. have unquestionably taken place in Fairbanks, near Carrizo creek of "fos- this remarkable region were the re- sile coral-islands, the coral forming ex- sult of natural phenomena of gradual, tensive beds about the summits of yet rapid, occurrence. After its iso- short isolated ridges detached from the lation from the sea, with rapid evapor- mountains of the western rim, and con- ation, few years were requisite to sisting at their bases of granitic or transform this basin from an arm of metamorphic rocks. The ridges appear the sea to a barren waste, the salt of to have been islands when the desert the sea water forming the salt mines formed part of the Gulf of California, at Salton. or of the Pacific ocean, and were at tbe The Colorado river doubtless hurried right depth beneath the surface for past as it does today to the gulf, until coral growth on their summits for a breaking down the barrier it had itself long period. With the coral occurred erected. With alternate periods of several fossil shells of forms quite un- evaporation and influx of fresh wa- like those of the late tertiary of Car- ter, the great basin changed first to rizo creek beds, and apparently unlike a brackish lagoon, and finally to a vast those now Inhabiting the Gulf of Cali- fresh water lake. fornia." The water of the Colorado river at Fragments of fossiliferous rock of Yuma is known to carry at high wa- the Carboniferous age have been found ter not less than ten per centuni of in the Carrizo creek region by various solid matter. The deposit of this sedi- collectors, but none in place have yet ment in the great basin doubtless rap- been reported. idly formed the deep and fertile lands The Indians, according to Dr. Stephen which are now being harnessed into Bowers, still preserve the memory of service at Indio and Imperial, and catching fish along the eastern base of being converted at the latter place, by the San Jacinto mountains, where the the utilizing under control of the wa- Cahuilla Indians pointed out to him ter from the Colorado river, ititO fields ' ' the artificial pools, or "stone fish of agricultural promise. ' traps," where their ancestors easily se- Dr. Robert Edward Carter Stearns,- in cured the fish on the receding of the a paper read before the California tides of the ancient sea. This would academy of sciences, entitled "Remarks seem to indicate that the change from on fossil shells from the Colorado an arm of the gulf is comparatively Desert" (published in the American recent, and a study of the fossils seems Naturalist, 13:141-154, March, 1879), dis- to confirm this view. An old Indian cussed the occurrence of fresh water in the Cuyamaca mountains pointed shells found in a well at -Walter's sta- out to miners a few years ago points tion at a depth of fifty feet. The sur- in the hills to the eastward where his face of the desert where this well was great grandfather used to catch fish sunk is 195.54 feet below sea level. Dr. from the sea. Stearns remarks: The cause of the separation of this "Shall we indulge in a guess as to region from the gulf can be readily un- the depth of the water when these derstood in the present encroachment shells were alive? Shall we add the of the land that is forming from the depth of the well to the elevation of sediment and debris of the Colorado bench marks, the ancient levels which river, where it empties into the gulf. form terrace lines in some places along With the formation of a barrier separ- the distant hills, once a part of the ating thebasin from the gulf, th^ im- shores of an ancient lake, the walls of prisoned waters were at once subject- the Tjasin which once Inclosed and held ed to rapid evaporation. a fresh-water sea? It may have bf,en,' The presence of fresh water shells however, that the lake was never so in a semi-fossil condition, of a brack- deep as the figures thus added would ish water mollusk, and of marine shells indicate, and that instead of a lake or of species now found living at San a series of lakes, there existed only a California Art & Nature 12 lagoon or chain of lagoons, connected anist and geologist of the United Statss