.h~^ V V\ . H-V \>s\X ^^ — f /^ U ."S ' ^^ RESOUKCES OF CALIFORXIA. THE RESOURCES OF CALIFORNIA, COMPRISING AGPJCULTURE, MmiXG, GEOGRAPHY, CLIMATE, COMMERCE, etc. etc. AND THE PAST AND FUTURE DEVELOPMENT OF THE STATE. BY JOHN S. HITTEL. SAX FRAXCISCO: A. ROMAN & COAIPAlSrY. NEW TORK: W. J. WIDDLETON". 1863. -'/'^. > If > > > Entered according to Act of Congress, in the year, 1863, by A. Eoman & Co., Proprietors, in ihe Clerk's Office of the District Court of the United States, for the Northern District of CaUfornia. M^ORKA h MILLEK, 8TEEE0TYPKUS. C. A. ALVORD, PHINTEK. ' "". PEEFACE I UNDERTAKE to write the resources of a state, which, though young in years, small in population, and remote from the chief centres of civilization, is yet known to the furthest corners of the earth, and, during the last twelve years, has had an influence upon the course of human life, and the prosperity and trade of nations, more powerful than that exerted during the same period by kingdoms whose subjects are numbered by millions, whose history dates back through thousands of years, and whose present stock of wealth began to accumulate before our continent was discovered, or our language was formed. I write of a land of wonders. I write of California, which has astonished the world by the great migration that suddenly built up the first large Caucasian community on the shores of the N-orth Pacific ; by her vast yield of gold, amounting within thirteen years to $700,000,000, which has sensibly affected the markets of labor and money in all the leading nations of Christendom ; by the rapid development and great extent of her commerce ; by the greatness of her chief port, which at one time had more large ships at her anchorage than were ever seen together in the harbor of either Liverpool, New York, or London ; by the swift settlement of her remote distncts ; by the prompt organization of her government ; ^,^ rREFACE. bv the liberality with which the mines were thrown open and made free to all comers ; by the rush of adventurers of every color and of every tongue ; by the prices of her labor, and the rates of her interest for money double those of the other American states, and quadruple those of Europe ; by the vast extent of her gold-fields, and the facility with M they could be worked; by the auriferous rivers m which fortunes could be made in a week ; by aatediluvian streams richer than those of the present era; by beds o. lava, which, after filling up the beds of antediluvian rivers were left, by the washing away of the banks and adjacent plains, to stand as mountains, marking the position of great Treasures beneath; by nuggets each worth a fortune; by the peculiar nature of her mining industry ; by new and su-ange inventions ; by the washing down of niounta^n^s ; bv filling the rivers of the Sacramento basin with thick mud throughout the year ; by lifting a hundred mountains from their beds ; by six thousand miles of mmmg ditches ; by aqueducts less durable, but scarcely less wonderful than those of ancient Eome ; by silver mines that promise to rival those of Peru; by quicksilver mines surpassing those of Spain ; by great deposits of sulphur and asphal- tum; by lakes of borax; by mud volcanoes, geysers, and natul-al bridges ; by a valley of romantic and sublime beauty, shut in by walls neariy perpendicular and more than thiee- quarters of a mile high, with half a dozen great cascades, in one of which the water at two leaps falls more than the third of a mile; by a climate the most conducive to health, and the most favorable to mental and physical exertion-so temperate on the middle coast that ice is never seen and thin summer clothing never worn, and that January differs in average temperature only eight degrees of Fahrenhe from July ; by a singular botany, including the most splendid known group of coniferous trees, of which half a PREFACE. Vll dozen species grow to be more than two hundred and fifty feet high, and one species has reached a height of four hun- dred and fifty feet, and a diameter of forty feet in the trunk ; by a peculiar zoology, composed almost of animals found only on this coast, and including the largest bird north of the equator, and the largest and most formidable quadiTiped of the continent ; by the importation in early years of all articles of food, and then by the speedy development of agriculture, until her wheat and wine have gone to the furthest cities in search of buyers, and until her markets are unrivalled in the variety and magnificence of home- grown fruits ; by the largest crop of grain, and the largest specimens of fruits and vegetables on record ; by a society where for years there was not one woman to a score of men, and where all the men were in the bloom of manhood ; by the first large migration of eastern Asiatics from their own continent; by the first settlement of Chinamen among white men ; by the entire lack of mendicants, paupers, and alms-houses ; by the rapid fluctuations of trade ; by the ac- cumulation of wealth in the hands of men, most of whom came to the country poor ; by the practice, universal m early years, of going armed ; by the multitude of deadly affrays, and by extra-constitutional courts, which sometimes punished villains with immediate execution, and sometimes proceeded with a gravity and slow moderation that might become the most august tribunals. I write of California while she is still youthful, and full of marvels ; while her population is still unsettled ; while her business is still fluctuating, her wages high, her gold abu?ndant, and her birth still fresh in the memory of men and women who have scarcely reached their majority ; and I write of her while she still offers a wide field for the adventurous, the enterprising, and the young, who have life before them, and wish to commence it where they may have the freest career, VIU TRE F A CE. in full sight of the greatest rewards for success, and with the fewest chances of failure. The general public are aware that California is a peculiar state, and their attention has often been called to certain j^rominent points of wonder, like those to which I have just referred ; but hitherto there has been no careful at- tempt to sum up all that is known of her resources and natural history. I have undertaken that task, and the re- suit of my undertaking is in this book placed before the *'eader. I have been a Californian since 1849, and expect to be as long as I may live. All the most interesting as- sociations of mv life are connected with this state. I arrived in the country while it was still under a territorial government, and more than a year before it was organized as a state under act of Congjress. I saw the land in its original wildness, and saw society, order, trade, industry and polity developed ; and I now see about me the begin- nings and promises of science, art, literature, philosophy, and whatever can enrich or honor humanity. I have seen the state grow up, and its history is part of my life. The land-marks of its chorography, and the prominent events of its political, social, and industrial progress, mark epochs in my memory. Many of the happiest days of my life have been spent here, and^ here I hope to enjoy whatever blessings the future may have in store for me. If then I fail to do justice in my book to California, the failure will not be for any lack of love of her. Neither will it be for any lack of attention or industry. During the last nine years, I have assiduously collected every thing within my reach relative to the industry, resources, natural history and population of the state. I have looked through all the newspapers published between Crescent City and San Diego, and have examined all the books written about the country, Spanish, 1^'rench and German, as well as English. I have TREFACE. IX been in the extreme north, and the extreme south ; I have gone to both extremities by land and sea ; I have travelled through the centre of her great basin ; I am intimately ac- quainted with her richest agricultural districts ; I know something of her mining and agriculture by experience and practice ; and, finally, I have endeavored to compress into this book all the important attainable facts. Amidst so much information, there are undoubtedly some little errors ; but the fair critic, before condemning and expatiating upon minor faults, will pass judgment upon thequestion whether the book is or is not more comprehensive and instiTictive than any other, or than all others relating to the same subject. Of course, when I quote from the writings of others, I use quotation marks, and give credit according to the rules of honorable authors ; but I have adopted, without quota- tion marks, various passages from articles written by my- self, and published in different newspapers and magazines. Since the work is intended for popular use, and should be free from every thing not intelligible and interesting to the general reader, I have made no references to authorities ; and, indeed, I have drawn my information from so great a variety of sources (in many instances newspapers), that it would have been very inconvenient for me, and cumber- some to the book, to cite the authority for every statement In case, however, that the accuracy of any statement in the work should be called in question, I think that I can pro- duce in every case credible evidence, and in most cases the conclusive proof While I have drawn my material from many different sources, I claim as much originality as is possible for so comprehensive a collection of facts, in so many and so distinct branches of knowledge. J. S. H. San Francisco, March, 1862. ijstdex of chapters. Chapters. Page I. Chorografhy 1 II. Climate 19 III. GEOLOaT 47 I Y. SCEXERY 72 Y. Botany 91 VI. Zoology 108 Yn. Agriculture 151 Vin. Mrs-LXG 238 IX. Other Branches of Intdustry 30^ X. Commerce , 326 XI. Constitution and La"ws 349 XII. Society 359 XIII. Topographical Xaites 422 XI Y. The Past and Future Development of the State 431 ■\ IXDEX OF SECTIO^STS. Chorography — Chap. I. Sec Page 1. General Remarks 1 2. Coast Mountains 2 3. Coast, Peaks, and Passes. . 3 4. Coast Rivers 5 5. Coast Lakes 6 6. Capes 7 7. Islands 7 8. Bays and Harbors 7 9. Sacramento Basin 10 iU. Rivers of the Sacramento Basin 12 11. TuleLand 13 12. Sierra Xevada 13 13. Peaks and Passes of the Sierra I'l 14. Lakes of the Sierra 15 15. Plateau of the Sierra Ne- vada 15 16. Klamath Basin 16 17. Utah Basm 16 18. Colorado Desert IT 19. Area of the State 18 Climate — Chap. IL 20. General Remarks 19 21. Temperature of the Middle Coast 20 22. Clear Days 25 23. The Sirocco 25 24. Temperature of the South- ern Coast 27 25. Sacramento Basin 27 26. Comparative Tables 28 27. Rain 30 28. Dryness of Chmate 38 29. Length of Days 39 30. Thunderstorms 39 31. HaU 40 32. Earthquakes 40 33. Saud-Storms 45 Geolo&y — Chap. III. Sec. Page 34. General Geological Charac- ter 47 35. Diluvium 48 36. Gold 50 37. Auriferous Lodes 51 38. Placers 52 39. Mineralogy of Gold 54 40. Silver 60 41. Platinum 61 42. Quicksilver 61 43. Copper 62 44. Coal 63 45. Asphaltum 63 46. Other Minerals 65 47. Artesian Wells 67 48. Paleontology 69 49. Relics of Early Humanity. 70 50. Mineral Springs 70 51. Cortes Shoal 71 Scenery — Chap. IV. 52. Introductory 72 53. Coast VaUeys 72 54. Tosemite Valley 73 55. Mammoth Tree Groves. ... 78 56. Geysers 84 57. Mud Volcanoes 85 58. Santa Cruz Ruins 86 59. Mirage 86 60. Caves 88 61. WaterfaUs 88 62. Solfataras 89 63. Mount Shasta 89 Botany — Chap. V. 64. Peculiar Fauna and Flora. . 91 65. Distribution of Plants 92 60. Superioritv of Conifers 92 67. Redwood." 92 XiV INDEX OF SECTIONS. Sec. Page 68. Pines 9^ 69. Firs 96 70. Cedars 96 11. Yew aud Xutmeg 97 72. Laurel 97 73. Madrona 98 74. Manzanita 98 75. Ceanothus 99 76. Oaks 99 77. Buckeye 101 78. Sycamore 101 79. Pitahaya 101 80. Yucca 102 81. Mezquit 102 82. Miscellaneous Trees and Shrubs 102 83. Poison Oak 103 84. Amole 104 85. Nutritious Herbage 104 86. 87. 88. 89. 90. 91. 92. 93. 94. 95. 96. 97. 98. 99. 100. 101. 102. 103. 104. 105. 106. 107. 108. 109. 110. 111. 112. 113. 114. 115. 116. Zoology — Chap. VI. General List 108 Bears 108 Panther and Wild-Cat Ill Wolves and Foxes 112 Badger, etc H-l The Squirrel Family 115 The Rat Family 120 The Deer Family. 121 The Hare Family 124 Aquatic Animals 125 Vultures 1^8 The Eagle Family 129 Owls 130 Road-runner 130 Woodpecker 131 Humming-Birds 132 Flycatchers 133 Singers 133 Scratchers 134 Waders 137 Swimmers 137 Fishes 14:0 Salmon 1-10 Halibut 141 Turbot 142 Sole 142 Mackerel 142 Rock-Fish 142 Sturgeon 143 Jew-Fish 143 Sun-Fish 144 Sec. 117. 118. 119. 120. 121. 122. 123. 124. 125. 126. 127. 128. 129. 130. 131. 132. 133. 134, 135. 137. 138. 139. 140. 14L 142. 143. 144. 145. 146. 147. 148. 149. 150. 151. 152. 153. 154. loo. 156. 157. 158, 159. 160, 161. 162. 163. 164. 165 Pago Green-Fish 144 Sea-Bass 144 Sheepshead 144 Smehs 144 Anchovies 145 Sardine and Herring 145 Viviparous Fishes 145 Fresh- Water Fishes 146 Shell-Fish and Crustaceans . 146 Reptiles 147 Honey-Dew Aphis 149 Agriculture — Chap. VII. General Remarks 151 Agricultural Districts 153 Agricultural Produce 100 Rotation of Crops 161 Ploughing 162 Advantages, etc 162 Fences 163 Barley 167 Wheat 170 Oats l"?? Maize l'''^ Potatoes 178 Hay 179 Tobacco, Cotton, Rice 181 Hop 181 Kitchen Vegetables 182 Fruit 184 Apples 186 Peaches 188 Pears 189 Apricots and Plums 189 Olives 190 Oranges 191 The Grape 193 Wine-making 201 Berries 207 Ornamental Shrubs 209 Pests of the Farmer 211 NeatCattle 212 Spanish Cattle 212 Rodeos 214 Brands 217 Early Maturity of CaUfornian Cows 218 Corral and Reata 219 Occasional Starvation 219 Lnported Cattle 220 Dairies 222 Soanish Horses 222 IXDEX OF SECTIONS. XV Bea Page 166. Horse-breaking 224 167. Blood-horses 228 168. Mules 229 169. Camels 229 170. Sheep 229 171. Swme 233 172. Poultry 233 173. Bees [[[[ 235 174. Silkworms 237 Mining — Chap. YIII. 175. Chief Industry 238 176. Metals obtained 238 177. Gold Mines 238 178. Placer Mines 241 179. The Sluice .' 243 180. Amalgamation 246 181. Cleaning up 249 182. Riffle-bars *.'.'. 250 183. Double-Sluices 252 184. Eock-Sluices 252 185. Hydrauhc Mining 253 186. Blasting 256 187. TaU-Sluice 256 188. Tunnel-Sluice 257 189. Ground-Sluice 257 190. Long-Tom 257 191. Cradle .' 258 192. Pan 262 193. Dry "Washing 264 194. Dry Digging 264 195. Puddling Box '. . 265 196. Quicksilver Machine 265 197. Tunnel Alining 266 198. Shafts 267 199. River Mining 268 200. Beach Mining 269 201. Mining-Ditches 270 202. Prospecting 271 203. Quartz Mining 272 204. Distribution of Gold in Quartz 273 205. Prospecting Quartz Rock. . . 275 206. The Divining Rod 277 207. Quarrying Quartz 277 208. Arastra 278 209. Chilean MiU 280 210. Stamps 280 211. Separation 281 212. Sulphurets 284 213. Chief Quartz Mills '..*.' 284 214 Silver Mining 285 Sec. Page 21 o. Quicksilver Mining 286 216. Platinum 287 217. Del Xorte and Klamath .. . 288 218. Siskiyou 289 2 1 9. Trinity and Shasta 289 220. Plumas and Sierra 290 221. Yuba and Butte 294 222. Xevada and Placer 295 223. El Dorado and Amador 296 224. Calaveras and Tuolumne. . . 298 225. Mono and Mariposa 301 226. Fresno, etc 303 Other B ranches of Ixdustey — Chap. IX. 227. High Wages 304 228. Lumbering 305 229. Fishing 313 230. Hunting ...\ 317 231. House-building 320 232. Furniture, etc 323 Commerce — Chap. X. 233. General Advantages 326 234. Tributary Population 327 235. Imports 330 236. Exports " . ' 330 237. Shipping 332 238. Unsteadiness of Business . , 333 239. Insolvencies 334 240. Interest of Money 335 241. Speculation in Land 337 242. No Paper Money 337 243. Opportunities for Invest- ment 338 244. Assurance 347 Constitution and Laws — Chap. XL 245. Outlines of Constitution. .. . 349 246. Inferiority of Colored Per- sons 350 247. Law Favorable to Debtors . . 350 248. Tenure of Land 352 249. Ownership of Minerals. . , . 354 250. Titles of Mining-Claims 354 251. Marriage 353 Society — Chap. XII. 252. Population 359 XVI INDEX OF SECTIONS, Sec, 253. 254. 'loo. 256. 257. 258. 259. 260. 261. 262. 263. 264. 265. 266. 267, 268. 269. 270, 271. 272. 273. 274. 275, 276. 277. 278. 279. 280. 281. 282. 283, 284, Page ] Nativities 361, Liberal Tone of Society ^6^ i Publicity of Life 364 j Amusements 365 Luxurious Living 366 | Health 366 | Proportion of Sexes 368 Education 369 Vigilance Committees 370 Lj-iich Executions 373 Squatter League 374 Anti-Chinese Mobs 3 • 55 55 0 • 56 C 57 > 57 a. ■— > 58 57 54 0 0 p 51 AVER- AGE. LATITUDE. Sau Francisco . . . 54 37°48' Benicia •47 52 53 57 59 67 67 66 64 62 54 47 58 58 03 Sacramento 45 48 51 59 67 71 73 73 66 64 52 45; 59 38 34 Fori; Miller 4T 53 56 62 68 83 90 83 76 67 55 48 1 66 37 Fort Reading . . . 44 49 54 59 65 77 82 79 71 62 52 44! 62 40 28 Fort Yuma 56 58 66 73 76 87 92 90 86 76 64 55 73 32 43 New York 31 30 38 47 57 67 73 72 66 55 45 34 51 40 37 New Orleans .... 55 58 64 70 75 81 82 82 78 70 62 55! 69 29 57 Steilacoom '-{8 40 40 42 42 48 46 5560 53:58 64 62 63 62 57 57 52 50 45 44 39, 40' 50 49 47 10 51 29 London 37 Citv of Mexico . . . 52 54 61 63 66 65 65 64 64 60 55 52 60 19 26 Naples 46 47 51 56 64 70 76 76 69 61 53 49) 60 40 52 Funtiial 60 60 62 63 64 67 70 72 72 67 64 6O1 65 32 38 Honolulu 71 72 72 74 76 77 78 79 78 76 74 73 75 21 16 Jerusalem 47 53 60 54 66 71 77 72 72 60 58 47 62 31 47 Canton . . 52 00 62 70 77 81 83 82 80 73 65 57j 69 23 08 Nagasaki 43 44 50 61 69 77 80 83 78 66 53 41' 62 32 45 By the study of this table, we can form an excellent idea of the temperature of the different portions of the state, as com- pared with each other, and as compared with those of some other countries. So far as we know^, San Francisco has the most equable and the mildest climate in the world. "Within the tropics there are, no doubt, many places which have a more equable temperature, but it is the equability of intense heat. Funchal, on the island of Madeira, has probably the mildest climate in the Avorld, but in equability it is inferior to San Francisco. Benicia is thirty miles from the ocean, and has a warmer summer and a colder winter than the immediate coast. Sacramento has the climate of Xaples and Jerusalem through- out the year : its summer being the same as that of Xew York, but its winter fourteen degrees warmer. Fort Reading and ISTagasaki have nearly the same figures. Fort Yuma, in the Colorado Desert, in latitude 32° 45', is w^armer than New Or- leans, in 29° 57'. A railroad, one hundred and eighty miles long, running eastward from Oakland, a suburb of San Francisco, passing 30 R K S O U R C E S OF CALIFORNIA. through Stockton and Sonora, near the Mammoth Grove of Mariposa and the Yosemite valley, to the summit of the Sierra Nevada, would ennble the people near the line to place them- selves, every summer's day, in any tolerable degree of heat or cold. Fourteen miles west of Oaldand is the ocean-beach, where a chilling wind blows without ceasing. Going from the coast, the traveller would gradually get into a warmer clime, until, in Stockton, he would find the thermometer indicating 100°, most of the summer noons ; and proceeding up the sides of the Sierra, he would gradually rise into greater cold, to the eter- nal frost on the summit. A branch road running south to Fort Yuma would enable the traveller to enjoy almost as great a variety of temperature in the winter. § 27. Ram. — Nearly all the rain in California falls between the first of November and the first of June — the period called the " rainy season," as contradistinguished from the " dry sea- son," which occupies the remainder of the year. Those names, however, when applied to any special season, do not signify an unchangeable number of months, but rather the term dur- ing which the rain falls or the dry weather lasts. Thus, we say that the rainy season of 1858-59 began in October, be- cause in that month the first heavy rains fell ; the rainy season of 1855-56 did not begin until December; the dry season of 1857 began in March; and so forth. The rainy season is so called, not because the rain falls then continuously, but because it does not fall at any other time. There are occasional show- ers in June, July, August, and September, but they are rare and light. The following table gives the average amount of rain, in inches, which falls during the four seasons of spring, summer, autumn, and winter, at various places in California, as com- pared with the amount which falls in other places in the United States CLIMATE. 31 PLACES. San Francisco . . Sacramento . . . . Fort Ro thousand five hundred feet above the sea, is from twice to thrice as great as in Stockton, onlv seventy miles distant, at the sea-level ; 9* 34 RESOURCES o'f CALIFORNIA. and the same difference is observed between Nevada and Mar rysville, which bear similar relations of distance and elevation to each other. The statistics given in the preceding part of this section relative to the amount of rain-fall at San Francisco, are intend- ed to represent ordinary years, such as all those between 1847 and 1860. But the winter of 1861-62 proved to be an ex- 1 traordinary season, the amount of rain being double that whic has fallen in any other winter since the American conquest. The average rain-fall during the winter months at San Fran- cisco is about 12 inches; whereas, between the 1st of Novem- ber, 1861, and the 1st of February, 1862, 37 inches fell in San Francisco, and during the same period 101 inches fell in So- nera, Tuolumne county. During the four months from the 1st of November, 1861, to the 28th of February, 1862, inclusive, 45.53 inches of rain fell in San Francisco, viz. : 4.10 in Novem- ber; 9.54 in December; 24.36 in January; and 7.53 in Feb- ruary. This rain caused a great flood, which did much damage along most of the rivers, and especially in the Sacramento Basin, where Sacramento City, Stockton, Marysville, and nu- merous minor towns, w^ere completely inundated, and the whole central part of the basin, including an area one hundred and fifty miles long and twenty miles wide, was converted into a great lake, which covered the land to a depth varying from two to ten feet for more than a month. The long dura- tion of the flood, its great height, and the vast damage which it did, Avill render it an epoch in the history of the state, and make it well worthy of study, especially so far as relates to the Sacramento Basin, where the most serious injury was done — that basin extending north and south from Mount Shasta to the Tejon Pass, a distance of four hundred and fifty miles ; and east and west from the summit of the Coast Ranofe to that of the Sierra Nevada, a distance of one hundred miles. These two ranges unite at the two ends of the basin, which has its outlet in the middle, where the Sacramento from the north and the San Joaquin from the south, having united their waters in CLIMATE. 35 latitude 39°, break through the Coast Moimtahis to reach the Pacific. It may be said that the watei-s of these streams, aftei their union, pass through three straits; one at the Golden Gate, one hundred feet deep and a mile wide ; one at the straits of Carquinez, fifteen feet deep and three-quarters of a mile wide, thirty-five miles from the ocean ; and one near the head of Suisun Bay, half a mile wide and ten feet deep. The Golden Gate and the straits of Carquinez aiford an abundant outlet for all the water from the interior, but not so with the pass at the head of Suisun Bay. The land at this place is low — not more than six or eight feet above low-water mark — for a width of three miles, beyond which there are hills, which prevent the spreading of the water to a greater distance. The river is shallow and crooked ; the banks lined with bushes and covered ^vith tules, which obstruct the passage of the water in time of flood. During the flood of January, 1862, there was very little perceptible increase in the height of the water in San Fran- cisco and Suisun Bays above the level of ordinary high tide. But there was no flow of the tide ; a continual ebb of thick, muddy water, poured out at the Golden Gate for weeks to- gether, discoloring the sea to a distance of forty miles from laud. In the bays the water became almost fresh, and the planted oysters were killed by it in tbeir beds near Oak- land. "We may presume, since thirty-six inches of water fell at San Francisco from November to January inclusive, of 1861- '62, that the same amount fell in all the low lands of the Sac- ramento Basin, nearly one-half of its area. We may presume further that the amount which fell at Sonora is a fair repre- sentation of the amount which fell on the Sierra Xevada, one- half of the area of the basin. But possibly snow, which has not yet melted, formed one-third of the snow and rain which fell on the Sierra Xevada. It is not, therefore, necessary to take any account of that third, in this consideration of the flood of 1862 — v\'ritten, as it is, before the waters have g:oue down. B6 R E S O U B C E S OF CALIFORNIA. There was, then, a fall of three feet of water over an area of about twenty-two thousand five hundred square miles, and a fall of eight and a half feet over an area of fifteen thousand square miles. This would give us an average of five and one- fourth feet over an area of thirty-seven thousand five hundred square miles. The first foot was absorbed by the sand and earth, dried during a very arid summer and fall; and then there were four feet of Avater to escape through an outlet half a mile wide, from an area nearly as large as England, or the state of Ohio. The outlet proved insufticient: the waters heaped them- selves up in the lowest part of the Sacramento Basin, the size of which low portion I have already given as one hundred and fifty miles long and twenty wide, or an area of three thousand square miles. Now, four feet of water over an area of thirty- seven thousand five hundred square miles, will, if collected within three thousand square miles, form a body forty-eight feet deep ; and that figure represents the amount of water that had to escape through the Sacramento River, below the mouth of the San Joaquhi. It is to be observed that, as the outlet of the Sacramento Basin is in its centre, so the freshets come simultaneously from the north and from the south. The rains fall along the whole length of the Sierra Nevada at the same time ; and as the mountain-streams are short and swift, they pour down their floods immediately and all together. Such are the circumstances which contributed to the great flood of 1862, and may contribute to other floods in the future. During January, 1862, 24.36 inches of rain fell in San Fran-' Cisco, according to records kept by Thomas Tennant, Esq. ; 8.66 inches fell in Sacramento, according to Dr. T. M. Logan ; 37.79 inches fell at Downieville, according to Dr. T. R. Kibbe ; and 33.79 inches fell in Grass Valley, according to Mr. Atwbod. I presume that all these figures are correct save those for San Francisco ; and while I admit the care and accuracy of Mr. Tennant, I must suspect that somebody played tricks with his gauge, upon which he could not keep a constant watch. CLIM ATE. 37 Between the 1st of November, 1861, and the 1st of Febru- ary, 1862, 37 inches of ram fell in San Francisco; 75.69 in Grass Yalley; 79.28 in Downieville ; 101 in Sonora; 42 inches of rain and 50 feet of snow (the siiow probably equalling 60 inches of water) on the summit of the Sierra N^evada at Hen- ness Pass ; and 34 feet of snow and a great amount of rain (not measured) on the summit of the same range at the Big- Tree Road. The observations at the Henness Pass were kept by Mr. S. K. Dunham; those at the Big-Tree Road by Mr. Richey. There have been " rainy seasons" in California which passed without rain ; and the grass, receiving no moisture in winter, spring, or summer, has remained brown for a period of eigh- teen months. • But no drouo-ht — more fearful than the worst of floods — has visited the country during the last twenty years, nor have we any accurate information about those that are re- ported to have happened before that time. So long as the wind blows from the north, we expect fair weather ; when it veers to the south, rain may be expected, usually within forty-eight hours. Sometimes, after a rain, the clouds near the earth move toward the south, while those higher up are going in the contrary direction : in such case, more rain may be expected. In no part of Europe or the Atlantic states can the state of the weather be predicted or guessed with so much reasonable confidence as in California. Here it is almost a certainty that nineteen days out of twenty in summer and fall, and that ten out of twenty on an average in winter and spring, will be clear and warm. Many circum- stances of value, in furnishing grounds for predicting the state of the weather in other regions, are of no use here. In the Mississippi valley, for instance, three consecutive frosty morn- ings are considered as an almost certain indication of rain ; but in California, frosts have no such significance : for a dozen may occur successively in the coast valleys or foot-hills of the Sierra N^evada, and nobody expects rain the more on that account. 38 RESOURCES OF CALIFORNIA. § 28. Dryness of Climate. — The small amount of rain dur- ing the winter, the entire want of it during the summer, the warmth of the sun, and the great number of cloudless days, render the climate a very dry one. As one conseqence or ac- companiment of our dry climate and clear sky, it may be worth while to observe that near the ocean the clouds are rarely pic- turesque or sublimely beautiful. The magnificent sunsets, where the god of light goes down amid curtains of gold and crimson— those high-piled banks of clouds which adorn the heavens before and after thunder-showers, in the Mississippi valley — are never seen near the coast. Dew is very rare or slight over a great part of the state. During the summer and autumn, many of the rivers sink in the sand soon after leaving the mountains in which they rise ; the earth is dry and baked hard to a depth of many inches or even feet ; the grass and herbage, except near springs, or on swampy land, are dried up, and as brown as the soil on which they grew. It has been said that very hot days are less oppressive in Califoi-nia than equal heat in the Eastern states, because the cool nights serve to invigorate the system, and the extreme dryness of the climate favors the evaporation of sweat, and thus keeps the body cooler than in districts where the earth is ahvays moist. Evaporation is so rapid, that a beefsteak hung up in the air vrill dry before it can commence to putrefy. A dead rat thrown into the street, where its body is crushed by wagon-wheels so that its viscera are exposed to the air, Avill "dry up," and its stiff hide and meat will lie during a whole summer in a mummy-like condition. In many places, steel may be exposed to the night air for weeks without getting a touch of rust. It is common to ascribe the effects of the dryness of the atmosphere to the "purity" of the air; but it is rather the absence of moisture. I know no reason for supposing that, apart from its dryness, the air in California is purer than in any other pai't of the continent. It may be, however, that tl^e CLIMATE. 39 constant decomposition of animal and vegetable manner, lying on wet ground, under a hot sun, causes the air in other states to be filled with such gases as are not set free to an equal 'extent here. In May and June, all California " dries up" — the rivers, the brooks, the springs, the ditches, the vegetation — and, with them, manv of the resources of the countrv. § 29. Length of Days. — The shortest day in the year, the 20th of December, measures nine hours and four minutes be- tween sunrise and sunset at Crescent City, and ten hours at San Diego ; Avhile the longest day, the 20th of June, measures fifteen hours and seventeen minutes on the southern border, and fourteen hours and nineteen minutes on the northern bor- der of the state — or, measuring from the beginning of twilight in the morning to the end of twilight at night, the day meas- ures nineteen hours and fortv-seven minutes on the Siskivon Mountains, and seventeen hours and forty-three minutes at Fort Yuma. § 30. Thunder- Storms. — Thunder-storms are very rare in California. Lightning is not seen more than three or four times a year at San Francisco, and then it is never near, but far off, playing about the peak of Mount Diablo. Thunder is still more rare. Indeed, many persons have been here for years, and cannot say that they have ever seen the one or heard the other. During eleven years' residence in the state, I have never seen a brilliant flash of lightning or heard a loud clap of thunder. Thunder-storms are sometimes witnessed high up in the mountains, and in the Great Basin ; vei-y rarely in any of the low land of the state. In May, 1860, a house in Sonora was struck by lightning; and in February, 1861, three vessels in Humboldt Bav were struck in the same manner: and, though there were persons in the house and on all the vessels, no serious injury was done to either person or prop- erty in any case. On the 2oth of May, 1860, a Chinaman was 40 RESOURCES OF CALIFORNIA. killed by lightning near the Lexington House, on the Coloma road, in Sacramento county. The weather never has that peculiar condition which isolates everybody electrically, and then fills them with electricity. In New York, on a dry winter evening, a man dressed in wool- len and shod in w^oollen slippers, after sliding along on the carpet a few steps, will accumulate so much electricity, that when he thrusts his finger at another person, a visible spark will fly off, and he can light gas with it ! But this amusing experiment, common as it is in the Eastern states, never has been successful, and probably never will be often practised, here. § 31. Hail. — Hail is a rarity; and instead of falling in July and August, as is usual in the Eastern states and Europe, it is seen in California only between February and May. On the 10th of May, 1856, a storm of hail-stone.«, some of them weigh- ing twelve pounds each, visited a small district at Butte Creek, in Shasta county. It has several times happened that hail- stones more than an inch in diameter have fallen in the Sacra- mento valley. The Aurora Borealis is seldom seen in California, perhaps not more than half a dozen times within the last ten years. The aurora of the 28th of August, 1859, seen over a great part of the world, was plainly visible in this state. § 32. Earthquakes. — Earthquakes are common in some parts of California, and especially at San Francisco, Los An- geles, and near the Tejon Pass, at the southern junction of the Sierra Nevada and Coast Mountains. They are rare at Sacra- mento, Marys ville, Vallejo, and Xapa. As a general rule, they are less frequent and less severe in the northe'-n than in the southern part- of the state. The vicinity ot Humboldt is more often shaken than any other place north of the bay of San Francisco. About a dozen earthquakes are felt in a year at different places in the state ; not so mnny at one place. Most CLIMATE. 41 of the shocks are so slight as to pass unnoticed by a great majority of the people; and there are persons who have re- sided six or eight years in San Francisco, and many who have resided ten years in other parts of the state, and say they have never felt an earthquake. Xo person has been hurt, nor has any strongly-built house been injured, by an earthquake in Cahfornia, north of latitude 35°, since the American conquest. Several brick walls have been cracked in San Fi'ancisco, but they were weak structures, built on "made ground," and would perhaps have cracked by settling, of their own weight. On three or four occasions, large four-story houses have been so much shaken, that the mmates have run out in great alarm ; but on examination it was found that the buildino^s were unin- jured, even in the slightest perceptible manner. On one such occasion, a friend of mine, who thought his life in great danger, and ran to save it, observed before he left his room that the water was splashed out of his basin by the movement of the house. The basin was of earthen ware, about fifteen inches in diameter at the top, six inches deep, half full of water, and it stood on an ordinary wash-stand. He sup- posed that, with another such a shock or two, the building must be in ruins ; and he was verv much astonished the next morninoj to find that there was not the slio-htest crack in the plastering. His room was in the fourth story of a brick hotel. It seems that the whole building: had moved to^rether. The fear of earthquakes prevents the erection of high struc- tures for show ; and, for this reason, there is not a tall steeple in San Francisco. The largest churches have been commenced on such a plan that they might be crowned with lofty spires, but it was thought more prudent to leave them with low tow- ers. The same motive induces manv wealthv families to reside in wooden houses, which are considered better fitted to resist the shocks of earthquakes. These wooden houses, it must be kept in mind, are not "framed" with mortices and tenons, as large wooden houses are usually erected in the Atlantic states, but are " Chicago frames," held together with nails. This 42 KESOUKCES OF CALIFOKNIA. Style of building, though introduced solely because of its ch'eapness and simplicity, is considered by far the most secure against earthquakes. No earthquake felt at San Francisco since 1846 has been more severe than one which visited Buffalo, New York, in 1857, as described in the American Journal of Science and Art for September, 1858. On the 10th of July, 1855, an earthquake cracked the walls of twenty-six houses m Los An- geles; but no wall was thrown down, nor was any person injured. Most of the earthquakes of California are confined to very small districts. Thus, not more than one in ten of those felt in San Francisco is perceived in Sacramento. The most ex- tensive Californian earthquake of which we have any record was that of January 9th, 1857. It shook the earth from Fort Yuma to Sacramento, a distance of five hundred miles, being most severe at Fort Tejon, about half way between these two points. Loud noises, either rumbling or like explosions, were heard to accompany the shock at Tejon, San Bernardino, Visa- lia, and in the Mojave valley. The waters of the Mokelumne River were thrown upon the banks so as almost to leave the bed bare in one place. The current of Kern River was turned up-stream, and the water ran four feet deep over the bank. The water of Tulare Lake was thrown upon its shores ; and the Los Angeles River was flung out of its bed. Li Santa Clara valley the artesian wells were much affected: some ceased to run, and others had an increased supply of water. Near San Fernando a large stream of water was found run- ning from the mountains, where there was no water before. In San Diego, and at San Fernando, several houses were thrown down ; and at San Bueueventura the roof of the Mis- sion Church fell in. Several new springs were formed near Santa Barbara by the shock. In the San Gabriel valley the earth opened in a gap several miles long ; and in one place the river deserted its ancient bed, and followed this new open- in o-. In the valley of the Santa Clara River there were large CLIMATE. 43 cracks in the earth. A larGje fissure was made in the western part of the town of San Bernardino. At Fort Tejon the shock threw down nearly all the buildings ; snapped off large trees close to the ground, and overthrew others, tearing them up by the roots ; and tore the earth apart in a fissure twenty feet wide and forty miles long, the sides of which rent then came together w4th so much violence, that the earth was forced up in a ridge ten feet w^de and several feet high. At Reed's ranch, not far from Fort Tejon, a house w^as thrown down, and a woman in it killed. In September, 1812, on a Sunday, an earthquake threw down the Mission Church at San Juan Capistrano, in latitude 33° 20', and thirty persons w^ere killed. The church at Santa Inez, in Santa Barbara county, was thrown down on the same day; but the shock, according to report, was an hour later than that at San Juan Capistrano, and there was nobody in the church when it fell. At the same time the sea receded a long distance from the ordinary place of the water's edge on the beach of Santa Barbara ; and the people there, knowing that it would soon rush upon the shore, fled to the higher ground, and by that means alone saved their lives. These reports made about this earthquake of 1812, to Dr. J. B. Trask, by old residents, have never been contradicted, though published six or eight years ago. The old Mission Church at Santa Clara was thrown down by an earthquake in 1818. On the 15th of May, 1851, a severe shock was felt in San Francisco. Windows w^ere broken ; mer- chandise was thrown down from shelves in stores ; and vessels in the harbor rolled heavily. On the 26th of ISTovember, 1858, nearly every brick building in San Jose was injured by an earthquake. On the 3d of July, 1861, Amador valley, in Ala- meda county, was severely shaken. Adobe houses were seri- ously injured, chimneys toppled down, furniture was flung from side to side of the houses and much broken, and men in the fields were thrown dov/n. A severe shock of an earthquake was felt at Fort Yuma and 44 RESOURCES OF CALIFORNIA. vicinity on the 29th of November, 1852. The low grounds near the Colorado cracked open with long, wide fissures, from which water, sand, and mud, spouted up. The fissures were in some places so large, that they turned the river from its course ; and the change was so sudden, that great multitudes of fish were left to die in the mud. At the same time, the mud-volcanoes of Lower California, distant forty-five miles southwestward from Fort Yuma, resumed their activity ; for, although tliere is no record of their previous action, yet they probably existed before. A pool of hot, sulj^hurous water had been observed at the place by Americans since 1849. Imme- diately after the shock of 1852, the officers at Fort Yuma saw a great body of steam shoot up at least one thousand feet in the desert to the southwest ; and when, soon afterward, some of them went out to examine into the cause of it, they found the mud-volcanoes on the site of the old pool, throwing up steam, boiling water, and mud, very much like the salses far- ther north. Earthquakes, according to the common theory of Califor- nians, are electrical in their origin, or closely connected with electrical influences. Many of the strongest shocks have been preceded by a condition of the atmosphere veiy similar to that which precedes thunder-storms in other lands. When the weather is sultry and oppressive in San Francisco, people say, " Look out for an earthquake !" And it usually comes — per- haps so faint as to be barely perceptible, and sometimes not until several hours after a change in the weather. The frequency of earthquakes in California has caused a number of persons, perhaps a hundred or more, to leave the state, and return to their former homes on the Atlantic side of the continent. And yet there they are in more danger from lightning than here from earthquakes, for there are fifty killed by lightning in the Mississippi valley for one killed by an earthquake in California. A year rarely passes that a dozen persons are not struck by thunderbolts within three hundred miles of St. Louis. [See Appendix, p. 464.] CLIMATE. 45 § 33. Sa?id-Storms, — In the Colorado Desert, and in some other districts in the southern part of the state, sand-storms, similar to the simooms of Africa, but not so dangerous, occa- sionally occur. The sand, which forms the greater portion of the soil, unprotected by sod, vegetation, or moisture, is swept away in dense clouds by every high wind, and carried many miles, a terror to man and beast. The storm stops the trav- eller, because he dare not open his eyes to the little flinty par- tides ; nor can he eat, for the dust covers his food and fills his mouth: and even in the most tightly-built houses the sand penetrates and fills the air. A newspaper correspondent speaks thus of a Colorado sand- storm : "Should the traveller happen to encounter a sand-storm, however, he may not get along so smoothly. A huge, black cloud, rising from the western horizon, warns him of its ap- proach. Rapidly it spreads over the sky, darkens the sun, and the fine particles of sand are swept before the gale in a dense and sufibcating cloud ; even the larger gravel and peb- bles are sometimes lifted from the plain and carried like hail before the force of the blast. The horses are blinded, para- lyzed with fear, and no urging can induce them to go forward. Were it otherwise, to go on would be folly ; the road and sun are hid from view ; no landmarks by which to be guided — safety bids you remain. The traces are unhitched, and the horses tethered to the wagon ; the only course is to securely fasten down the sides to the wagon-top, and wait with what patience one can command until the storm has passed, which will be, doubtless, in from six to ten hours. "Once the sta^e encountered a sand-storm while within three hundred yards of a station ; the horses could not be in- duced to move, and there was no remedy but to stay by them till the gale had spent its force, though the station was even in sight. " I have found such a storm sufficiently disagreeable while housed by the river-side, the fine sand penetrating everywhere, 46 RESOURCES OF CALIFORNIA. and have no ambition to encounter one upon the central des- ert. Luckily, they are not very common in the severest aspect; in summer, quite rare." Note. — The chief writers upon the Meteorology of California have been, Dr. Henry Gibbons, of Alameda, and Dr. T. M. Logan, of Sacramento, whose writings have been published in the books of the Smithsonian Institute, and in the newspapers of San Francisco and Sacramento. GEOLOGY. 