or disconnected, according to the vol- boundary commission, in reporting a ume of water, which probably varied reconnoissance made in 1849, wrote, one season as compared with another; concerning this region, as follows: a system of shallow reservoirs, receiving "On leaving the last rocky exposures water in the catchment or surplus per- to enter on the open desert plain, we iods or seasons of unusual rainfall, pass, some distance down the bed of sometimes, after a prolonged and wide- Carrizo creek; along the course of spread storm of great severity, uniting which are exposed the high bluffs of extensive a and forming an expanse sand, marl and clay, exhibiting a fine few feet only in depth, as was seen in sectional view of the tertiary format'on the the valleys of California during on which the desert plateau is based. rate of notable winter of 1861-62. The At the point where the road the depression may have been such as to bed of the creek, to mount to the des- continue to keep the lagoons supplied, ert tableland, some 150 feet above, fos- • • * within a re- and that only very sil marine shells of Ostrea are found, cent period has this depressed por- and gypsum makes its appearance in tion of the Colorado basin become bare extensive beds. The upper layer of and dry. Are the phenomena which the tableland shows a variable th'ck- exhib- this vast and remarkable region ness, composed of water-worn pebbles, * * * its the result of catastrophic ac- derived fromi the adjoining mountains. tion, sudden, violent, and widespread, Near the mountain base this plat au or the result of gradual changes mov- has a height of about 500 feet above ing slowly through countless cen- the level of the Colorado river. The turies?" surface extends in a gentle slope to- At Salton fresh water sihells are found wards the Colorado, or eastward, about in countless myriads, with recent spec- the distance of 25 miles, where it reach- ies of marine shells, on the surface of es its lowest depression at the lagoon the plain, 250 feet below sea level. Por- or Newi river basin, which is in fact a tions of the Dry lake are 300 feet below part of the extended alluvial tracts be- sea level. These minute fresh water longing to the Colorado river." shells are drifted into windrows in The New river region receives the places, where they may be scraped up drainage of a large scoce of country, by the quart. which is sometimes visited by heavy Along the eastern base of the San showers. "It retains this rain-water, Jacinto mountains, an old beach line and river overflows, for several is well defined, and can be easily traced months; when both these sources fail, for miles. The rocks are worn and it becomes a perfectly dry bed, or con- rounded up to this line, sharp and jag- tracts into quaggy saline marshes" ged above. This line by actual meas- (Parry). After a heavy rain or over- urement has been found to be even with flow there is a rank growth of grass, the present leval of the sea. and other vegetation, while consider- Major W. H. Emory, in report of the able portions sustain a heavy growth United States and Mexican boundary of the mesqulte. This affords fine survey, gave the following table of grazing for stock, which cattle men distances: have not been slow to appropriate. San Felipe to Vallecito, 17.85 miles, Between the peninsula range and the Vallecito to Carrizo creek, 16.6 miles. Colorado river and the gulf lies a high Carrizo creek to Big laguna, 26.41 mountain range, to the most northern mile.si. and western point of which has been Big laguna to New river, 5.83 miles. given the name of Signal mountain; New river to Little laguna, 4.5 miles. this consists of a form of syenite, as- Little laguna to Alamo Mocho, 16.44 sociated w.ith recent lava. "Its sur- miles. face is bare, and presents a forbidding Alamo Mocho to Cook's well, 21.84 outline of dark weathered rock, vari- miles. ously marked by furrows, and shows Cook's well to Fort Yuma, 20 miles. an irregular crest, gradually sloping Dr. Charles Christopher Parry, bot- towards the east." (Parry). Copyright, 1894, by W, J. Demorest • CEREUS MOJAVBNSIS Bngelro,