47 CHAPTER III. GEOLOGY. § 34. General Geological Character. — California, geologi- cally considered, belongs chiefly to the paleozoic and tertiary epochs. The carboniferous rocks are wanting, or their exist- ence in the state is confined to a very small district, and has not been demonstrated even there. A tertiary sandstone, some of which is metamorphic, having lost its original stratification under the influence of intense heat, underlies the valleys of the Sacramento, the San Joaquin, and the coast, and is seen in the Coast Mountains, the Great Basin, and the Colorado Desert. Granite occupies the higher portions of all the mountainous districts, and considerable portions of the Great Basin and the borders of the Colorado Desert, The scarcity of stratified rocks is plainly discoverable by the traveller in the number and ruggedness of the mountains; only primary, eruptive, and metamorphic rocks make such steep hill-sides. The thinly- stratified rocks, with intervening layers of clay, are soon worn down by the water into gentle slopes, and covered with fertile soil, every foot of which may be turned over by the plough, and with profit. Such is not the character of California, nearly all of which is primary or metamorphic. Many rocks besides granite and tertiary sandstone appear in irregularly-distributed patches. About Mounts Shasta and Lassen, Castle Peak, the Marysville Buttes, in the plateau of the Sierra Xevada, the Great Basin, and the Colorado Desert, there are considerable tracts of basalt, lava, trap, and trachyte ; and in other places there are small tracts. Some very remark- able hills of basalt, called "Table Mountains," are found in the 48. RESOURCES OF CALIFORNIA. Sierra Nevada. Tlie largest of these is in Tuolumne county, about three thousand feet above the sea, and one hundred miles eastward from San Francisco. It is thirty miles long, tliree hundred to eight hundred feet high above the surround- ing country, and about a quarter of a mile wide, in many places less. The basaltic formation is evident at a distance, from the perpendicularity of the sides near the top, and the flatness of its summit, gently descending toward the west. Along the sides of the Sierra Nevada, near the line of separation between the sandstone of the valley and the granite of the higher parts of the Sierra, are found various other rocks, among which slate, quartz, and limestone, are prominent. The slates are usually soft, their cleavage often perpendicular to the horizon. Limestone is abundant about two thousand feet above the sea, between latitudes 37° 30' and 39°. It is all metamorphic, and some of it is a fine marble, which may prove of value for stat- uary. Most of it is gray in color. Metamorphic limestone is also found near Santa Cruz, near New Almaden, at Monte Diablo, and in Shasta and Siskiyou counties. It is said that some stratified secondary limestone has been found in Shasta county, but this is a matter of doubt. No secondary coal has been found in the state. Tertiary coal, much of it a lignite, has been found at various places in San Diego, Santa Clara, Alameda, San Francisco, San Mateo, Contra Costa, and So- noma counties, and much money has been spent in opening veins. § 35. Diluvium. — The Sacramento and San Joaquin valleys are covered with a diluvium from four hundred to fifteen hun- dred feet deep. It is composed of alternate layers of sand, gravel, and clay. The most complete information which we have as to the nature of this diluvium is given in the report of the boring of an artesian well, one thousand feet deep, at Stockton. This is, I believe, the only artesian well in the Sac- ramento Basin ; at least, it is the most notable one. An at- tempt was made to bore an artesian well in Sacramento, but the auger struck a stratum of boulders about four hundred feet GEOLOGY. 49 from the surface, and was unable to pass through it. The fol- io wingr is a statement of the different strata encountered in the Stockton well, and the thickness of each in feet, beginning at the surface : Black loam, 6 ; red clay, 6 ; dark-red clay and sand, 18 ; blue clay, mica, and sand, 10; blue clay, hard, highly stratified, 4; blue clay, mica, and sand, 3 ; blue clay, hard, and highly strati- fied, 4 ; green sandstone and clay, very hard, 29 ; blue clay, sand, and gravel, slightly impregnated with gold, 2 ; blue clay, sand, and gravel, 18 (100) ; green sandstone, clay, and mica, hard, 15; fine gravel, 5; gray quicksand, 15; blue clay, 8; gray sand and clay, 27 ; dark-blue clay and sand, 33 (203) ; coarse gravel and pebble-stone, 27; blue clay, 7; gray sand, 13 ; blue clay and sand conglomerated, 12 ; light-gray sand, 3 ; blue clay, 6 ; light sand, 9 ; bhie clay, 1 ; fine gray sand, 12 ; dark clay, 2 ; fine gray sand, 7 (302) ; clay and sand, 10 ; coarse gray sand, 1; light clay, 19; coarse sand, 14. (Xote. — At 340 feet, in this stratum of sand, a red-wood stump was found, and a stream of water ascended to within three feet of the surface.) Light clay, 8; fine gray sand, 1^; light clay, 20i; coarse gray sand, 20 ; clay, very hard, 4 (400) ; gray sand and clay, 5; clay, 20; coarse gray sand, 3; light clay, 15; fine gray sand, 4 ; light clay and sand, 1 ; coarse gray sand and clay, 1 ; light-blue clay, 11 ; gray sand and clay, 7 ; light-blue clay, 15; fine gravel, 1; light-blue clay and gravel, 13 (496); fine gravel, 25; clay and sand, 2; sand and clay, 5; coarse gray sand, 7 ; fine blue clay, 8 ; fine gray sand, 42. (Xote. — At 560 feet, in this stratum of sand, obtained a stream of water, rising five feet above the surface.) Gray sand and clay, 15 (600) ; light clay and sand, 6 ; fine gray sand, 24 ; clay and sand, 3 ; fine sand, 9 ; fine graA^el, 3 ; fine gray sand, 5 ; coarse sand, 2 ; blue clay and sand, 8 ; gray sand and clay, 8 ; clay and sand, 5 ; fine gray sand, 10 ; clay, 5 ; coarse gray sand, 2 ; fine light-blue clay, 4 ; hard, chocolate-colored clay, 2 ; blue clay, 2 (698) ; fine gray sand, 30 ; clay and sand, 8 ; gray sand, 4 ; light clay, 10 ; coarse sand, 6 ; blue clay, 4 ; dark clay, very 3 50 RESOURCES OF CALIFOK XI A. hard, 2 ; gray sand, 4 ; blue clay, 14 ; liglit-drab clay, 3 ; very fine gray sand, 24 (80V) ; light-drab clay, 1 ; light-gray sand, very fine, 27 ; dark-gray clay, IV ; light-blue clay, very hard, 22 ; light clay, 11 ; dark, chocolate-colored clay, very hard, 10 ; light clay, very hard, 15 (910) ; fine gray sand— a good stream of vi^ater, 2 ; clay and sand, 11. (Note.— A large stream of water was obtained in this stratum, rising seven feet above the surface.) Fine sand and gravel, 10; blue clay, 20; sand and gravel, 6 ; blue clay, 27 ; clay, gravel, and mica, 14 (1,000) ; in sand, 2. The depth of the well is 1,002 feet. The temperature of the water, as it issues from the well-surface, is 77°, the atmosphere being 60° Fahrenheit. The water rises eleven feet above the surface of the plain, and nine feet above the established grade of the city. The quantity of water discharged is about sixty thousand o-allons in twentv-four hours. The diluvium in the coast valleys bears a strong general re- semblance, in its material and stratification, to that of the San Joaquin valley. In many places where artesian wells have been sunk, fossil wood and bone have been found three hun- dred and four hundred feet below the surface of the ground, and two hundred feet or more below the present level of the sea. In the mountains there are also large bodies of diluvium, but the material is coarser than in the valleys, being usually a gravelly clay, deposited in distinctly-marked layers, with inter- vening strata of sand and boulders. § 36. Gold. — Gold is found in nearly all parts of California, but is most abundant on the western slope of the Sierra Ne- vada, between two thousand and six thousand feet above the sea, -from latitude 37° to 40° — a district two hundred and twenty miles long by forty wide. This may be called the Sac- ramento district. It is drained by the Feather, Yuba, Ameri- can, Cosumnes, Calaveras, Stanislaus, and Tuolumne rivers. The next district in importance is in the northwestern corner of the state, including that part of the Sacramento Basin west of Shasta, and the lower portion of the Klamath vaUey. Next GEOLOGy. 51 is the Kern River district, including White River between 35° and 36° on the western slope of the Sierra Xevada. There are gold diggings on the San Gabriel and Santa Anita Rivers, and in the San Francisquito canon in Los Angeles county. In the Colorado vallev, fiftv miles above Fort Yuma, o-old has been found. Xearly every one of the coast counties has more or less gold : it has been foimd in the valleys of Russian River, Putah Creek, Soquel Creek, Coyote Creek, the Salinas River, and in the earth in which the city of San Francisco is built. § 37. Auriferous Lodes. — Gold is found fastened in stony veins, and loose in earthy matter : the latter called placer dig- gings, the former auriferous quartz lodes. It is the accepted theory among geologists that all gold was once enclosed in quartz lodes, and that the gold in the placers was obtained from the disintegration or breaking up of the lodes. The surface of the earth was once all rock'^ the earthy matter was formed bv the action of air and water on this rock. The earthy matter was then deposited in diluvium, among which was the gold that had existed in the rock pre- vious to its disinteg^ratiou. Gold is sometimes found in granite, syenite, limestone, slate, and other rocks ; but the auriferous lodes, regularly worked, are all of quartz. Most of the quartz veins run parallel with the main divide of the Sierra — that is, north-northwest and bouth-southeast — are from a line to thirty feet thick, and are nearly perpendicular, dipping to the eastward. They are be- tween two thousand and six thousand feet above the sea. The general color of the rock is white, occasionally bluish, fre- quently reddish-brown, the color of iron-rust, derived from the decomposition of iron pyrites. In some veins the rock is com- pact, and then it is usually very white ; in others it is full of cracks and crevices, and ready to break into small pieces with a little pounding. Most of the veins have gold in them; only a few have enough to pay for working. The gold is in par- ticles of irregular shape, but with some regularity of size, scat- tered through the rock. The particles are seldom larger than 52 RESOURCES OF CxVLIFORNIA. a pea, never weigh more tlirni an ounce, and often are so fine as to be invisible to the naked eye. A lode has usually a peculiar kind of particles, either large or small. Most of the gold in a lode is usually in a rich streak, near the " foot wall" or lower side, as if the metal had settled down by its gravity. The rock near the " hanging wall" or upper side of the lode is poorest. Occasionally several rich streaks will be found in a lode — one streak with coarse par- ticles of gold, another with fine. All parts of a lode are not equally rich ; but the gold is found in spots. A lode which is very rich in one place may be very poor in another not far off; indeed, there is no auriferous vein in the state known to be regularly rich for a long distance on the surface. The gold is found in streaks or pockets ; the rich streak i-uns downward, and has a regular dip in the lode. It is a matter of very great importance to the miner to ascertain the direction of this dip, and here is the rule : Take out some of the vein stone, and examine the wall rock carefully. In most veins it will be found that the wall has little furrows, as though the lode had been pushed upward. These furrows indicate the direction of the dip of the rich streaks. Pockets may be considered as interrupted streaks ; and when one rich pocket is discovered, others may usually be found by going down into the vein in the proper direction, and that is ascertained in the same man- ner as for continuous streaks. This is an important rule, and it is now published for the first time. I am indebted for it to J. E. Clayton, Esq., mining engineer. § 38. Placers. — The placers are of two kinds — diluvial., or those deposited under large bodies of water, as if in a deluge ; and alluvial., or those deposited under the influence of streams of water, such as the present rivers and brooks of the country. It is evident, from an examination of the mining districts, that large tracts of auriferous ground have been deposited under diluvial influences. The same strata are found extending over wide areas, and the deposition is different from that made by a river. The gold, being nineteen times heavier than water, GEOLOGY. 53 and from six to eight times heavier than the clay and stones with which it is found, has sunk to the bottom of the diluvium. The best diQr2:ino:s are therefore near the "bed-rock." The dirt in which the gold is found is usually a stiff clay, with gravel and large stones intermixed. The common phrase "golden sands" may mislead. Pure, fine sand rarely has any gold in it ; and the richest deposits of the precious metal are in a clay so tough as to give the miner much trouble to dis- solve it, with stones in it weighing from a pound to several hundred weight. The character of the pay-dirt varies greatly. A hill of diluvium may be three hundred feet deep, with a dozen strata of different material, and all of them auriferous in different degrees. In some places the pay-dirt is full of boul- ders, weighing several hundred pounds or more; in other places the stones are all about as large as a man's head ; in others, as large as a hen's egg. In one stratum the dirt is red, in another blue, in another brown. In some places the dirt was deposited in basins of rock, four or five miles across, and from ten to fifty feet deeper at the centre than at the rim. The placer-diggings are all found in a very rough, mountain- ous country. The gold has not been carried far ; its weight has anchored it near its mother-vein. There may be much gold in the Sacramento valley ; but if so, it is deposited be- neath one thousand feet of diluvium, and nine hundred feet below the level of the sea, where it will never be disturbed. The diluvial placers are in what are called hill and flat dig- gings ; the alluvial, made by streams running through the diluvium, are in river-beds, bars, ravines, and gullies. The alluvial placers, as a general rule, are richer than the diluvial. The streams have carried away much of the dirt, and left nearly all the metal. Most of the gold of the rivers comes from gulhes. There is a gully on a mountain : it is dry, ex- cept during heavy rains ; it has steep sides. The rain comes ; the water pours down its sides, fiercely sweeping clay, gravel, and gold along. The bed of the ravine is not so steep as the Bides ; most of the gold stops there ; the dirt is carried away 54 RESOURCES OF CALIFORNIA. into the river, with a little gold. A thousand such gullies, contributing each a little gold, make a river rich. The heav- ier particles are deposited in the middle of the river-bed ; many of the smaller particles are deposited at the sides. The richest spots in gullies are usually where the bed-rock is full of crev- ices, as where slate, with perpendicular strata, crosses the gully. In those parts of a gully where the bed is very steep, there is usually less gold than in spots nearly level. In rivers, the richest spots are usually just below canons, where bars are formed. Wherever there are eddies at times of high water, there the gravel, clay, and gold will be deposited ; and when the river falls, a bar is exposed. The richest bars of California have been found at the mouths of caiions. § 39. Mineralogy of Gold. — The particles of gold in quartz are usually very rough in shape, but sometimes they are in octahedral crystals, and at others in smooth, leaflike sheets. Very rarely specimens of crystals are found, clustered together so as to resemble pieces of coral. Placer-gold, called " gold dust," is fine and coarse. The fine is in scales^ grains^ flour^ shot, and wire. Flour-gold is very fine dust. Grain-gold is in particles about as large as the end of a pin. Scale-gold is in scales from a sixteenth to an eighth of an inch across, and as thick as heavy wrapping-paper. Shot-gold is in roundish particles, the size of a pin-head. Wire-gold is in small wires, from an eighth of an inch to an inch long, and as thick as a pin. Sometimes the wires are fluted, or hollow on one side ; and sometimes they are knotted together. Coarse gold is coarse-shot, pea, bean, moccasin, cucumber- seed, pumpkin-seed, large wire, and miscellaneous coarse. The pea, bean, cucumber-seed, and pumpkin-seed varieties of gold, have particles resembling in shape the seeds whence they derive their names. The coarse-shot is in particles re- sembling coarse shot in shape and size. Moccasin-gold is in pieces resembling a low shoe or moccasin in shape, and about GEOLOGY. 55 half an inch long. Large wire-gold is in wirehke pieces, about a sixteenth of an inch thick, and from a quarter of an inch to an inch long. Miscellaneous coarse gold is in pieces of very irregular shape and size. Fine gold is often found without any admixture of coarse ; coarse is rarely found without some admixture of fine. The different varieties of gold are often found separate from each other. One gully will have scale gold, another fine wire- gold, another moccasin-gold, another pumpkin-seed gold, and 80 on. These different varieties of gold are frequently found very near to each other : a cucumber-seed gully will not be more than a hundred yards from a pea gully. There is a small hill in El Dorado county ; all the gold on one side is fine, all on the other coarse. The gold as it originally comes from the quartz is rough, but by friction among the gravel and sand it becomes smooth. Where all the pieces of gold are rough, it has not moved far from its maternal lode ; where all the par- ticles are small and smooth, the presumption is that it has moved a considerable distance. The larger the stream, the finer and smoother its gold, as a general rule. Most of the gold now obtained is miscellaneous coarse ; the little gullies which yielded the delicate varieties are now nearly all exhausted. Most of the placer-gold is coarse, in pieces worth half a dol- lar or more. Pieces worth five dollars are very common, and numberless nuggets worth one hundred dollars or more have been found in California. The largest nugget of gold on rec- ord was found at Ballaarat, Australia, on the 9th of June, 1858 ; it weighed two hundred and twenty-four pounds Troy, of nearly pure gold, and was called " The Welcome Nugget." The next, weighing one hundred and ninety-five pounds Ti'oy, was found in Calaveras county, California, in November, 1854. The third, called " The Blanche Barkly Xugget," weighed one hundred and forty-five pounds Troy, and was also found iu Australia. Smaller lumps are too numerous to mention. All placer-gold is called " dust," but the particles of the dust are 5(5 RESOURCES OF CALIFORNIA. sometimes pretty large. No satisfactory explanation has been given of the fact that placer-gold is usually in particles so much larger than that found in quartz. Gold is fine and coarse mechanically — that is, in the size of its particles — and chemically in its composition. Most metals are found in ores, combined chemicallv with non-metallic sub- Stances which hide them. The ores have usually neither the .color, the specific gravity, the strength, nor the other peculiar features of the metals. Native gold is never found as an ore ; it is always in a metallic form. The reason of this is, that it does not rust on exposure to the air, nor is it dissolved by any of the simple acids. And yet it is never found pure, but always mixed with silver, in nearly all possible proportions. Fre- quently copper and lead are also found in native gold. The amount of other metal in gold is designated by figures of fine- ness, estimated according to thousandths. Perfectly pure gold is 1,000 fine; gold containing one-tenth of its weight in silver . is 900 fine; that is, 900 parts in 1,000 are gold, and 100 are silver. In gold 600 fine, 400 parts in 1,000 are of other metal. The native gold in California varies in fineness from 500 to 990, averaging about 880. One large piece, found at Downie- ville, was 992 fine. In Mariposa, Fresno, and Buena Yista counties, and at Mono Lake and Walker's River, east of the Sierra Nevada, the fineness is very low. The gold of the Col- orado is very fine. In other districts there are great variations in the fineness within small distances. One has gold 900 fine ; another, one hundred yards distant, has gold only 800 fine. Ordinarily, all the gold in a gully or in a river-bar is of the same fineness ; so also all the gold in a quartz-lode is of the same fineness. But there are the same differences of fineness between the gold taken from different quartz-lodes as in that taken from different gullies. For these differences there is no satisfactory explanation. Let us now run through the list of the principal mining dis- tricts of the state, giving the fineness of the placer-gold of each ; GEOLOGY. 67 The gold found in the bars and beds of the Klamath and Salmon Rivers is in coarse particles, averaging 868 fine, and mixed with iridium. The gold of Scott River is coarser and poorer. That of the South Fork of Scott River is about 875 fine, and coarse. The gold on Trinity River, near Weaverville, is in small particles, from 885 to 940 fine. Twenty miles below Weaverville, on the same river, the gold is poorer — from 865 to 870. Still farther down, iridium becomes so abundant, that the gold is worth a dollar or a dollar and a half per ounce less than it would be if clear of that metal. In the gullies and hills near Weaverville there are rich dig- gings of coarse gold, from 890 to 960 fine. At Gold Blufi"the gold is 950 fine. The gold found at Yuba is coarse, in rough, flat particles, from ^20 to 830 fine. In some lumps from Yuba little pebbles have been found hidden in their centre. The gold of most of the creeks near Yuba is from 845 to 850 fine. McAdam's Creek, near Shasta, yields gold from 875 to 885 fine. Cottonwood Creek, near the Oregon line, yields gold of the same fineness. At Oro Fino, near Yuba, the gold is in wires, and, like all wiry gold, is of poor quality, from 760 to 780 fine. The Shasta gold is generally coarse, ranging from 865 to 925 fine, except at French Gulch, where it is only 830 fine. The Pit River gold is coarse and poor, 830 fine. The Feather River gold is all good, from 890 to 920 fine. At Oroville it is from 920 to 940 fine. At La Porte, Gibsonville, and Pine Grove, in Sierra county, the diggings are deep, and the gold coarse, and from 915 to 970 fine. At Poor Man's Creek, the gold is coated with some- thing like an enamel, the color of iron-rust. When the gold is pounded, this enamel breaks ofi*. 3* 58 RESOURCES OF CALIFORNIA. The Downieville gold is coatse, and from 895 to 925 fine. At Goodyear's Bar the fineness varies from 880 to 885. At Foster's Bar, and farther down, from 890 to 900. At Slate Creek and Canon Creek, from 900 to 910. At Forbestown, in Yuba county, the gold is 890 fine. At Camptonville, the fineness is from 920 to 970, except in one hil], which has wiry gold, 870 fine. The gold of the Middle Fork of the Yuba River is fine, from 885 to 890. That of the creeks and ravines tributarv to that stream is Still finer— from 900 to 920. At Xorth San Juan the fineness is from 960 to 965. At French Corral it is 920 fine. The gold of the Southern Fork of the Yuba River is from 890 to 900 fine. Every hill about the town of N^evada has a quality of gold differing from that of other places in the vicinity. Some of it. is very good, but the general character is j^oor, from 800 to 850. Most of it is rough. The Grass Valley gold is jDOor, from 800 to 840. At Rough and Ready the gold varies as at ISTevada. The gold of Yuba county is good, from 940 to 970. The Timbuctoo gold in Yuba county is 950 fine. The gold of Park's Bar is 910 fine. The Xorth Fork of the American River has gold from 915 to 920 fine; the Middle Fork from 865 to 900; the South Fork from 915 to 920. At Iowa Hill, the gold is 900 fine ; at Michigan Bluff*, 930 ; at Forest Hill, 900; at Yankee Jim's, from 890 to 910; at Auburn, 860 ; below Auburn, and near Ophir, 820 ; and at Secret Ravine, 780. All these placers are in Placer county. At Gold Hill, in Placer county, iridium is found fastened in with the gold; the only j^lace on the coast where the two metals are found fastened together. Next we come to El Dorado comity. The Coloma gold is good, about 915 fine; and ^ome of the hill gold in the vicinity GEOLOGY. 59 of the town is from 920 to 930 fine. The Georgetown gold is coarse, and from 890 to 920 fine. At Kelsey's Diggings the fineness is 860, At Placerville the range is from 870 to 970. Coon Hollow, near Placerville, produces gold 970 fine. At Diamond Springs the fineness varies from 870 to 900. The El Dorado or Mud Springs gold is 860 fine. The gold of the Cosumnes River varies from 865 to 875. The gold along the American River, in Sacramento county, is from 915 to 920 fine. Most of the gold in Amador county is poor, from 865 to 920. The gold about Vf/cano averages 870; Jackson, 865 to 868 ; the Buttes, near Jackson, 920. The gold of the Mokelumne River, above Mokelumne Hill, varies from 850 to 910. At the hHl, some of the gold has been 980 fine. At Campo Seco the fineness is 900. Along the Mo- kelumne River are many placers where the gold is in coarse, wiry pieces, and poor in quaHty. At Vallecito, the fineness is 915 ; at San Andres, 920 ; at Murphy's, 885 ; at Douglas Flat, 890; at AngeFs, 890; at Jesus Maria, from 858 to 860; and at Carson, from 890 to 920. The gold found along the Stanislaus River is from 875 to 880 fine. Columbia, in Tuolumne county, is the best place for good gold in the state ; it ranges from 930 to 970. There are many other places where gold equally fine is obtained, but none which produces so much gold of a high fineness, with so small a proportion of poor gold. The average of the Sonora gold is 900 ; Jamestowm, 870 ; Montezuma Flat, 900 ; ravines at Chi- ' nese Camp, 950 ; the river and creek claims at Chinese Camp, 860; Don Pedro's Bar, 880; Big-Oak Flat, 800; and Garote' 810. La Grange, in Stanislaus county, has gold 885 fine ; that of the Merced River is from 845 to 860 fine. The gold of Mariposa county is poor, and much of it wiry, ranging from- 700 to 820 fine, averaging about 760. Some of the gold of Mariposa county is coarse, and resembles that of 60 RESOURCES OF CALIFORNIA. high fineness from other districts, but, on assaying, it proves to be poor. The gold from the San Joaquin River is in smaU scales, and about 800 fine. The Kern River gold is 630 fine. The Colorado gold is 930. The Walker's River gold is 560 ; the Mono gold 600. The above figures of the fineness of gold from various dis- tricts refer only to the placer-gold. The gold from diflferent quartz-lodes also varies. As a general rule, the quartz-gold is not so rich as the placer-gold ; but some of the gold taken from quartz is nearly as rich as any from the placers. § 40. Silver.— A large amount of silver is found in Califor- nia. One-tenth in weight of the gold-dust is silver. But it was not until I860 that valuable veins of argentiferous ore were discovered in the state. As gold predominates on the western side of the main divide of the Sierra Nevada, so does silver on the eastern side. The Washoe mines are not in Cali- fornia ; but the Esmeralda and Coso districts are. Esmeralda is in latitude 38° 15', about two hundred and fifty miles in a direct line from San Francisco in an eastward direc- tion, and just within the limits of the state, as is generaUy sup- posed, though some persons assert that it is in Utah. The country is mountainous ; the rock is porphyry and trap. The argentiferous veins are of a bluish-white quartz, containing sul- phuret of silver. The principal vein of the district runs north and south, and this has very little gold ; many other veins, containing considerable quantities of gold mixed with the sil- ver, run east and west. The main vein is about twenty feet Avide. The ores assay from thirty to fifteen hundred dollars per ton, but the hitter figure was only obtained from picked specimens. Timber suitable for firewood is abundant, and there is sufticient water to supply the wants of a small town. The Coso silver district is about one hundred and fifty miles northward from Los Angeles, one hundred miles eastward from Yisalia, and twenty miles southeastward from Owen's Lake. GEOLOGY. 61 Wood and water are very scarce. Little is known about the district as vet. The Coso and the Esmerelda districts are both in the Great Basin of Utah, and about five thousand feet above the level of the sea. It is said that rich silver-mines have been discovered in the valley of the Mojave River. In the Coast Mountains, in Monterey county, a silver-inine called Allisal has long been known to exist, but it is not rich enough to pay. Similar veins are found in the Coast Moun- tains, in Santa Cruz county. Veins of silver ore are also found in Xevada county. § 41. Plati7iurn. — Platinum, iridium, and osmium, are three white metals resembling steel, often found in the placer mines of Cahfornia. Thev usuallv occur toirether : and are found more abundantly in the lower part of the Klamath valley than in any other part of the state. In many districts they are entirely lacking. Platinum is found in lumps by itself; iridi- um and osmium are found united, and are then called irid- osmium. These metals are found in small particles, usually fine scales ; the largest piece was of irid-osmium, found on the Lower Elamath, and weighed an ounce and a quarter. They are not found separate from the gold, nor are they ever the main object of search ; they are obtained in small quantities only, and are rarely bought and sold in the state ; they have no fixed market price. When mixed with gold-dust, they injure its value, and prevent its reception at the mint on de- posit. § 42. Quicksilver. — There is probably no country in the world so rich in quicksilver as California. That metal is ob- tained only from its sulphuret or cinnabar, of which extensive deposits are found in Santa Clara county, about sixty miles southward from San Francisco, and fifteen miles from San Jose. There are three mines here — the Xew Almaden, the Euriqueta, and the Guadalupe. The ore is found between trap on one side, and metamorphic limestone on the other. The mines are about one thousand feet above the level of the sea. 62 RESOURCES OF CALIFORNIA. The gangue or vein-slone is quartz. The ore varies in rich- ness from 5 to TO per cent. : the ore of the Ahnaden mine averages 18 per cent. ; that of the Enriqueta mine is about the same; that of the Xew Idria mine is about 8 per cent. The lodes are extremely irregular ; sometimes there will be a mere thread, which will widen out into a mass foi'ty feet in breadth, twenty high, and seventy long, of rich ore, and then diminish aeain to a thread. The total annual production of the state will probably amount to three miUion seven hundred thousand pounds, of which two million four hundred thousand at least will come from Xew Almaden. The Kew Idria mines, in the Coast Mountains, about seventy-five miles southeastward from San Jose, furnish about three hundred and fifty thousand pounds per annum. In Xapa county, on the slopes of Mount St. Helena, and in Sonoma coimty, in the Geyser Mountains, west of Clear Lake, cinnabar has been found, and companies are now at work opening the mines. Whether they will prove to be of value is as yet a matter of doubt. It is a singular fea- ture of the cinnabar veins in these two last-mentioned places, that they are accompanied by a porous hmestone which is full of pure quicksilver ; and when the stone is shaken or struck, the liquid metal flies out in minute globules. There have been rumors of discoveries of cinnabar in other parts of the state, but they are not well authenticated. § 43. Goxjper. — Copper ore has been found near Crescent City ; at Copper Caiion, in the southwestern corner of Calave- ras county ; in San Diego county ; in Xapa county ; six miles below Grizzly Flat, in El Dorado county; near Sweetland, in Nevada county ; and in Shasta county. Sulphuret of copper, or copper pyrites, is found in auriferous quartz-lodes in nearly all the minmg counties. Near Sweetland, Nevada county, there is a claim in which so much copper is found with the gold, that the dust is worth only eleven dollars per ounce. No copper has been smelted in the state ; the only attempts to mine for the ore have been at Copper Canon, and on the bank of the Cosumnes River, below Grizzlv Flat. Some of GEOLOGY. 63 the Copper Cailon ore has been exported. There are rich veins of copper-ore near Crescent City, in Del Norte county ; but, with the present high prices of labor and coal, they cannot be profitably wrought. Vitreous copper is found at WiUiam- son's Pass, sixty miles from Los Ansreles. § 44. Coal. — The old red sandstone and the " true carbon- iferous" rocks, as they are called, are wanting in California ; and it was long supposed that no valuable coal would ever be discovered in the state ; but within the last year some veins of a very good quality have been found near Mount Diablo. The mineral belongs to the tertiary epoch, but contains far more sohd combustible matter and less incombustible material than most tertiary coal. In the strict geological meaning of the terms, it is not " coal," but " lignite," belonging to a later date than the true coal, and lying in a different formation. The rocks are sandstone and shale, of the upper tertiary or pliocene age, and were formed by alternating depositions in salt and fresh water. The coal-veins are situated on the north- eastern slope of Mount Diablo, are from two to nine feet in thickness, dip to the north at an average of 30°, and open on the southern declivities of the hills. A chemical analysis of some of the best specimens showed 50 per cent, of carbon, 46 per cent, of volatile bituminous substances, and 4 per cent, of ashes. The coal is bituminous in character, breaks readily, shows a bright surface where fractured, and burns with a brilliant flame. The quantity is large, and it can be profitably supplied in San Francisco at eight dollars per ton, whereas imported coal has hitherto cost twice as much. § 45. Asphalturii. — Bituminous springs are numerous near the coast, from the northern line of Monterey county to San Diego. They throw up a dark, pitch-like fluid, of a strong odor, which on exposure to the air grows thick, and finally solid. It collects in great masses about the springs, and in some places covers several acres of ground. After being ex- posed to the air for some time, it is called " asphaltura," which i.> very hard in cold weather, but grows soft at about 75°, and 64 RESOURCES OF CALIFORNIA. becomes liquid at 85°. Some springs of it rise in the sea, near San Diego, and others near Santa Barbara ; and masses of the asphaltum are seen floating many miles from shore. The air at sea is even scented with it, and on several occasions frights on shipboard have been caused by its odor, which Avas sup- posed to come from some hidden fire. The principal places in which these springs of asphaltum are found are the following : 1. In the Santa Cruz Mountains, in the southeastern part of Santa Clara county. A tract of twenty-five acres is here cov- ered by the hardened asphaltum. 2. In San Luis Obispo valley. The asphaltum covers thirty acres. 3. The Napoma ranch, in San Luis Obispo county. The springs are small, and yield but little. 4. On the ranch of La Purissima, in Santa Barbara coun- ty- 5. A place six miles west of the town of Santa Barbara. The deposit of asphaltum covers three hundred acres from two to eight feet thick. 6. Rincon of San Buenaventura, Santa Barbara county. 7. A place near the San Buenaventura River, twelve miles from its mouth, in Santa Barbara county. 8. A place near the Santa Clara River, eighteen miles from its mouth, in Santa Barbara county. 9. A place in the Sierra Santa Susanna, in Los Angeles countv. 10. In Los Angeles valley, Los Angeles county. 11. The San Pedro Hills, in Los Angeles county. 12. San Juan Capistrano, Los Angeles county. One of the deposits in Santa Barbara is so near the sea, that the mineral might be thrown with a shovel into a shute which -^ ould carry it into the hold of a vessel at anchor. A spring of mineral oil has been found in Mattole valley, Humboldt county. This is probably the same material with that of the asphaltum springs Of the southern coast. GEOLOGY. 65 The asphaltum generally comes up through sandstone. The springs of Santa Barbara seem to have ceased to flow, while those in Los Angeles county are still active. It is supposed that the amount lying on the surface at the various deposits is not less than five thousand tons. § 46. Other Minerals. — Iron pyrites, or the sulphuret of iron, is found with gold in many of the quartz-veins. Iron is found also in a number of chalybeate springs. Iron-ore con- taining, it is said, 83 per cent, of metal, has been found near Auburn, in Placer county ; and the assessor of Shasta county, in his report for 1857, said "rich iron-ore" had been found in that county. Magnetic iron ore is found in the Canada de las XJvas, and at Williamson's Pass. Tin-ore, of the kind called "tin-stone," of a rich quality, has been found in a large vein at Temascal, in San Bernardino county ; and it is reported that another lode of similar charac- ter has been found in the valley of White River, Buena Vista county. Galena has been found in Humbug valley, Siskiyou county ; in Tuolumne county ; and on the banks of the Cosumnes River, in El Dorado county. Plumbago has been discovered near Columbia, Tuolumne county. Cobalt is found, in various ores, in many counties in the state. At San Emidio, about twenty miles westward from Tejon Pass, is a rich and large lode of sulphuret of antimony ; the vein is from four to twelve feet thick, and is about six thou- sand feet above the level of the sea. Arsenic exists in many of the lodes of auriferous quartz, in the argentiferous lodes at Esmeralda and Coso, and in the an- timonial ore of San Emidio. Sulphur is abundant in California. It exists in large beds near the Geysers, in Sonoma county ; near Clear Lake, in Napa county; in San Diego county, thirty miles northward from the town of that name, and twelve miles from the sea ; near the sea- shore, fifteen miles eastward from Santa Barbara; 66 RESOURCES OF CALIFORNIA. in the valley of Santa Clara River, near its head ; and near San Juan Bautista, Monterey county. The most abundant and most accessible suj)ply is that near Clear Lake. Alum is found in Santa Clara county, eastward of San Jose ; near Lancha Plana and Carapo Seco, in Calaveras county ; at the Geysers, and at Owen's Lake. At the two last-named places there are hot alum-springs. Three miles above the forks of Clear Creek, in Shasta coun- ty, there are twenty salt-springs. Springs strong with sulphate of magnesia, or Epsom salts, are found at the Geysers. Chalk is found in Amador county and in Sonoma county. Suisun marble, the most beautiful form of sulphate of lime, is found in Solano county. Gypsum is found in Santa Cruz and Amador counties. Fine specimens of alabaster have been obtained in El Dorado and Monterev counties. Fine varieties of porcelain clay exist in many of the mining counties, particularly in Tuolumne. Clay, suitable for making fire-brick, may be obtained near Richmond, in Honey Lake valley. Chromium is found on the bank of Feather River, near the mouth of Nelson Creek ; near the town of Xevada ; on the bank of Bear River, above Anson's Ferry ; and on the ridge between the N^orth and Middle Forks of the American River. Chrome iron is found in Monterey county. During the summer and fall, in many parts of the state, a saline efflorescence covers the earth, or those low^ parts of it w^here w^ater collects during the rains of winter. This efflo- rescence is composed chiefly of carbonate and borate of soda, mixed wdth various other salts. The largest deposit of this kind is probably found at Soda Lake, at the sink of the Mojave River. California is very rich in borax, and the day is probably not far distant when w^e shall supply a large amount of it to com- merce. It is found in springs in Tehama county, and in springs and lakes in Napa county. One of these lakes covers a hun- GEOLOGY, 67 dred and fifty acres of ground, and is strong with the solut^n. In the mud at the bottom of this lake, the borax is found crys- tallized in large quantities. Boracic acid has been discovered in the sea-water near the coast. § 47. Artesian Wells. — There are a great number of arte- sian wells in California. In Santa Clara county, within a dis- trict six miles wide by fifteen long, there are three hundred and eighteen — more than are to be found in any other district of equal size in the world. Their water is nearly all used to irrigate land ; some for manufacturing purposes. They supply about two million gallons in twenty-four hours. The wells are from fifty to four hundred feet deep ; the bore varies from six to nine inches. Only a small portion of Santa Clara valley yields artesian water ; the artesian district lies north of a line commencing at Mountain View; thence rimning nine miles with the road through the 'town of Santa Clara to San Jose; and thence southeast to the mountains. South of this line no artesian water is found. It is supposed that the water comes from certain subterra- nean streams. One well has abundant water at one hundred feet ; another, not more than one hundred yards distant, has no water short of three hundred feet. The wells throw up living fish and shell-fish, wliich are of different species in dif- ferent wells. Some wells throw up soft-shell clams good to eat, and of a kind not found in the superterrene waters of the state, before the opening of these artesian supplies. One well throws up a snail, with a long spiral shell ; another has snails with flat shells ; and others have blind fish, evidently of a spe- cies that has lived longr in stibterrene waters, and lost its eves because it had no use for them. Like the fish of the Mammoth Cave, in Kentucky, these artesian fish have the eye-socket and a blind eye in it. The wells that produce these fish and shell- fish are mostly shallow, not more than one hundred and fifty feet deep. If put into water fresh from wells two hundred and fifty or three hundred feet deep, they soon die, as do su- perterrene fish ; either, it is supposed, because the water is 68 EESOURCES OF CALIFORNIA. to<4warra, or because it has not enough air in it. The deeper the well, the warmer the water. Many of the wells have gone dry — " been drained by other wells," as people say ; but yet how can one well " drain" an- other, the mouths of both being on a level with each other ? The wells whose mouths are at a lower level may take water from those farther up the valley ; but the theory that the water deserts one well, to flow out of another of equal or higher elevation, is not sound. There is very little difi'erence of elevation, perhaj^s ten feet, between San Jose and Alviso ; and the wells near the latter place throw their water about five feet higher above the surface than do those of the former. One cause of the failure of the wells may be the filling up of the pipes. From many of them great quantities of sand, gravel, and stones half a foot in diameter, have been thrown up ; and if a large stone should happen to lodge crosswise in the pipe, other smaller stones and gravel might soon stop it up entirely, or break the force of the current so that the water could not rise to the top. In many cases the pipe has not been driven down to the foundation ; and the water, whirling round at the bottom of the pipe, has torn away the earth and made an excavation, thus preparing the way for a caving in of the ground, and filling up of the well. It is the general oj^inion in Santa Clara valley