Copyrijlht, 1894, by W, J. Demorest.

CEREUS SENILIS Salm-Dyok. Copynght, 1894, by W. J. Demorest. Copyright, 1894, by W. J. Demorest.

CEREUS GIGANTEUS Engelm. 13 California Art & Nature 14

The Maricopas (of Arizona), the doubt seek at tim^s the pinyons or pine Cuchanos or Yumas, and the Cocopas ffiuts in the forests at the summit of are said to have originally formed one the peninsula range. tribe. The Coeopa Indians reside with- The townsite of Imperial is situated in the limits of Mexico and the Yumas about 30 miles east of the old stage in United States territory. Major station on Carrizo creek, and here a Heintzelman, in speaking of their ag- new civilization, based on modern agri- riculture, says: "It is simple; with cultural methods, is like to thrive an old axe, if they are so fortunate as where roamed the nomad in former to possess one, knives, and Are, a spot time. likely to overflow is cleared; after the waters subside, from the annual rise, small holes are dug at proper intervals, a few inches deep, with a sharpened stick, having first removed the surface for an inch or two, as it Is apt to cake; the ground is tasted; if salt, rejected and if not the seeds are planted. No further care is required but to remove the weeds, which grow most luxuriant- ly wherever the water has been. They cultivate watermelons, muskmelons, pumpkins, corn, and beans. The water- melons are small and indifferent, musk- melons large, and pumpkins good; these latter they cut and dry for win- ter use. Wheat is planted in the same manner, near the lagoons, in December or January, and ripens in May or June. It has a fine, plump grain and well- fllled heads. They also grow grass- seed for food; it is prepared by pound- the seed in wooden mortars made of ing CEREUS mesquite, or in the ground. With wa- BBRLANDIEJRI Engelm. ter the meal is kneaded Into a mass and then dried in the sun. The mesquite Dr. J. Le Conte, gave an interesting bean \s prepared in the ^ame manner, account of some volcanic mud springs and will keep to the next season. The or solfataras, near the Southern Pacific pod-mesquite begins to ripen the lat- railroad, on the Colorado desert in Sil- ter part of June; the screw-bean a lit- liman's Journal (2d ser. XIX, Ja. 1855). tle later. Both contain a great deal Arthur Schott mentions a severe earth- of saccharine matter; the latter is so quake which occurred November 23, full, it furnishes, by boiling, a palatable 1852, and quotes from manuscripts by molasses; and from the former, by boil- Major Heintzelman, as follows: "There ing and fermentation, a tolerably good exists, about 45 miles below Fort Yuma, drink may be made. The preat depend- in the desert between the western Cor- ence of the Indian for food, besides the dilleras and the Colorado, a pond, con- product of his fields, is the mesquite sidered as an old orifice, which had bean. Mules form a favorite article been closed for several years. The first of food; but horses are so highly priz- shock of an earthquake, in 1852, caused ed, they seldom kill them, unless press- a mighty explosion. The steam rose ed by hunger, or required by their cus- a beautiful snowy jet more than 1,000 toms." feet high into the air, where it spread Much the same methods are followed high above the mountains, gradually by the Cocopas today, as observed by disappearing as a white cloud. This the writer. They also visit the can- phenomenon repeated itself several yons opening on the desert from the times in a diminishing scale. Three west, and gather the sweet and edible months later I visited the place; jets palm fruits, there so abundant, and no took place at irregular intervals, from Nature. i6 15 California Art &

15 to 20 minutes. The effect was beau- DEAN, GEORGE^ ^^: ^^^^^ ^.^^ ^^ ^^ with the tiful, as they rose mingled ^g^^ ^ successful nurseryman and flor- black mud of the pond. The tempera- ist, well known to many as an ardent ture of the water in the principal pond collector of shells. was 118 degrees F., in the smaller one goodB. GEORGE BROWN: 135, and in one of the mud holes, from port 2 of the report of the U. S. Na- 1897 is a niemorial of which gases escaped, 170. The air tional Mus.eum for ... , ^ ,, * „„i^i,„^„f„/i this eminent naturalist, together with a full of which escaped was sulphurated sgie^.tjon of his papers on museums and hydrogen, and in the crevices crystals on the history of science in America. of yellow sulphur were found. The Portraits of the earher scientific men, ground near abeut was covered with lt^XLl\%lnif l^l\^nonTf^lT a white efflorescence, tinged with red tiflc and educational institutons of the and yellow. On the edge of a small United States," and "the beginnings of natural history in America," form a r,nnrl crystalsprv<3ta1<3 otnf sal

EDITORIAL.

Our aim in journalishm is to popular- ize study, to create a greater interest in the beauties of the world, to increase the number of lives that shall leave a mark on the world's history—lives more worthy of the Creator of the universe. Our direct aim is a review of our present knowledge, and a record of new discoveries, in natural hstory and other branches of science. Descriptions ot animals and , not easily accessi- ble to the young student, notes of eco- nomic or geographic significance, biblo- graphy, synonymy, and an interchange of ideas, will be means used to a com- Le CONTE, JOSEPH: mon end. One of the most eminent scientists, of the University of California, died July 6, 1901. BIOGRAPHICAL. He was of Huguenot descent, and was born in Liberty county, Georgia, 26 F 1823. BIRTWBLL, FRANCIS J.: As a teacher he was suggestive, inter- Wiell and favorably known to ornithol- esting and inspiring, and his naturally ogists as a writer on the birds of New kind and genial disposition gained him Mexico, ascended a lifty pine tree to pro- the affection of his pupils. Geology, cure a birds' nest, 29 Je 1901, became optics, aerostatics and physiology were entangled in the rope and strangled In branches upon which he became author- the presence of his bride. ity. msRfnsK^n'^i^m Volume I. Number 2. January, igo2. Price 20 cents; $2 a year.

Califorr\ia Art & Natuire

Art (2f Nature No. 868 San RW^^n^^^nCompany, publishers, 15th st., Diego, California.

25 California Art & Nature 26 THOMAS MEEHAN. e al contributor. The professor was often asked to write his biography, but "Friend after friend departs, said that at his age he would rathe^ Who hath not "eta f -ie d?" be making history that writing it. He of The State Botanist Pennsylvania was fond of music and said: "When 1 senior editor of Meehan's Monthly and want a change from scie.ice I take my "bettet of Germantown, passed to the flute and play over some old church 75 He land" Nov. 19, irOl, aged years. tunes. Indeed I sometimes think that in March was born London, England, when they bury me I would listen with 1826. He once wrote: earliesr 21, "My pleasure to "Autumn" if they would is of in a field recollection butter-cups sing it over my grave." waves a of grass tossed into mimic by MRS. E. E. ORCUTT. summer breeze, at three years of age, West London, England." HOUSE HOLD PESTS. His early home was the Isle of Wight. There being no schools there 'The Silver Fish' belongs to the low- his mother taught him to read and est order of insects—the Thysanura— write. The "Book of Common Prayer" is wingless, of very simple structure, was his primer, the Bible and Bunyan's worm-like, about 1-3 inch long, taper- Pilgrim's Progress his readers. After ing from near the head to the extrem- th? moved 4o Ryde he went to ity of its body, and often one of the school two years. Eager for learning most troublesome enemies of books, h3 improved every cppcr.uiity, anl papers, card lables in museums, wi h his hard earned pocket money startched clothing, and more rarely boLght a Latii Dictionary and Gram^ stored food substances. The entire mar, Logic and some other books and surface of the body is covered with s ud'ei nights in his father's green- very minute scales like those of a house. And thus became so proficient moth. The head carries 2 prominejit that before he was 19 he was elected antennae, and at the tip of the body meber of tha Royal Wernerian Soci- are 3 long, bristle-shaped appendages, ety cf Edinburg, on account of his or- one pointing directly backward, the iginal contributions, cne of them bsirg other 2 extending out at a consider- a paper in which a knowledge of Latin able angle; 4 shorter appendages are wa? an fcs;e:tal re;usite He also near; 6 legs spring from the thorax, studied Greek the same way, and be- and, while not very long, they are pow- came so fami'iar with French as to erful and enable the insect to run with read it like English. This young man great rapidity. saw Victoria, the then young queen, Heavily glazed paper is very attrac- more than once, whi'e he was a stu3ent tive to this insect, while it often causes at Kew gardens. Ihe young man went wall paper to scale off by its feeding to America, and at the age of 22 en- on the starch paste. Pyrethrum fur- tered Philadelphia, where for more nishes the best means of control, than ha'f a century he has been one wherever it can be applied. C. L. Mar- of the leading mi ids of the c'ty, being latt describes and figures it in bulletin 20 years on the school board and long No. 4, new series, division of entomol- a member of the city legislature and ogy, U. S. department of agriculture, being the means of gettin'^ up 23 small from which the above notes are main'y parks for the benefit of the poor. Ha taken. Lepisma saccharina L. is the became respected and beloved by the common species of Engla-nd, now prac- large community. He was the friend tically cosmopolitan. cf the genial Botani-t, Dr. A?a Gray, and spoke of him as "one of the kii»d- EPIDOTE—The United Btates pro- est of heart among my friends." Prof. duced $250 worth of this seml-p'^eciGUs Meehan has been for some years an stone in 1895. Crystals in masses have efficient director of the Philadelphia been obtained by the writer near the Academy of Natural Science, the col- Alamo, and associated with crystals of lections of which are the th!rl best o -. i»alcite from near the coast south of this continent, to which he was a iib^ Santo Tomas, . 27 California Art & Nature ^8 WEST AMfiRICA.