that the arte- sian wells have drained away the surface-water, and the soil is much drier than it was before the wells were bored. In 1849, Dr. Bascom found water w^est of Santa Clara by digging three feet ; and since then he has been going deeper every year, un- til now his surface-well is fifty feet deep. In Pellier's garden, at San Jose, the surface-water was six feet below the surface in 1849 ; now it is fourteen. Ten years ago, there was a con- stant stream of water along the Alameda, between Santa Clara and San Jose ; but that ditch has been entirely dry for several years. A multitude of such observations are mentioned ; yet there is no conclusive proof that the artesian wells have taken away the surface-water. It seems that the soil began to get GEOLOGY. P,9 dry before these wells were bored. The Artesian wells cannot draw the water from the soil immediately around them, for they throw their waters above the earth ; it may be, however, that their supplies are derived from the soil in the upper part of the valley — supplies which, if the wells were not there, would not be drained avray into subterranean channels, but would go to moisterf the whole valley. It is to be observed that, at the very time when the soil of the Santa Clara valley was becoming so dry, a similar disappearance of the surface- water was noticed far beyond the influence of the artesian wells — Honey Lake, on the plateau of the Sierra Xevada, and Lake Ehzabeth, in the Great Basin, both disappearing about the same time, in 1859 ; and several other little lakes and ponds in other parts of the country following their example, soon after. There are artesian wells at various places in the state besides Santa Clara valley, but they offer nothing new in a geological point of view. § 48. Paleontology. — It is a general rule, that the animals of former geological eras, in any given district, appear to have been the gigantic ancestors of those of the present time. Thus the kangaroo and emu of Australia, found in no other part of the world, were preceded by gigantic kangaroos and emus, whose fossil remains are found in New Holland only. So, too, South America, in antediluvian times, had gigantic sloths and tapirs, akin to the animals now found within her limits. Each continent has a fauna of its own, to which its antediluvian ani- mals were nearly akin. Every continent has several zoological districts ; and the ancient and modern fauna of these districts are sometimes as clearly related to each other, and as distinctly separate from those of other parts of the continent, as are the fauna of different continents from each other. But the ante- diluvian animals of California possessed no peculiar relation- ship to the animals now indigenous in the state : the former fauna was totally distinct from that of the present age ; the fossil bones found are not numerous, and no large and valuable 70 RESOURCES OF CALIFORNIA. s-keletons have been brought to light — only fragments here and there. Of quadrupeds, we have the remains of a mastodon, an elephant, and a new species of horse. Of birds and reptiles, nothing noteworthy has been found. We have no entire fossil fishes, but a few teeth. Dr. W. O. Ayres found near Pit River the teeth of a shark, of the genus Lamna — a genus now extinct on this coast. There are numerous beds of marine shells, the most remarkable being on the shores of San Pablo Bay, on the sides of Mount Diablo, and on the slopes of the Sierra Nevada. In the blufls of the coast, near the Lake Hou'se, are shells iden- tical with those now found alive in the vicinity. All our fossils are of the tertiary period, save a few ammonites of the second- ary era, found in tlie northern part of the state. § 49. Belies of Early Humanity. — In May, 1859, an Indian arrow-head was found, eighty feet below the surface of the earth, at Buckeye Hill, IS'evada county. About the same time, another aiTow-head was found three feet deep, in undisturbed alluvium, near Freeman's Crossing, in the same county. In April, 1859, the skeleton of a man was found sixteen feet deep, at Tehaehepe, in Los Angeles county. In October, 1855, two stone mortars, such as were used by the Indians for grinding acorns and grass-seeds, were found near Diamond Springs, El Dorado county, at a depth of one hundred feet below the surface. In October, 1854, the skeletons of two men were found at Rattlesnake Bar, fourteen feet below the surface, and under ancient strata, which had apparently not been disturbed from the time of their deposition. These are a few only of the fossil evidences that California has been inhabited by men many thousands of years. § 50. Mineral Springs. — Mineral springs are very numer- ous in California. The greatest number are found in the coast valleys, from latitude 40° southward to 32°. Nearly every little vale has one or more ; many of them warm or hot. The most common temperatures range from 60° to 120°. Some of these springs yield a lai-ge quantity of water, and are in ro- GEOLOGY. 71 mantic sites, destined to become places of fashionable resort when our population grows dense. There are so many of these springs in the state that there is not room here to men- tion them all. In San Bernardino valley there are a number of warm springs. Their temperatures are thus reported: 108*^, 128°, 130°, 166^ 169°, and 172°. The heat of the springs at Aguas Calientes, in San Diego county, is thus given: 58°, 74°, 130°, 136°, and 140°. Near Warner's ranch, in San Diego, is a spring with a tem- perature of 135°, rising from a cleft in the granite rock. § 51. Cortes Shoal. — About one hundred miles west of San Diego is Cortes Shoal, twenty miles long and three miles wide, with a depth of only fifteen feet in one place. This shoal is evidently the summit of a submarine ridge of moun- tains, parallel with the other ridges of the coast. The shoal was discovered in December, 1852, by Captain Cropper, of the steamship Cortes, who asserted that there was evidently a sub- marine volcano in operation there. The water was in violent commotion, and at intervals was thrown up into the air in col- umns ; there was an escape of steam, and he suddenly found the depth of water change from forty-five to nine fathoms. He saw also light and smoke, and at one time the place looked as though it were a ship on fire. The general opinion is, that he saw only the waves breaking upon the Bishop Rocks, as the rocks at the shallowest place are called ; but some persons ad- here to his opinion of a submarine volcano. Note. — The chief ^Titers upon the Geology of California are W. P, Blake, J. S. Xewberry, an 1 Jules Marcon, in the United States Pacific Railroad Sur- vey reports, and Dr. J. B. Trask's reports to the state legislature, and Jules Marcon's book on the Geology of North America. For the chemical fineness of the gold in the various mining districts, I am indebted to Henry Yan Yalk- enburg. 72 RESOURCES OF CALIFORNIA. CHAPTER IV. SCENERY. § 52. Introductory. — California has much beautiful scenery. The atmosphere is remarkably clear, giving the eye a wide range. The raoimtainous character of the state not only pre- vents monotony and secures a rich variety of landscapes, but gives them extent and grandeur. The large rivers, the high snow-peaks and ridges, wide bays, forests of the largest and most graceful evergreens, parks of majestic oaks, natural mead- ows covered in the spring with brilliant grasses and flowers, are all magnificent in their kind. The valleys are mostly bare of timber, with here and there a grove of oaks, and lines of trees and bushes along the water courses. The coast val- leys are very beautiful, and in the course of ten or fifteen years, when ornamented with thorough cultivation, will be as pretty as any places in the world. Sonoma, Napa, Amador, San Ramon, and Suiiol \^lleys inay be made as beautiful as any part of the world. -^■..^„^^ § 53. Coast Valleys. — Napa vaUey, which is now the most beautiful of these valleys, because most thickly settled and most thoroughly cultivated, is thirty miles long, five miles wide at its mouth, gradually growing narrower toward the head. Napa River, a small stream, runs through the whole length of the valley, which is of level land, bounded on both sides by steep mountains, about two thousand feet high. These moun- tains, brown near the foreground and blue in the distance, oak groves, bi'illiant laurel and madrona, fields of wheat and bar- ley, ploughed fields, good fences, elegant farm-houses, and nu- merous gardens and orchards, go to make up the landscape. • SCENERY. 73 The valley should be seen from the mountain-top, whence it appears spread out as level as a floor. The fields, differing in color accordinGT to the season and their condition of cultiva- tion, lie like a great checker-hoard, over which are scattered numerous farm-houses, and irregular streaks of timber mark- ing the position of the river and its tributaries. The oak-trees form a most important part of the scene. They are wide in proportion to their height, thick in the trunk, heavy in the main boughs, many of which have a horizontal or downward course. The top of the tree has the semicircular shape, and the smaller branches have the pendant grace seen in the Eastern states only in the elm. The large upper boughs of the Cali- fornian white-oak have at their extremities some branches or twigs that hang perpendicularly down from three to twenty feet, and many of the trees for this reason look in the summer as though they were covered with vines. Add to these pecu- liarities the abundant gray Spanish moss, hanging like long and venerable beards from all the twigs and boughs, and the dark druidical mistletoe, and we have one of the most important and characteristic features of the Californian land- scape. Sunol valley, a little dale about three miles in diameter, nearly circular in shape, and shut in on all sides by mountains, is destined to become famous at some future day for its beauty. Now it is in a state of nature, but art will give it new charms. The places in the state most visited on account of their nat- ural scenery are the Yosemite valley, the big-tree groves, and the Geysers. § 54. Yosemite Yalley. — Yosemite valley is a dell of match- less chffs and cascades, with more scenes of grandeur and beauty than can be found within an equal space in any other part of the world. Shut in closely by walls of rock almost perpendiculai', from two thousand to four thousand five hun- dred feet high, it has within a radius of five miles five cas- cades, one of which is two thousand feet high, another nine hundred and forty, another seven hundred, another six hun- 4 74 JJESOUKCES OF CALIFORNIA. dred, and another three hundred and fifty, and tlieir waters flow through a natural meadow ornamented by beautiful trees and brilliant verdure. The valley is a chasm in the Sierra Nevada, four thousand feet above the level of the sea, and distant about one hundred and twenty miles in a direct line from San Francisco, and in a nearly due eastAvard direction. It is watered by the main branch of the Merced River, which above and below makes its way through the mountains in deep and dark gorges, the bottom of which is rarely seen by the sunlight. The valley is ten miles long and nearly three wide in the middle, from which it decreases each way. It is bounded on all sides by walls of yellowish granite, from two thousand to four thousand feet high, in some places perpendicular, and everywhere precipit- ous. It is only at the ends of the valley that it is possible for travellers to get in or out of it, and even there the entrance and exit are difficult for horses and impassable for wagons. The general course of the valley is east and west. The main entrance is at the western end, where a steep path leads down a descent of two thousand five hundred feet. The view from the ridge overlooking the valley is splendid. The chasm is seen winding away amidst the cliffs ; a cascade is in sight, and numerous mountain-peaks rise in various directions. At the bottom of the dell are seen the meandering river, the green grass, and lofty trees diminished to the appearance of shrubs. The waterfall seen on the right several miles distant, is a mere white streak on the face of the rock, and does not appear grand in the least, but it is nine hundred and forty feet high, and be- comes imposing as the traveller approaches it. The body of water is about seventy feet wide on the first of June. The fall is called the Cascade of the Rainbow, from the beautiful colors which always, in sunlight, adorn the mist floating about it. Nearly opposite this cascade, on the northern . side of the valley, and about three-quarters of a mile distant, but apparently much nearer when the tourist looks up at it, is the Capitan (or Captain), a rock which projects into the valley and rises up SCEXEP. T. 75 perpendicularly from the level green-sward three thousand and ninety feet. Continuing our course up the valley, we come soon to another high peak on the same side of the valley, known as the Signal Rock, two thousand nine hundred and twenty-eight feet high. Four miles above the Rainbow cas- cade we come to the great falls of the Yosemite, where the stream of that name, eighty feet wide, leaps down two thou- sand and sixty-three feet in three falls, of which the first is one thousand three hundred feet high, the next two hundred and fifty, and the third four hundred and fifty. About three hundred feet from the top of the upper fall there is a project- ing ledge on which the stream breaks when the water is low, but up to the middle of June, while the current is large and swift with melted snow, the great body of the water leaps clear of the ledge, and pitches sheer down into the hill of rocks below. The Yosemite fall, sometimes calh d by the Indian name of "Cholook," is, in so fir as height is concerned, the greatest cataract in the world; but it does not impress the observer like Niagara. The body of water, never large, is almost lost in spray before reaching the bottom ; and in the late summer, the stream dries up entirely. Niagara is sublime, overwhelming the soul ^yhh the idea of power ; Yosemite is beautiful and romantic— that is all. The tremendous precipices here, as throughout the valley, are greater and more impres- sive than the cascades, which have not enough water to con- found. Besides, the falls cannot be approached from those points whence they might be seen to the greatest advantage and looking from a distance, the Yosemite somewhat resem bles a great sheet qf white satin hanging over the cliff. But inferior as this one cascade is to Niagara, the valley, taking all its scenery together, is far superior in variety and romantic beauty, and equal in grandeur. A day or two at Niagara is enough ; while a lover of nature may stay at Yosemite for months and continually find new delights in the study of the scenery. I have given the total height of the three falls of the Yosemite, all of which are very near together, at two thou- > 76 R E S O U C E S OF CALIFORNIA. sand and sixty-three feet, which is the figure given by the offi- cial surveyor*^ of that county; but others have estimated the lieicrht at two thousand three hundred and two thousand five hundred feet. Across from the Yosemite Falls, on the southern side of the valley, is the Pyramid Rock, so named from the shape which it bears when seen from some points of view. It is three thousand two hundred feet high. Three miles further up and at the head of the valley is "Mirror or Tocoya Lake," a beau- tiful body of water covering about eight acres. The northern side of this lake washes the foot of the North Dome, a huge mountain of rock crowned with a dome-like knob, three thou- sand six hundred and thirty feet high ; and near the southern edge of the lake is the perpendicular face of the South Dome, a still higher mountain, which rises up four thousand four hun- dred and eighty-one feet, towering above all the peaks in the vicinity. This*^peak is a sublime sight, with its perpendicular wall, which, as you look up at it, seems as if it would keep going up forever. Winding back now along the southern side of the valley, we soon come to tlie southern fork of the Merced River, which rushes down through a gorge. We ascend this gorge on foot, climbing with great labor over rocks and through the brush- wood, and at the distance of a mile and a half come to the Vernal or Canopah Falls, where the stream, about one hun- dred feet wide, falls three hundred and fifty feet into a basin surmounted by large evergreen trees. This cascade possesses one great advantage over all the others of the Yosemite val- ley, and that is, it can be approached from above, where we look down upon it from the top of the granite cliflT, leaning over a natural parapet of rock, as convenient as though made expressly for the accommodation of picturesque tourists. About half a mile above the Vernal Fall the river takes a another leap, called the Nevada or Awanee Falls, but it costs a mile and a half of roundabout clambering to get to it. The fall is seven hundred feet high, half of which the water shoots SCENEIIY. T7 plumb dowu through the air, and strikes the projecting rock, breaking mto spray. About two miles west of Nevada Falls is the cascade of Tu- sayac, about six hundred feet high, but it is very difficult of access. A few hundred yards above Lake Tocoya is Lake Tesahae, which has an area of about six acres, and is forty feet deep. Xo description can convey a clear idea of the great variety of scenery in the valley. There are a thousand nooks and cor- ners and woody dells, full of enchanting picturesqueness. The rocky cliifs take all manner of queer forms, resembling pyramids, castles, and domes, chimneys and spires. Li one place there is a narrow cleft one hundred feet deep in one of the rocks, as though some giant had commenced to split off part of the mountain and had left his work unfinished. The river, as it meanders through the valley, is a great ad- dition to its beauty ; and its waters, as well as those of the lakes, are clear as crystal in the summer, though turbid in the spring. Mountain trout are found in all these streams. The climate of the valley is cool. The numerous cascades agitate the air, and near the fall there are often gusty winds. There is much difference between the vegetation and tem- perature of the two sides of the valley; the northern side, where the sunshine is felt throughout the day, being much warmer than the shadows of the southern cliffs. Shrubs and flowers are in the full glory of foliage, and flower along the northern wall in May and June, while the same species are still bare or budding a mile or two to the southward ; but the more delicate annual shrubs are usually more healthy on the southern than on the northern side of the stream, because those in the warmer spots are stimulated to come out so early as to be badly nipped by the frosts, which prevail here all through the spring and into the summer. Tiie valley is almost inaccessible, on account of snow, before the middle of May, and the best time for a visit is in June. In the late summer and fall the quantity of water in these streams decreases 78 RESOURCES OF CALIFORNIA. greatly, and the Yosemite cascade becomes a mere trickling brooklet. There are a couple of houses for the accommodation of trav- ellers, but the fashionable way with those who visit the valley is to go in parties on horseback, provided with pack animals, carrying tent, bedding, provisions, and cooking utensils along. Ladies dress in the Bloomer style. Wagons do not come within forty miles of the valley. There are some quail and hare, but no larger game. The dell was inhabited by a war- like tribe of red men eight years ago, but they undertook to fight with the Avhites and have all been cut off, and scarcely a sign of their existence remains, save here and there the dim vestio-e of a trail. The valley was first entered by white men in 1848, if rumor be true, and afterward in 1850 and 1852, but its wonders at- tracted no notice from the press, and were unknown to the public until 1854, and did not attract many visitors until 1856. § 55. 3Iainmoth Tree G-roves. — The next great natural wonder of California is the big-tree grove in Mariposa county. It is a grove of four hundred and twenty-seven mammoth trees, the largest of which are thirty feet in diame- ter and three hundred feet in height. This is the largest spe- cies of tree in the world, and this is the largest grove of them. The grove is about twenty miles from the Yosemite valley, and thirty miles southeast of the town of Mariposa, and about four thousand five hundred feet high on the western slope of the Sierra Nevada. When the traveller enters the grove he sees on all sides of him numerous giants of the forest, varying from twenty to thirty-four feet in diameter, and from two him- dred and seventy-five to three hundred and twenty-five feet in heio-ht. Sublime sight ! Each tree fills him with wonder as he looks at it. A glance at one of these immense trunks conveys a new idea of the magnificence of nature ; '' glorious as the universe on creation's morn" is this grove. The Titans and the gods fought with such tree-trunks as these for clubs, when the attempt was made to carry heaven by storm, as re- SCENERY. 79 corded iii Grecian mythology. The trees are so high that you must look twice before you can see their tops, and then you must keep on looking before you can comprehend their height. The best way to see them is to lie down and look up, and re- member that the spire of the Xew York Trinity Church, which is the highest artificial structure in the United States, tower- ing far above all the rest of the American metropolis, though two hundred and eighty-four feet high, would be entirely lost to distant view if set down among these trees. The grove covers a space half a mile wide and three-quar- ters of a mile long. Classifying its trees according to their size, w^e find that there is one tree thirty-four feet in diameter; two trees of thirty-three feet ; thirteen between twenty-five and thirty-three ; thirty-six between twenty and twenty-five ; eighty-two between fifteen and twenty ; making a total of one hundred and thirty-four trees between fifteen and thirty-four feet in diameter ; and then there are two hundred and ninety- three between one and fifteen feet through. One very large tree has fallen, and a considerable portion of it has been burned ; but appearances indicate that it was nearly forty feet in diameter, and four hundred feet high. The Mammoth Tree is a cone-bearing evergreen, belonging to the botanical genus named Ciqyressus (cypress) by Linnasus. After the time of that naturalist, his genus of the Gupressus was divided ; so that the Mammoth Tree would have come under the head of the Taxodium^ w^hich, about the year 1850, Avas again divided by Endlicher, the German botanist, and the redwood-tree was declared to belong to a new genus, called Sequoia. In 1853, the mammoth trees first came to the notice of the public. The botanists in San Francisco, engaged in the tur- moil of business, looked at the specimens, but had not time to examine them, and supposed them to be of the same species with the redwood, to which the mammoth tree certainly does bear a very close resemblance. Thinking the tree, however, to be very remarkable on account of its great size, they sent so RESOURCES OF CALIEOKNIA. some of its cones, leaves, and wood, to botanists in New York, bnt they were unfortunately lost on the way. A few months later, an English collector sent some specimens to Professor Lindley, Avho not only found the tree to be of a new species, but determined to make a new genus of it, and he aihxed to it the name Wellingtonia gigantea. When the news of the se- lection of this name arrived in California, a foolish and preten- tious fellow, who meddled with matters of science of which he knew nothing, wrote a ranting article against Lindley, for try- inc to confer the honor of the great tree of America upon a BHton like Wellington, and declaring that the only proper title for the tree would be Washingtonia gigantea. If there had been any bad taste in conferring the name of a Tory and a man of blood upon such a magnificent tree, still the rules ol botanical nomenclature are well estabUshed, and the matter of the name is left entirely to the discretion of the man who first a most symmetrical and graceful conifer, growing to be nearly three hundred feet high. § 71. Yew and Nutmeg. — The Western yew is an upright tree, from fifty to seventy-five high, with thin and fight fofi- age, the leaves being about an inch long. Its growth is straighter, its branches fewer, and its foliage thinner, more feathery, and lighter in color, than the European yew. It grows on the Sierra Nevada from 34° northward to British Columbia. The coast cypress ( Cupressus macro-carpus) is found only on Cedar Point, at Monterey, and there are not more than one hundred trees of it there. The foliage is very dense. The Californian n iriiie-r {Torre >j a calif or nica) is a graceful and beautiful evergreen found in the Coast Mountains near the bay of San Francisco. It grows from fifty to seventy-five feet high, and resembles the Western yew in foHage and general form. The fruit is like a nutmeg in size and shape, but it has a disagreeable terebinthine taste, and is never used as a condi- ment. § 72. Laurel. — The Californian laurel, or bay {Oreodaphne callfornica)^ is one of the most common and beautiful trees of the coast valleys. It is an evergreen, which grows to a height of fifty feet, with a trunk sometimes thirty inches in diameter. 5 98 KESOUKCES OF CALIKORXIA. Tlie leaves are dark green, lustrous, four inches long, one mch wi.le, sharp at both ends, with smooth edges. The iohage >s dense. The wood is grayish in color, very hard, durable, and difficult to split. Both leaves and wood have an aromatm odor, whicli is stronger in the former ; and becomes s .11 stronoer when the leaves are bruised. The odor resembles that of bay-rum. It gives the headache to some sensitive persons. . .... 8 73 3£adrona.—ThG madrona {Arbutus 7nenziesii) is one of the most striking trees of the Californian forest. It is an evergreen, with an open growth, somewhat hke that ot a maple, bright-green and lustrous leaves, and a bright-red bark. Its height is sometimes fifty feet; its diameter in the trunk two feet. The leaves are oval in shape, three inches long, pea-green underneath, and dark and shining above. The bai-k is smooth, and it peels off at regular seasons ; the new bark is a pea-green, which changes to a bright red. The wood is very hard, and is used to some extent in the arts, especially for ma- king the wooden stirrups commonly used m the state, ihe tree bears a bright-red berry in clusters, of which the birds are fond. . 7 7 7 \ 8 Y4 Manzanita.—ThQ manzanita {Arctostaphijlos glauca), another prominent feature in the Californian forest, is a dense clump-like shrub, which grows as high as twelve feet, and nearly as broad as it is high. The trunk divides near the ground into several or many branches, and these terimnate m a great multitude of twigs, so that the shrub is a dense mass of branches and branchlets, all of which are very crooked. The wood is dense, hard, and dark-red in color. The bark is red and smooth, occasionally peeling off and exposing a new light-green bark, which soon turns red. The leaves are regu- larly oval in form, about an inch and a half long, thick and shining, and pea-green in color ; they set vertically upon then- stems. The manzanita bears a pinkish-white blossom m clus- ters, and these are replaced by round red berries about half an inch in diameter ; they have a pleasant, acidulous taste, and i BOTANY. 99 are often eaten by the Indians and grizzly bears, but there is too Httle meat on them to pay white men for the trouble of gathering them. The shrub grows in the coast valleys, and in the Sierra Nevada, up near to the limit of perpetual snow. The name means " little apple," manzcma being the Spanish for apple. § 75. Ceanothus. — The ceanothus, sometimes called the Cali- fornian lilac, of which there are many species, is a beautiful evergreen shrub, growing about ten feet high, with clusters of hlac-like flowers, of various shades of blue, violet, and red, according to the species. The tree produces a multitude of little twigs, and a dense foliage, and may be trimmed into almost any shape. § 76. Oaks. — The Californian white oak ( Quercus hindsii)., or long-acorned oak, is a very large tree, and the characteristic oak of California. It resembles the white oak of the Atlantic slope in the color of its bark and. the shape of its leaves ; but its growth is very different. It seldom reaches a greater height than sixty feet, and is often wider than high. Some- times it measures one hundred and twenty-five feet from side to side. The trunk, which occasionally grows to be eight feet through, throws out large horizontal boughs within ten feet of the ground, and above that point the trunk is soon lost amomr the lar^e branches. The tree fiirnishes no straio-ht timber, and the wood is so soft and brittle as to be of no use in the arts ; whereas the white oak of the Mississippi valley is a most valuable tree, with a trunk so tall and straight, flmt sills and beatns of it sixty feet long are common, and with a wood so tough, that it supplies all the axles and plough-beams of the countrv. The Cahfornian white oak is not even tit for fence-rails. The tree, however, is very beautiful and majestic, and the open groves of it in the valleys and foot-hills form, as Dr. Newberry says, "the most important element in those scenes of quiet beauty which so often excite the admiration of the traveller in California." The tree bears much resemblance in form and size to the oak of England, the groves of it appear- 100 RESOURCES OF CALIFORNIA. in- like the English parks. At the ends of the large boughs are branches which hang down like vines-giving the tree, when seen from a distance, something of the appearance ot an elm. The acorns are large, sometimes two and a half inches long. They once formed the chief article of food of the Cah- fornian Indians. The evergreen oak ( Quercus agrifoUa) is a low, spreadmg tree, much like an apple-tree in size and shape. The foliage, however, is darker and denser. The acorns are small, thm, and sharp-pointed. The wood is hard, crooked in gram, and valuable for knees in ship-building. The Californian chestnut oak {Quercus densiflora) is a low, handsome evergreen tree, with a leaf very much like that of the chestnut. The bark is very rich in tannin, and is exten- sively used for the tanning of hides. The tree is rare north of latitude 39°, and is most abundant in the mountains about Santa Cruz. The Western chinquapin ( Castanea chfysophylla), or golden- leaved chestnut, is an evergreen shrub that grows in the Sierra Nevada. At the height of three feet it bears an edible and palatable fruit, something like the beechnut in shape, but larger. The flowers and ripe fruit are often found on the same bush. The leaves are dark-green above, and covered with a yellowish powder beneath. THe Western chinquapin grows to be a tree thirty feet high in some parts of Oregon. The fulvous oak {querms fulvescens) is a deciduous tree, that grows about thirty feet high, with leaves somewhat like those of the Western chinquapin. The acorn, when young, is concealed in the cup, the two together resembling a little wheel ; but the acorn, when mature, is an inch and a half long, and projects considerably beyond the cup. The wood is tough- er than that of most of the oaks of California. Kellogg's oak ( Quercus kelloggii) is a large deciduous tree, found onfv in California. Its leaves are deeply smuate, with three principal lobes on each side, terminating in several acute points. It bears fruit only in alternate years, or at least most EOTAXY. 101 abundantly every other year. An idea prevails that the acorns give to swine a disease of the kidneys. The huckleberry -leafed oak ( Quercus vaccinifolia) is a shrub, from four to six feet hio-h, which ^rows on the mountains in the northern part of the state. Its leaves, in size and form, resemble the huckleberry ; the acorn is of the size and shape of a small hazel-nut. § 77. JjiicJceye. — The Californian horse-chestnut, or buck- eye {.j^culus californica)^ is a shrub, or low, spreading tree, abundant in the Sacramento, San Joaquin, and coast valleys. It likes to grow about rocky ledges, in ravines, and on the banks of streams. Sometimes it throws up a dozen stems, which grow to a thickness of three or four inches each; but usually it has one trunk, six or eight inches through. The tree rarely exceeds fifteen feet in height, and it has a hemi- spherical shape, very dense foliage, rising from the ground in a globular form. It continues to put forth large clusters of fragrant blossoms from early spring till late summer. The leaves are among the first to open of the deciduous trees of the state. Five leaves grow together on one stem. The fruit has a close resemblance to that of the buckeye-tree of the Mis- sissippi valley, but is larger and more abundant. It is a staple article of food with those few Californian Indians who stiU depend upon wild fruits and game for their subsistence. § 78. Sycamore. — ^The Mexican sycamore {Plataiiics race- mosa) exhibits a striking resemblance to the Western syca- more of the Atlantic slope. It has the same straggling, irreg- ular growth; the same smooth, white, scaly bark; the same large, yellowish leaf : but instead of having only one ball on a stem, like the Atlantic sycamore, it has several, the stem run- ning through one or two, and terminating in the last one. § 79. Pltahaya. — The pitahaya {Cereus giganteus)^ a gigan- tic cactus, is one of the most prominent features of the botany of the deserts in the southern part of California. It grows to a height of fifty feet, with a trunk thirty inches in diameter. Sometimes the trunk has no boughs, but usually it throws out 102 RESOURCES OF CALIFORNIA. from two to six, which are about half the thickness of the trunk ; they run out horizontally for a foot or tw^o, and then turn upward and rise parallel with the trunk. There are no twigs or leaves, but flowers and fruit grow on the tops of the trunk and branches. The whole plant resembles a huge can- delabrum. The flowers are three inches long, as wide, with stifi; curling, and cream-coloi-ed petals. The fruit is as large as a hon's egg, and the meat is a red pulp, full of little seeds. The taste is insipid ; but when the fruit is dried, according to the Indian custom, it acquires a flavor somewhat like that of a fig. § 80. Yucca.— The yucca, or bayonet-tree, is a kind of palm, an endogenous tree that lives in the southern deserts. It sometimes grows to be thirty-five feet in height, with a trunk two feet through ; but usually it is about ten feet high, with a trunk eight inches in diameter. It has no twigs or branches, but sometimes it divides into two trunks. The foliage, con- sisting of leaves eighteen inches long, and shaped like the blade of a bayonet, hangs down from the tops of the trunks. § 81. 3Iezquit.—The mezquit {Algarohia glandulosa) is a low tree of the Colorado Desert. It sometimes reaches a height of twenty feet, with a trunk fifteen inches m diameter. The lower branches are very near the ground, and the whole tree has a very regular, semispherical form. The leaves are like those of the black locust, and the foliage thin. The tree bears numerous pods, from three to five inches long, full of sweet, nourishing beans, about the size of the common white bean. The mezquit-bean is often eaten by men, and horses and mules are very fond of it. The curly mezquit {Stromhocarpus 2ntb€scens) is a similar shrub, and bears a crooked bean, called the " screw-bean." It also grows only on the desert. § 82. Miscellaneous Trees and Shnths.—A few walnut-trees grow along the SacramCiito River, and it is said that some chestnuts have been found in Mendocino county, but they are unknown in the greater part of the state. We have no indi- BOTANY. 103 geriOiis beech, elm, hickory, locust, acacia, or sassafras. Our wild cherry and wild plum are bushes, but their fruits resem- ble the wild plums and cherries of the East. We have willows and Cottonwood, which differ little in appearance from those of the Mississippi valley. There are wild grapes, blackberries, gooseberries, huckleberries, raspberries, salmon-berries, and strawberries. A truffle, or a root resembling it, is found in the valleys of the coast and the Sierra Xevada. The grizzly bear considers it a delicacy, and frequently digs it up. A shrub called the "joint-fir" (a species oi Ephedra)^ sometimes used for making tea, is found in Calaveras and Tuolumne coun- ties. In the valleys of the Coast Mountains is found the yerba huena (Spanish for "good herb"), a creeping vine, bearing some resemblance in its leaf and vine to the wild strawberry. It has a strong perfume, half-way between peppermint and camphor. The yerba de la vibora (Spanish for " rattlesnake- herb," known to botanists as the Daucus pusillus) is a carrot- like vegetable, the leaves of which are said to be a specific for the bite of the rattlesnake. § 83. Poison OaJc. — The poison oak, or poison ivy {Ithus toxicodendron)^ grows abundantly in the Sacramento Basin, and along the coast. It thrives be'st on a moist soil, and in the shade. In a thicket with other bushes it sends up many thin stalks eight or ten feet high, with large, luxuriant leaves at the top ; in the shade, the leaves are green. In the open, dry ground, exposed to the sun, and without support from oth- er bushes, the poison oak is a low, poverty-stricken little shrub, with a few red leaves. If it can attach itself to an oak-tree, it becomes a parasitic vine, and attains a thickness, though very rarelv, of four inches in the trunk, and climbs to a height of forty feet. The touch of the leaf is poisonous, and causes a very irritating eruption of the skin. It rapidly communicates by the touch from one part of the body to another, causing severe inflammations and swellings. The most delicate parts of the body are most affected by the poison. The eyes are Bometimes closed up entirely by the swelling round them ; and 104 RESOURCES OF CALIFORNIA. many cases are recorded of faces so swollen, that they could not be recognized by intimate friends. Some persons are not aftected by the tc ach of the Rhus ; but instances have occurred wherein persons supposing themselves, after long experience, to be free from danger, have at last been poisoned : and when the poison has once taken hold, the system is always very easily affected from that time forward. Even passing to the leeward of the bush on a windy day, or going through the smoke of a fire in which it is burning, will bring the poison to the surface ao-ain. § 84, Amole. — The amole [Chlorogalumpoineridlanmn)^ or soap-j^lant, has an onion-like, bulbous root, which, when rubbed in water, makes a lather like soap, and is good for removing dirt. It was extensively used for washing, by the Indians and Spanish Californians, previous to the American conquest. The amole has a stalk four or five feet high, from which branches about eighteen inches long spring out. The branches are cov- ered with buds, which open in the night, beginning at the root of the boughs, about four inches of a branch opening at a time. The next night, the buds of another four inches open, and so on. § 85. Nutritious Herbage. — Of indigenous nutritious grasses there are a number in the state. The wild oat, though not a grass, may be mentioned under this head. It resembles the cul- tivated oat so nearly, that there has been some doubt whether they are not identical, but the opinion among botanists is that they are a distinct species. The wnld oat, in the year 1835, was found only south of the bay of San Francisco ; but about that time, when the white men crossed frequently from the southern to the northern side of the bay, the oat was sown in a natural way by horses and cattle, and it spread rapidly over the Sacramento valley and the coast region. It grew very luxuriantly, and in some places surj)assed in the height, size, and abundance of stalks, any field of cultivated oats which I have ever seen. It is said that in some localities the oat-stalks were so high, that men sitting erect on horseback could not BOTANY. 105 see each other at a distance of ten feet. The soil and climate were evidently very favorable to it. During the last six or eight years, the wild oats have been eaten down so closely by cattle, that in many places they have been killed out. They are propagated from year to year, not by the roots, but by the seeds, many of which fall into cracks in the earth, where they lie in safety until the rains come, when the ground closes up and the grain sprouts. The earth cracks in the summer, in many parts of the state ; and in places where the wild oats grow, the position of the cracks of one year may be traced the next season by the position of the stalks of the grain. The wild oat grows on hill and plain, and furnishes a large part of the wild pasture of the state. It is wholesome, nutri- tious, and palatable for cattle. Much of it is cut for hay. The amount of grain which it furnishes is small in proportion to the quantity of straw, and it is never threshed. After the wild oats, in importance to the herdsman, comes the "burr-clover," so named from a spherical burr, about a quarter of an inch in diameter, which it bears in clusters of three. Tliis burr-clover is found in all the settled parts of the state. Cattle do not like it when greeil ; but after it dries, the burrs fall upon the ground, and are picked up by the cat- tle, while the strans^er is astonished at seeino- them eatino* and keeping fat on what appears to him to be bare earth. On ex- amining the surface of the ground, he will find that it is cov- ered with the dry stalks and burrs of the burr-clover. The bloom consists of three very small yellow flowers. It is said that the stalks of this clover take root whenever the joints touch the ground. The alfilerilla {Erodlwn ciciUarium) is another indigenous nutritious herb of much importance to the herdsman. It is succulent, sweet, hardy, bearing clusters of spikes or pins an inch and a half long. These spikes have given it the name of pin-grass ; and the resemblance of its leaves to the geranium has sugrgrested the name of " wild oferanium," bv which title it is also known to some persons. It has a large root, which it 5* 106 RESOUllCES OF CAT. IFOR NIA. sends deep into the ground, thus enabhng it to resist the drought, while above the surface it puts forth a dense mass of stalks and leaves, spreading out sometimes several feet in every direction. Cattle prefer it to every other indigenous herb of the state. The seeds seem to abound throughout the soil, for wherever the earth is ploughed up for the first time, there the alfilerilla appears, though it may never have been seen there before. It is common in gardens, cultivated fields, and fallow lands. The white Californian clover has a large yellowish-white bloom, from an inch to an inch and a half in diameter, a beau- tiful plant, well suited as an ornament for yards and gardens. It grows very large, and two feet high in moist, favorable sit- uations ; while in dry places it will also mature its seed with- out rising more than two or three inches above the ground. It is very sweet, and it is often eaten by the Indians, who like it both raw and boiled. Cattle are also extremely fond of it. Another species of clover has a round bloom about a third of an inch in diameter, composed of violet-tinged flowers. Another clover has a bloom from a sixth to a quarter of an inch in diameter, the flowers of which are subdued green, tipped with pink at the end. The Melilotes officinalis, another herb, commonly called a clover, though not strictly entitled to that name, likes a very moist soil, and then grows luxuriantly, crowding out nearly every thing else. Its bloom consists of a drooping head about an inch long and a sixth of an inch thick, hung with little yel- low flowers. Cattle are not fond of this herb in any shape, but they like it better in hay than when green. Of nutritious grasses there are a number, but they do not form a sod. The drought of summer and fall seems to kill the roots. Of wild flowers there are a great variety and abundance in California, and they have their diflerent seasons for blooming ; and in canons where the soil is always moist, flowers may be seen in every month of the year. In the spring-time the hill- BOTANY. 