*r MOLLUSCA. proximate teeth. White of yellowish. Length 3.3, diameter 2.5 mm. BINNEYA NOTABILIS J. G. Cooper. Living: San Diego, California (Orcutt). San Lucas, Baja California. Tryon, Monog T M 32, t 3 f 4. Cape Depressed, smooth and shining, epider- CAELATA mis expending beyond margin of apeit- SELENITES Mazyck. translucent when but Shell small, depressed, brownish horn- uro, young, opa- with thickened old. Nuclear color, very coarse, rough, crowded, quely when whorl which are with about 30 delicate transverse ribs. subseo.u. distant, irrtgular ribs, obsolete at the apex; whorls 4, rounded, Pale brown. Diameter 12, 3 mm. height somewhat inhated in- Santa Barbara Island, California; below, gradually creasing*,, the last not descending at the Guadalupe Island, Baja California (G. "W. Dunn). ai>' r ure; suti re mpres ed; umbilicus On the mainland near wide, clearly exhibiting all the volutions; San Quintin, almost Baja California (Orcutt). aperture circular, slightly oblique; pei\s Oiiie simple, its ends approaching and joined a BORNIA PULCHRA Philippi. by very thin, transparent, whitish callus, through which the ribs Dr!?, U S Na Mu 21: 889. pr 880, are distinctly seen. Greater diameer 4, Kellia pulchra Philippi, Zeitschr fur heieht. 1.75 mm. Santa Barbara (Dr. L. Mol 5: 149 (1848). "Probably a Pythina, G. Alameda but Yates); Hay ward's, county, unflgured."—Dall. "West America." California (W. H. Dall). Mazyck, U S Na Mu pr 9:460-461, f 1886. BORNIA RETIFEiRA Dall. "Shell thin, white, moderately convex, SELENITES DURANTI. rounded, trigonal, nearly equilateral; Mazyck, U S Na Mu pr 9:460-1 f (1S86). beaks distinct, not high; surface polished, Helix durantl Newcomb, Ca ac pr 3:118 with faint incremental lines and minute (1864). close punotations whose interspaces give Patula durantl Tyron, Am J Conch the effect of a fine netting; hinge normal, 2:2i-'. t 4 f 53 (1866). Mong. T. M. 51, t 4 delicate; adductor scars rounded, high f E-'. up; posterior basal margin very slightly Hyalina durantl Binney and Bland L-F f crenulate. Lon. 12, alt. 9, diam. 4 mm. S 1:37, 49 (1869). One left valve dredged by the U. S. Fish Macrocyclis durantl W G Binn T M Commission at station 2900, in 13 fath- 5:9';-, 18S. Man Am L S 85 f 49 (1885). oms, off Santa Rosa Island, California." 'Shell depressed, discoidal, pale cor- —DrII. U S Na Mu pr 21: 889, 880, t 87 f 2 neous, under the lens minutely striated, (1899). opaque, broadly and perspectively um- bilicated; whorls 4, the last shelving but ANOMIA SUBCOSTATA Conrad. not discending (at the apeture); suture Obtusely ovate, rather thick; umbo of linear; aperture rounded, lunate, l.p the external and internal larger valve ventricose; hinge thickened, simple, ap- surface of the valve obtusely undulated proaching. Santa Barbara Island."— concentrically, and marked with waved, Newcomb. not at all wrinkled, interrupted ribs, much raised, Tryon says: "spire elevated, except towards the base, where they are perfectly plane above." larger and somewhat tuberculiform; up- Binney says: "with very coarse rough per valve entire, or with obsolete radii striae." towards the base. Diameter 5, height 1.75 mm. Miocene: Carrizo creek, San Diego Pilsbry, Phila ac pr 1889, p 196, treats county, Calif. Selenites caelata Mazyck as a variety of this. MELAMPUS OLIVACEUS Cpr. Gould. Obconic; spire short, suture SELENITES SPORTELLA indistinct; t 3 f 7. whorls 7-9, Tyron, Mong T M 33, obtusely angulated on the Gould. ' body below the suture; Macrocyclis sportella aperture long the of the last and narrow, lip covered Whorls 5, superior part with sharp ono fattened the lammae within, parietal wall with from upon approaching apert- 1 to ?, small ure, rounded below; very light apple revolving laminae; there is and also a stout fold on the columella green, dull, very closely sharply Epi- reticulated revolving dermi.s olivaceous, below which the color striate, by slight, is lines; suture moderate, umbilicus mod- white with patches or lines of revolving erate and deep. Diameter 18 mm. Puget red. Length 13, diameter 8 mm. Sound to San California Living: San Diego, California to Maz- Diego, (Orcutt). a;tla.n. SELENITES VOYANA N^ewc. Lagoon Head, Baja Ca'ifornia (Orcutt Depressed; whorls 5, convex, the last 1954); San Diego, Cal. (Orcutt 1929). declining towards the aperture and some- what flattened oi* concave above, striate; PEDIPEg LIRATA, W. G. Binney. aperture sinuate above, the lip slightly Shell globosely conical, solid, with reg- oxnanfled, its extremities joined by a ular spiral lines; spire short, with ob- callu