107 sides are frequently covered with them, and their red, blue, or yellow petals hide every thing else. Each month has its floAv- ers : in March the grass of a valley may be hidden under red, in April under blue, and in May under yellow blossoms. There is such a variety that within an hour I have counted twenty species on a spot not more than twenty feet square. This was on dry, sandy soil, in Sonoma valley, in the montli of May. Kone of the flowers are large, brilliant in color, or rich in sweet, strong perfume. The tule is a reed which covers all the large tracts of swamp lands in the state. It has no leaf, but a plain, round stalk, va- rying from half an inch to an inch and a half at the butt, and tapering gradually to a point. It is usually not more than ei2:ht or ten feet his^h, but at the Tulare Lake it grows to fifteen or twenty feet. The grass and herbage begin to grow and clothe the land- scape in green after the first heavy rains of the rainy season. These rains may come in December, January, or February; and until they do come, the earth, in the districts not covered with timber, is brown. The grass continues green until June, when it begins to dry up and turn yellow and brown, which colors then predominate in the landscape until the rains come again. The death of the grass, except at high elevations, is caused not bv the cold but bv the drouo-ht : and in those months when the prairies of Indiana and Illmois are covered with snow, the vallevs of California are dressed in the brilliant green of young grass. The mistletoe grrows abundantly on the oak-trees of Califor- nia. The Spanish moss, which hangs in long lace-Hke gray beards from the branches, also serves to give beauty to the groves in the valleys. Note — Most of my information about the botany of the state has been derived from the reports of Dr. J. S. Xeu'berry, in the United States Pacific Railroad Survey, and from the conversation of Dr. A. Kellogg, Dr. EL iBehr, and Mr. 11. G. Bloomer, of San Francisco. 108 UESOURCES OF CALIFORNIA. CHAPTER YI. ZOOLOGY. § 86. General List. — Among the indigenous animals of Cal- ifornia are the grizzly bear ; the black bear ; the panther , the wild-cat; the gray wolf; the coyote; three foxes; the badger; the raccoon; the opossum; the mountain-cat ; the weasel; two skunks ; one porcupine ; three squirrels ; two spermophiles ; two ground-squirrels ; three rats ; three jumping-rats ; one jumping-mouse ; nine mice ; one mole ; the elk ; one deer ; one antelope ; the mountain-sheep ; three hares ; two rabbits ; the seal ; the sea-otter ; the sea-lion ; the beaver ; two vul- tures ; the golden eagle ; the bald eagle ; the fishhawk ; eighteen other hawks ; nme owls ; the road-runner ; twelve woodpeckers ; four humming-birds ; eleven flycatchers ; one hundred and nine singers; one pigeon; two doves; three grouse; three quails; one sandhUl crane; forty-one waders; sixty-six swimmers, including two swans and five geese ; about two dozen snakes, including the rattlesnake ; half a dozen sal- mon ; two codfish ; and one mackerel. §87. Bears.— "Ti\Q grizzly bear {Ursus horrihilis) is the largest and most formidable of the quadrupeds of California. He grows to be foiir feet high and seven feet long, with a Aveight, when very large and fiit, of two thousand pounds, be- ing the largest of the carnivorous animals, and much heavier than the hon or tiger ever get to be. The grizzly bear, how- over, as ordinarily seen, does not exceed eight hundred oi nine himdred pounds in weight. In color the body is a light grayish-brown, dark brown about the ears and along the ridge- of the back, and nearly black on the legs. The hair is long. ZOOLOGY, 109 coarse, and wiry, and stiff on the top of the neck and between the shoulders. The "grizzly," as he is usually called, is more common in California than any other kind of bear, and was at one time exceedingly numerous for so large an animal ; but he offered so much meat for the hunters, and did so much damage to the farmers, that he has been industriously hunted, and his numbers have been greatly reduced. He ranges throughout the state, but prefers to make his home in the chaparral or bushes, whereas the black bear likes the heavy timber. The grizzly is very tenacious of life, and he is sel- dom immediately killed by a single bullet. His thick, wiry hair, tough skin, heavy coats of fat when in good condition, and large bones, go far to protect his vital organs ; but he often seems to preserve all his strength and acti^dty for an hour or more after having been shot through the lungs and liver with laro^e rifle balls. He is one of the most dangerous animals to attack. There is much probability that when shot he will not be killed outright. TThen merely wounded he is ferocious ; his weight and strength are so great that he bears down all opposition before him; and he is very quick, his speed in running being nearly equal to that of the horse. In attacking a man, he usually rises on his hind-legs, strikes his enemy with one of his powerful fore-paws, and then commences to bite him. If the man lies still, with his face down, the bear will usually content himself xAth. biting him for a while about the arms and legs, and will then go off a few steps and watch him. If the man lies still, the bear will believe him dead, and will soon get tired and go away. But let the man move, and the bear is upon him again ; let him fight, and he will be in im- minent danger of being torn to pieces. About half a dozen men, on an average, are killed yearly in California by grizzly bears, and as many more are cruelly mutilated. Fortimately, the grizzly bear is not disposed to attack man, and never makes the first assault unless driven by hunger or maternal anxiety. The dam will attack any man who comes near her cubs, and on this accoimt it is dangerous to go in the 110 RESOURCES OF CALIFORNIA. early summer afoot through chaparral where bears make their home. Usually a grizzly will get out of the way when he sees or liears a man, and sometimes, but rarely, will run when wounded. It is said that grizzlies in seasons of scarcity, used to break into the huts of the Indians and eat them. No in- stance of this kind, however, has been rej^orted for some years past. The greater portion of the food of the grizzly is vegetable, such as grass, clover, berries, acorns, and roots. The manza- nita, service, salmon, and whortleberries, are all favorites with him. The roots which he eats are of many different species, and it was from him that we learned the existence of a Cali- fornian truffle, very similar to the European tuber of the same name. The grizzly is very fond of fresh pork, at least after he knows its taste, and if swine come within his reach, he soon learns the taste. The farmers in those districts where the bears are abundant, shut up their hogs every night in corrols or pens, surrounded by very strong and high fences, which the bears frequently tear down. After having killed a hog, if any jDart of the carcass is left, the grizzly will return the next night and feast upon the remains, and go until it becomes putrid. He prefers, however, the fresh pork if it can be had. Not un- frequently the grizzly discovers the carcasses of deer, elk, and antelope, killed by hunters, Vv^ho have gone off for horses to carry their game home. In such case, the hunter usually finds little left for him when he gets back. They do not like climb- ing, and rarely attempt to ascend trees. The grizzly, though he often moves about and feeds in the day, prefers the night, and almost invariably selects it as the time for approaching houses, as he often does, in search of food. The cub is one of the most playful, good-humored, and amusing of animals. He will tumble somersets, sit up on his haunches and box, and in some of his pranks will show a humor and intelligence scarcely inferior to that of very young children. The grizzly may easily be tamed, and it becomes very fond of its master. Adams, the Californian mountaineer and bear-hunter, trained several griz- ZOOLOGY. Ill zlies so that tbey accompanied him in his hunting excursions, defended him against wild animals, and carried burdens for him. The meat of the young grizzly resembles pork in tex- ture and taste, exceeding it in juiciness and greasiness ; but the meat of the old he-bear is extremely strong, and to delicate stomachs it is nauseating. The black bear ( Ursus americanus) is found in the timbered portions of California, but is not abundant. It is more often seen near the coast north of Bodega than in any other portion of the state. Dr. Newberry, speaking of the food of the black bear on this coast, says: "The subsistence of the black bears in the northern portion of California is evidently, for the most part, vegetable. The manzanita, wild plum, and wild cherry, which fruit profusely, and are very low, assist in making up his bill of fare. Rarely, too, we saw trees of yellow-pine bear- ing marks of bears' teeth, where they had torn off the outer bark to get at the succulent inner layer, which is capable of sustaining life, and to which the Indians very generally have recourse when pressed with hunger." It is believed that nei- ther the grizzly nor the black bear hybernates in California. § 88. Panther and Wild- Cat. — The panther of California, supposed by Dr. Newberry to be the Felis concolor — the same with the panther found on the Atlantic slope of the continent — ^has a body larger than that of the common sheep, and a tail more than half the leng^th of the bodv. Its color is dirtv-white on the belly, and elsewhere a brownish-yellow, mottled with dark tips on all the hairs. The panther is a cowardly animal, and, except when driven by some extraordinary motive, never attacks man. A friend of mine, who was out hunting, dressed in a buflf coat, was creeping through some brush to get near a deer, when he felt a heavy animal strike his back. He sprang up very suddenly, and saw a panther, which had jumped down upon him from a tree, probably mistaking him for a calf or a deer. The brute seemed very much astonished and frightened at seeing a man there, and immediately fled at full speed. The panther is nocturnal in his habits, and always prefers the night 112 EESOURCES OF CALIFORNIA. as a time for attacking colts, wliich are a favorite prey with him. He is found in all parts of the state where there is tim- ber, but he never stops long in any place, unless he can find bushes to hide in. The American wild- cat {Lynx rufus) is common in Califor- nia, particularly in the vicinity of the bays of San Francisco and San Pablo, where he often catches fish and water-fowl as well as land-animals. His color is a light brown, with dim, dark spots on the sides, and longitudinal lines along the middle of the back. § 89. Wolves and Foxes. — The gray wolf ( Canis occidenta- lism is found in all the inhabited parts of California, but is not abundant. The coyote is very common in the state, and occupies the same place here with that occupied in the Mississippi valley by the prairie-wolf. Dr. Newberry thinks the two belong to the same species (^Cayiis latra7is\ but I am inclined to believe that they are specifically difierent. The color of the coyote has more of a reddish tinge, he howls more, does not bark so much, and is more cunning. His food consists chiefly of rab- bits, grouse, small birds, mice, lizards, and frogs ; and in time of scarcity he will eat carrion, grasshoppers, and bugs. He is very fond of poultry, pigs, and lambs, and will destroy almost as many of them as would a fox. He is one of the worst ene- mies and most troublesome pests of the farmer. His method of catching chickens is to hide near the hen-roost about day- light, and, as the hens come down, he pounces upon them from his hiding-place ; and his motions are often so quick, that the victim has not even time to squall before she dies. In the spring and autumn, when wild geese and ducks are abundant, many co^^otes make their homes in the tules, where they catch the birds which have been wounded by the hunters. The coyote loves nothing better than a young pig. When he sees an old sow with her young ones, he will hide, and wait a long time, in hopes that a little one will come within his reach ; but if there be no hiding-place, he goes up boldly. The ZOOLOGY. 113 SOW will at once face the assailant, and start to attack liim. He allows her to come up within a few feet of him, and then moves Oil slowly ; and she, like a fool, thinking she will catch him, continues the chase. While running, he keeps his head turned to orie side, partly to watch her, and partly to watch the pigs ; and when he has seduced her far enough away, he suddenly makes a dash at the pigs, and, getting one of them, runs off with it, leavino; the a^^onized and furious sow far be- hind. If the coyote does not succeed in getting a pig at the first attempt — that is, if he does not lead the sow far enough away — ^he tries it again and again, till he succeeds, the sow being so stupid as to follow him, after having repeated oppor- tunities to see his purpose. The coyotes frequently go in packs, and sometimes will un- dertake to attack a cow. On such occasions, they have a con- certed plan of operations : they surround their intended victim, and while those in front rush at her as a feint, those behind attempt to cut her hamstrings. As their teeth are very sharp, they often succeed. The cow's hamstrings once cut, she falls, and is completely at their mercy ; and they quickly pick her bones. The coyote is a great thief, and will steal the pillow from under a sleeping man's head ; for it happens in California that bags of provisions are often used as pillows. When the coyote is hungry, he will gnaw any thing that is greasy, and for that reason he frequently cuts off the hemp and raw-hide ropes with which horses are tied out at night ; but he never bites into hair-ropes, which for that reason were formerly used ex- clusively for staking out horses. . The coyote is nocturnal in his habits, and is very fond ^^ howling or yelping. lie begins with a shrill, quick bark, ana follows up with a succession of yelps, ending in a long-drawn, quavering, melancholy howl. When one begins, all others within hearing take up the cry. Ten years ago, the traveller in the Sacramento valley rarely passed a night without hearing their music. They are not so numerous now, but still they 114 RESOURCES OF CALIFORNIA. are frequently seen in the most densely-settled parts of the country. The red fox ( Vuljjes fulvus macrourus) is found north of latitude 37° ; the gray fox {Vul]yes viigi?iianus) in all the tim- bered parts of the state. The coast fox ( Vuljyes Uttoralis) is found only on the island of San Miguel, off the coast of Santa Barbara. In its color it bears a great resemblance to the gray fox, but it is not more than half as large, is less cunning, and is slower in its motions. Its tail is only one-third the length of its body. The specimens observed were very bold and stupid, allowing themselves to be caught, over and over again, in the same manner. The desert fox ( Vul^yes macrourus), which is found in the central deserts of the continent, crosses the Sierra Xevada, and is often killed in Calaveras and Tuolumne counties. § 90. Badger, e^c— The American badger {Taxidea aineri- caiia) is abundant in the plateau of the Sierra Xevada, and is occasionally found in other parts of the state. It is very shy, and is rarely seen by the traveller. The black-footed raccoon [Procyon hernandozii) is found in the timbered portions of the Pacific slope of our continent from Santa Barbara to British Columbia. It is longer than the At- lantic raccoon [Procyon lotor\ but resembles it very closely in its mental character and capacity, habits and appearance. The raccoon is fond of grapes, and when he enters a vineyard selects those of the finest flavor. An opossum {Bidelphys calif ornica) is found in the wooded portions of the state, but is not abundant. The vellow-haired porcupine {Erethizon epixantlius), a na- tive of California, is the largest of its genus. The spines are a couple of inches long, yeilowish in color, with brown tips. On the lower part of the sides the spines are replaced by long, stiff bristles. The mountain-cat, or striped bassaris {Bassaris astuta), is abundant along the western base of the Sierra Nevada, be- tween latitudes 36° and 39°. The body is about the size of ZOOLOGY. 115 that of the domestic cat, but the nose is very long and sharp, and the tail very long and large. The color of the animal is dark orrav, with rinsrs of black on the tail. The miners call it the " mountain-cat," and frequently tame it. It is a favorite pet with them, becomes very playful and familiar, and is far more affectionate than the common cat, which it might replace, for it is very good at catching mice. The pine-marten (3Iustela americajia) is found in California, but is rare. The yellow-cheeked weasel (Putorlus xanthogenys) is found along the coast, in the vicinity of the bay of San Francisco. The common mink [Putorius vison) has a skin as valuable as that of the beaver ; the fur is of a dark, brownish, chestnut color, with a white spot on the end of the chin. California has two skunks (Jlej^hitis occidentalis and Me- phitis bicolor), very common animals. The JMephitis bicolor, or little striped skunk, is chiefly found south of latitude 39° ; the other in the northern and central parts of the state. The colors of both are black and white. § 91. The Squirrel Phmily. — The Californian gray squirrel (Sciurtfs fossor), the most beautiful and one of the largest ot the squirrel genus, inhabits all the pine-forests of the state. Its color on the back is a finely-grizzled bluish gray, and white beneath. At the base of the ear is a little woollv tuft, of a chestnut color. The sides of the feet are covered with hair in the winter, but are bare in the summer ; the body is more slender and delicate in shape than that of the Atlantic gray squirrel. It sometimes grows to be twelve inches long in the head and body, and fifteen inches long in the tail, making the entire length twenty-seven mches. Dr. Xewberry says: "The Cali- fornian gray squirrel is eminently a tree-squirrel, scarcely de- scending to the ground but for food and water, and it subsists almost exclusively on the seeds of the largest and loftiest pine known {Pinus larahertiana)^ the ' sugar-pine' of the Western coast. The cones of this magnificent tree are from twelve to sixteen inches m length, and contain each one hundred or more 116 RESOURCES OF CALIFORNIA. seeds of the size and shape of the small white bean of com- merce. Tliese cones would be unmanageable by the squirrel in the tree, and he has the habit, so common in the family, of dropping them to the ground, where he can dissect them at leisure. This he usually does early in the morning, climbing to the extremities of the topmost branches, where the cones hang, and cutting off a sufficient number to supply his wants for the day. He then descends, and, commencing at the base of the cone, tears off the scales in rapid succession, and skil- fully possesses himself of the seeds which they conceal. He is compelled, however, to supply other wants than his own, for the smaller pine-squirrel [Sciurus douglasii) and the ground- squirrel ( Tamias townsendii) appropriate a large share of his booty. When oak-trees are near, and acorns are ripe, he has recourse to them for subsistence ; as often as opportunity offers, robbing the woodpeckers of their stores, in which also he has the active co-operation of his more diminutive congeners. From the fact that he feeds upon the ground, it has been sup- posed that he was less active and less fitted for climbing than most tree-squirrels. This, I think, is not true. He is exceed- ingly quick and graceful in his movements ; and if less fre- quently seen to spring from tree to tree than the black and gray squirrels of the eastern states, it is because he inhabits coniferous trees, which are remarkable for the insignificance of their branches compared Avith the size of the trunk, the limbs never stretching out and interlocking, as those of the oak _ and maple and other trees, in which our com.mon species live." The Californian pine-squirrel [Sciuriis douglasii) inhabits the pine and redwood forests of the state. He is gray above and red beneath, with a black stripe separating the two colors. He lives in a burrow or hollow log, but climbs well, and ob- tains his food chiefly from the pine-cones, which he cuts off in numbers at a time, and tears to pieces at his leisure, after they have fallen to the ground. He lays up a store of the seed in his burrow, for his winter supply. He is quick in his motions, graceful in his attitudes, and shy in his habits. . ZO OLO G Y. 117 The Missouri striped ground-squirrel has five dark-brown stripes on the back, separated by four gray stripes ; the sides are reddish-brown, the belly grayish-white, and the tail rusty- black above and rusty-brown beneath. The animal is four or five inches long. It is found in the northern parts of the state. It eats acorns and the seeds of the pine, manzanita, and ceaiio- thus, in the thickets of which last-named bush it prefers to hide its stores. The Spermophile has two species in California, which resem- ble each other so closely, that they are usually supposed to be the same ; they are popularly known as the Californian ground- squirrels, the little pests which are so destructive to the grain- crops. Their bodies are ten or eleven inches long in the largest specimens ; the tail is eight inches long, and bushy ; the ears large ; the cheeks pouched, and herein consists the chief differ- ence between them and squirrels ; the color above black, yel- lowish-brown, and brown, in indistinct mottlings, hoary-yel- lov>"ish on the sides of the head and neck, and pale yellowish- brown on the under side of the body and legs. They dwell in burrows, and usually live in communities in the open, fertile valleys, preferring to mate tJieir buiTOws under the shade of an oak-tree. Sometimes, however, single spermophiles will be found living in a solitary manner, remote from their fellows. Their burrows, like those of the prairie-dog, are often used by the rattlesnake and the little owl. Dr. Newberry says: "They are very timid, starting at every noise, and on CA^ery intrusion into their privacy dropping from the trees, or hurrying in from their wanderings, and scudding to their holes with all possible celerity ; arriving at the entrance, however, they stop to recon- noitre, standing erect, as squirrels rarely and spermophiles habitually do, and looking about to satisfy themselves of the nature and designs of the intruder. Should this second view justify their flight, or a motion or step forward still further alarm them, with a peculiar movement, like that of a diving duck, they plunge into their burrows, not to venture out till all cause of fear is past. Should you in the mean time have 118 RESOURCES OF CALIFORNIA. seated yourself with your back against a tree, and have re- mained for a time as immovable as the trunk agahist which you lean, you will soon see sundry little heads protruding from the burrows, with as many pairs of eyes and ears skilled to detect the least sign of danger from their equally-feared ene- mies, the coyote, the Californian vulture, the red-shouldered and red-tailed hawk, and man himself. If, however, your si- lence and quietness persuade them that you are none of these, they will swarm forth from their holes, and at first timidly, but, gaining confidence, more fearlessly, engage in all the sports and antics for which the schiridcB are noted, and in which none excel the species under consideration. It is a pretty sight, and one to which I have often treated myself, to sit down quietly under these old oaks, and watch the squirrels running about over the grass and trees, gambolling and play- ing together. As far as the eye could reach through the vista, the sprightly movements of these innocent animals could be discerned." The two species are called Beechey's sj^ermophile (Spenjio- philus beechei/i) and Douglas's spermophile {S2)er7no2?hilus douglasii). The size, habits, and general a^Dpearance of the two species are the same, but they differ in the color of a stripe along the spine from the base of the head to the middle of the back: in Beechey's spermophile it is yellownsh-hoary, in Doug- las's it is dark-brown. The former species is found very abun- dantly south of the straits of Carquinez; the latter north of it, and fewer in number. Beechey's sperm ophiles are among the most formidable ene- mies of the farmer in those districts where they make their homes. They increase very rapidly in the vicinity of farms, and do great damage in grain-fields and gardens ; they eat grain and garden vegetables in all stages of their growth ; . they peel young fruit-trees and vines ; they are, in short, dan- gerous to nearly every thing that is cultivated. They are very industrious, and lay up large stores for the winter, spending several hours every pleasant summer's day in gathering food. ZOOLOGY. 