SPORTELLA CAL'PORNICA Dall. Cva'e conic, very thin, pellucid, shining, "Shell small, comprtssed, ruae, with a t^ci-.ate: spire acu e, attenuate; whorls yellowish epidermis; slightly arcuate, revolving very obliquely; aperture two- dorsal margin evenly arched, base con- thirds the total length, ovate, broadly cavely arcuats; inequilateral, the anterior rounded below, angled above; columella part longer, roundtd, the posterior end without fold Light horn color or grey- more blunt; teeth normal, the larger i.':h. Length 15, diameter 8 mm. right cardinal nearly parallel with the Living: Snake river, Oregon; to Clear dorsal margin, the ligamentary nymph Lake, California. obscure, the attachment for the resilium thickened and projecting; scar of the SUCCINEA OREGONENSIS Lea. mantle w.de and somewhat irregular, the Tryon, Monog T M 23, t 2 f 18. anterior addtictor scar not well distin- Keep, West Coast shells, 129. guished from it. Lon. 6, alt. 4.2, diam. Elongaled oval, thin, diaphanous, 1.5 mm. A single rather worn right valve shining;, striate; spire acute, suture well war. collected on the beach at Monterey, impressed; whorls 3, well rounded: body California, by Dall in 1S66."—Dall, U S seven-eighths and aperture two-thirds Na Mu pr 21: 885, 879 (1899), t 88 f 5. the total length; aperture ovate, one- third longer than broad, columella arcu- SUCCINEA GABBII Tryon. ate. Color deep orange or galden. Length Tryon, Monog T M 22, t 2 f 14. 9, diameter 6 mm. Keep, West Coast shells, 129. Living: Vancouver Island to Baja Cal- Elongato ovate, thin, subpellueid, ifornia. coarfexy undulaiely striate; spire long, a'u e, suture deeply impressed; whorls SUCCINEA RUSTICANA Gould. nearly 4, but slightly oblique, very con- Tryon, Monog T M 24, t 2 f 19. VvX, the last 3-4 of the totaJ length; Elongate ovate, thin fragile, diaphan- aperture small, roundly oval, columella ou.<, irregularly striate; spire elevated, wtU incurved. Light yellow. sh. Length acute, suture moderately impressed; d'.ameter 5 considers this whorls not '.', mm. Binney o, very convex; body long, i. vj'rety of S. oregonensis. oval, not inflated; aperture narrowly Living: Southeasern Oregon; north- ovai, ttree-flfths the entire length. Pale ea.;ern Ca.ifornia (W. M. Gabb). greenish or yellowish. Length 14, diam- eter 7 mm. SUCCINEA HAWKINSII Eaiid. Living: ; Vancouver Island, to n rycn. Mong T M 28, t 2 f 31. Baja California. Very narrow, sub-cylindrical, thin, ru- gosely striate; spire very short, apex SUCCINEA SILL IMA NI Bland. mamillary; whorls 2%, suture not im- Tryon, Monog T M 24-25, t 2 f 21. pi- ssed; body very long and narrow, the Kfe,«, West Coast shells, 129. ridt'f! flattened, sub-parallel; aperture Obiong-ovate; thin, coarsely striate, narrow ovate, two-thirds the total length. shining; spire short, acute, suture im- Viewed from the base exhibiting the in- presfed; whorls 3, convex, much flat- terior of the whorl to the apex, columella tene