119 They go considerable distances to fields; and the traveller, wliose approach scares them, sees them in hundreds running across the road before him, with their tails erect, hurrying from the field to hide tliemselves in their burrows. Many a large wheat-field, which would have yielded forty bushels to the acre if there had been no spermophiles to trouble it, is so despoiled by them, that the crop will not pay for harvesting. They are particularly abundant in the Santa Clara, Amador, and Pajaro valleys ; and their number is an important consid- eration in the estimate of the price of land. They will not live in moist land, nor very near the ocean, wiiere the fogs prevail. They are poisoned with strychnine and phosphorus, drowned by irrigation, and shut out by tight board-fences. In wet winters many of them are drowned ; after a dry winter they are' always numerous. Away from cultivated fields they depend for food chiefly upon grass-seeds, grass-roots, and acorns. The Californian gopher {Thomomys hulUvorus) is, next to Beechey's spermophile, the most abundant and most trouble- some rodent of the state. W^hen full grown, it has a body six or eight inches long, with a tail of two inches. The back and sides are of a chestnut-brown color, paler on the under parts of the body and legs ; the tail and feet are grayish-white ; the ears are very short. In the cheeks are large pouches, covered Avith fur inside, white to their margin, which is dark-brown. The gopher inhabits the fertile valleys of the coast from lati- tude 34° to 39°. He spends nearly all his time under ground, and does most of his mischief there, gnawing off the roots of fruit-trees and garden vegetables, eating newdy-sowm grain and seeds, and nibbhng at flowers and sw^eet bulbs. He is not a climber, nor is he very agile : if he gets into a trench eight inches wide and a foot deep, with perpendicular sides, he will run a long distance in it rather than clamber out; and one of the best methods of catchinsr him is to make such a trench round a field, and place square tin boxes, fifteen inches deep, eight inches square, and open at the top, in the bottom of the 120 RESOURCES OF CALIFORNIA. trend], at regular intervals of about fifty yards. The gopher frequently travels at night, and when he comes to this trench iie falls in. He then runs along in it, looking for a convenient place to get out, and, coming to a tin box, falls into that. He can neither jump out nor gnaw through ; so he remains a pris- oner till he starves to death, or the farmer comes along and kills him. The Colorado gopher {Thomomys fidvus) is found in that portion of the state south of latitude 34°, but is not abundant. It is smaller than the Californian gopher, and has more of a reddish tinge in its colors. Its habits and appearance other- wise are very similar to those of its northern congener. The broad-headed gopher {Tiiom.oniys laticeps)^ found in the vicinity of Humboldt Bay, is about five inches long. Its color on the back, sides, and belly, is yellowish-brown, with a reddish tinge between the fore legs. § 92. The Mat Family. — California has a number of indi- genous jumping-rats, jumping-mice, and other rats and mice, too many and not sufficiently singular, or interesting to the general reader, to deserve a complete description here. I shall content myself, therefore, with giving a simple list of them, with the districts they inhabit, their entire length from the point of the nose to the end of the tail, and the main color of the back : Philip's jerboa, or jumping-rat {Dqyodomys pMlipi) ; Sac- ramento Basin and the southern valleys ; twelve inches ; yel- lowish-brown. The dun jumping-rat {Dipodomys aglUs) ; coast valleys south of San Francisco ; twelve inches ; lead-color. The Colorado jumping-rat {^Perognathus peniGillatus) ; Col- orado Desert ; nine inches ; tawny. The King's River jumping-rat {^Perognathus parvus) ; King's River vallev ; four inches. Hudson's jumping-mouse {Jacidus hudsonii) ; valley of Ca- noe Creek; eight inches; yellowish-brown. Black rat (JSlus rattus) ; coast from Humboldt Bay to San ZOOLOGY. 121 Diego ; fourteen inches. There is much doubt whether it is indigenous. The long-tailed mouse {Reithrodon longicauda) ; coast near San Francisco ; five inches ; dark-brown. Gambel's mouse {^He'^peromys gamhelii) ; from Tomales Biy to Kern River ; five inches ; glossy-brown. Boyle's mouse (Hesj^eromys boylii) ; valley of the American River ; eight inches ; glossy-brown. Cahfornian mouse iyHesperorays ccdlfornicus) ; Santa Clara valley ; six inches ; sooty-brown. Desert-mouse {Hesperomys eremieus) ; Colorado Desert ; five inches ; grayish-yellow. The bush rat {N'eotoma raexicanci) ; near San Diego and in the Colorado desert ; thirteen inches ; yellowish brown. The Neotoma fuscipes^ a rat ; coast valleys, from 38° to 40° ; fifteen inches ; reddish above. The Armcola montana^ a mouse ; near Petaluma, Monte- rey, and Lost River ; six inches ; yellowish brown. The long-faced mouse (Arvicola loiigirostris) ; Pit River valley ; six inches ; yellowish brown. The Californian ground-mouse {Arvicola edax) ; coast val- leys soutli of San Francisco ; six inches ; yellowish brown. The Arvicola californica^ a mouse much like the species last named. The Oregon mouse {Arvicola oregona) ; near Tanales Bay ; four inches ; vellowish brown. The Oregon mole {Scalo2)s tounsendii) is found near the bay of San Francisco, and perhaps in other parts of the state. It is six or seven inches long, nearly black in color, with faint- purplish or sooty-black reflections in the hair. § 93. The Deer Family. — The American elk {Cervus cana^ densis) is found in California as well as in many other parts of the continent. The animal is nearly as large as a horse, and has some resemblance to it in general shape, though smaller, and slimmer in the head, neck, and legs. Its length from the nose to the tail is seven feet ; its height five feet ; its 122 RESOURCES OF CALIFORXIA. greatest weight one thousand pounds. The color is a chest- nut brown, dark on the head, neck, and legs, lighter and yel- lowish on the back and sides. The horns are very large, some- times more than four feet long, three feet across from tip to tip, measuring three inches in diameter above the burr, and weighing, with the skull, exclusive of the lower jaw, forty pounds. The horns of the old bucks have from seven to nine, perhaps more, prongs, all growing forward, the main stem running u]:)jrard and backward. The elk were very abundant in California previous to 1849, and they were frequently seen in large herds ; but within the last ten years they have become rare, and before the close of another decade they will be ex- tinct in our state. A few are found in the San Joaquin valley, but the best place for hunting them is in Mendocino county. Several hundred carcasses find their way every year to the San Francisco market. The young fat elk furnishes a very juicy and sweet venison. The white-tailed Virginian deer, once common in the states east of the Mississippi, is not found in California, but in its place we have the black-tailed deer {Cervus colwnhianus)^ which is a little larger and has brighter colors, but does not furnish as good venison, the meat lacking the juiciness and savory taste of the venison in the Mississippi valley. The av- erage weight of the buck is about one hundred and twenty- pounds, and of the doe one hundred pounds, but bucks have been found to weigh two hundred and seventy-five pounds. The summer-coat of the black-tailed deer is composed of rather long and coarse hair, of a tawny brown, approaching chestnut on the back. In September this hair begins to come off, expo- sing what the hunters call the " blue coat," which is at first fine and silky, and of a bluish-gray color, afterward becoming chestnut brown, inclining to gray on the sides, and to black along the back. Occasionally deer purely white are found. The horn, when long, is about two feet long, and forks near mid-length, and each prong forks again, making four points, to which a little spur, issuing from near the base of the horn, may ZOOLOGY. 123 be added, making five in all. This is the general form of the horn ; sometimes, however, old bucks are found with but two points. The deer likes the hills and the timber ; the prong- horned antelope [AjifAlocapra americcma) loves the valley and the open land. Before the Americans took California, the Sac- ramento and San Joaquin valleys abounded T\'ith herds of an- telope ; but now they are rare in the northern part of the state, and not abundant in the southern part. The traveller in the Tulare valley and in the Great Basin near the Coast Moun- tains, sees herds of them everv dav. Thousands are killed yearly for the market. In size the antelope is not quite so large as the Califoraian deer, which it resembles closely in form and general appearance. They are distinguished at a distance by their motion : the antelope canters, while the deer runs ; the antelope go in herds, and more in a line following the lead of an old buck, like sheep, to which they are related, while deer more frequently are alone, and if in a herd they are more inde- pendent, and move each in the way that suits him best. In color, the back, upper part of the sides and outside of the thighs and forelegs are yellowish brown ; the under parts, lower part of the sides, and the buttocks as seen from behind, are white. The hair is very coarse, thick, spongy, tubular, slightly crimped, or waved, and like short lengths of coarse threads cut ofi' bluntly. The horns are very irregular in size and form, but usually they are about eight inches long, rise almost perpen- dicularly, have a short, blunt prong in front, several inches from the base, and make a short backward crook at the top. The female has horns as well as the male. The hoof is heart- shaped, and its print upon the ground may be readily distin- from the long, narrow track of the deer. The antelope is about two feet and a half high, and four feet long from the nose to the end of the tail. The mountain sheep ( Ovis rnontana) is found on the Sierra Nevada, from the Tejon Pass to the Oregon line, but it is a rare and very shy animal, and is seldom killed. Its length is about five feet, and its weisrht sometimes three hundred and 124 RESOURCES OF CALIFORNIA. fifty pounds, considerably greater tlian that of the deer or do- mesticated sheep. The color is white beneath, grayish brown elsewhere. The horns of the ram are very large, sometimes five inches through at the base and three feet long. Tlie horns, after starting upward, turn backward, then downward, and so round with a circular or spiral shape, the tip inclining outward. Mountaineers assert that these horns are used by the sheep in getting down from the high cliffs which he is fond of frequenting. Instead of clambering down toilsomely over the rugged and broken rocks, he makes an easy job of it by leaping headlong, confidently down, over precipices fifty, yes, one hundred feet high, and alights head first on his horns, which are strong enough to be unbroken by the shock, and elastic enough to throw him ten or fifteen feet into the air — and the next time he alights on his feet all right. § 94. The Hare Family. — The Californian hare, or "jackass rabbit," as it is commonly called [Lepus calif omicus)^ is one of the largest of its class, growing sometimes to be two feet long from the nose to the end of the tail. Its ears are very large, and have suggested the vulgar name. It was once abundant in all the valleys from the Klamath to the Colorado ; it is more rare now. The color beneath is a pale cinnamon ; above it is mixed black and light cinnamon, the longest hairs being of a light smoky-ash color for about half the length, then dark sooty-brown, then pale cinnamon-red, and finally black at the tip. The prairie hare [Lejncs campestris) also, one of the largest hares, inhabits the plateau of the Sierra Nevada, Pit River valley, and the country about the Klamath lakes. It is all white in winter; in summer yellowish gray, with brownish tinges above and white beneath. The length, from the tip of the nose to the root of the tail, is from seventeen to twenty- three inches ; and the tail and ear each measure about four inches. Audubon's hare {Lepus aicduhonii) inhabits the coast val- leys from Petaluma to San Diego. It is fifteen inches long. I ZOOLOGY. 125 with a tail measuring to the end of the hairs on it three inches. The color is mixed yellowish-brown and black above, white beneath, thighs and rump grayish. Trowbridge's hare {Lepus troichridgii) is found along the coast southward from 39°. The length is from eleven to fifteen inches ; the tail, with hair and all, less than an inch. The back is yellowish brown mixed with dark brown, paler on the sides, and ash-colored beneath. The sage rabbit {Lepus artemisia) is found in all the open parts of California north of the Straits of Carquinez. It is from eleven to sixteen inches in length ; in color, brown above and white beneath, with a yellowish tinge, the under part of the neck a yellowish brown. The fur on aU parts of the body is lead-colored at the base. § 95. Aquatic Mammals. — The American beavers {Castor canadensis) were once very abundant in all the large streams of California, and it was chiefly for their sake that the first Ameri- can trappers entered the country some thirty-five or forty years ago. They are still found in nearly all parts of the state, and even numerous, it may be said, in some of the sloughs near the junction of the Sacramento and San Joaquin Rivers. They rarely build dams in California, but Hve in burrows in the banks. When they dive they slap the water with their tails, makinsr a noise that can be heard at a considerable distance in a still night. Their skins, which once commanded very high prices, have lost much of their value since the adoj^tion of silk for making hats. The common mink {Patorlus viso?i) is found in California, but is not abundant. The general color of the animal is dark brownish-chestnut, with a white spot on the end of the chin. The skin of the mink is as valuable as that of the beaver. The Californian otter {Liitra californica) is found all along this coast, and was formerly abundant on all the large streams. It is carnivorous, living entirely on fish and shell-fish. It pre- fers large streams and lakes for its home, while the plant-eating beaver prefers small streams. The Californian otter is some- 126 RESOUKCES OF CALIFORNIA. times five feet long from the point of the nose to the tip of the tail. When in the water, its hair is at times beautifully iridescent. The sea-otter {Enliydra niarina) is larger than the Califor- niau otter, and is also carnivorous. It generally makes its home near islands, and roams about in the water within ten or twenty miles of land. The sea-otter was at one time very abundant along the coast of California, and it was one of the attractions Avhich induced the Russian Fur Company to estab- lish a post at Fort Ross, in latitude 38° 30', where a number of Aleutian Indians were employed from 1812 to 1840 in the otter fishery. They w^ould start out in their little single ca- noes, made water-proof with a covering of fish-bladders, so that there was no danger of their sinking if the sea should sweep over them, and thus they w^ould go out fifty miles to sea and travel up and down the coast, usually coming home well laden with sea-otter skins worth sixty or eighty dollars each. The sea-otter is still abundant on the southern coast, and there are men in Santa Barbara county who make it a business to hunt them. " The otter," says Mr. W. A. Wallace, " is very harmless, and always seeks to escape from human observation. When attacked they make no resistance, but endeavor to escape by sinking in the sea. If closely pursued and there is no escape, they scold and grin like an angry cat. If they escape the ene- my, as soon as they are safe they turn and deride him with various diverting tricks, such as standing on end in the water, jumping over the waves, holding the paws over the eyes, as if to shade them from the sun while looking at the enemy — then lying flat upon the back and stroking the belly. In their escape they carry their sucklings in their mouths, and drive before them those not fully grown. They were formerly taken, by the Russians and Indians, by means of nets, clubs, and spears. The young are said to be delicate eating, the flesh resembling lamb. The flesh of the old ones is insipid and tough. ZOOLOGY. 127 " The otter is never seen upon land. He is purely an aquatic animal. AViien he swims he turns upon his back and propels himself with great rapidity. The fore-paws are rounded like a cat's, but the claws of the older ones are generally worn ofl". The hind-legs, or propellers, are broad and flat, like paddles, and are used very dexterously. The seal much resembles the otter, seen at a distance, but he swims upon his belly, and the hunter seldom mistakes the one for the other. The otter sleeps in the water, lying upon his back, and anchors himself from the motions of wmds and waves by drawinor a strino; of kelj) across his breast, just below his fore-legs. \Yhen discov- ered in this j^osition, they are often approached very near by the hunters. They are very buoyant in the water, but when the chase has been long continued, and the blood of the otter becomes heated by the exercise, on being shot the body sinks rapidly to the bottom, and never rises. More than half the otters shot are lost in this way. " Once a day the otter comes near the shore for food. He eats every thing that grows in salt water, and is particularly fond of abelones (haliotus), mussels, and sea-eggs. At high water the abelone loosens its shell from the rock, to receive the nourishment which the overflowing waters bring to it, and it is then easily taken from the rock and removed from its shell. The otter is well acquainted with all the peculiarities of this fish, and this opportunity to capture it for food." The common seal, a species of phoca, is abundant along the coast. The sea-lions, of the Otaria genus, fi-equent the coast from May to Xovember, making their homes during the winter in Bome other cUme, but where is not known. They deUght to collect on clear summer days on rocks near the water's edge, and bask in the sun. They may often be seen on the rocks near the Golden Gate, and heard too, for they keep up a kind of barking or growling in chorus, which grows louder as they see any one approaching. They do not wait, however, to let a man come near, but pitch off" into the sea before he is within 128 KESOXJKCES OF CALIFORNIA. two hundred yards of them. Their color varies from light yellowish-brown to dark brown. § 96. Vultures. — The Californian vulture ( Cathartes calif or- nicmus)^ sometimes improjDerly called " condor," the largest bird on the continent, and next to the condor the largest flying bird in the world, inhabits all parts of the state, though it is not abun- dant in any place. It is as prominent and peculiar a feature of the birds of California as the grizzly bear among the quadru- peds. It is very shy, and is rarely killed. The total length of the Californian vulture is about four feet, and its width from tip to tip of the outstretched wings, ten feet or more. Its color is brownish black, with a white stripe across the wings. The head and neck are bare, and red and yellow in color. The bill is yellowish white, and the iris carmine. Dr. Xewberry says : " A portion of every day's experience in our march through the Sacramento valley, was a pleasure m watching the graceful evolutions of this splendid bird. Its flight is easy and eftbrt- less, almost beyond that of any other bird. As I sometimes recall the characteristic scenery of California, those intermina- ble stretches of waving grain, with here and there, between the rounded hills, orchard-like clumps of oak, a scene so solitary and yet so home-uke, over these oat-covered plains and slopes, golden yellow in the sunshine, always floats the shadow of the vulture." Dr. Heermann, of the United States Pacific Railroad Sur- vey, wrote thus : "Whilst unsuccessfully hunting in the Tejon valley, we have often passed several hours without a single one of this species being in sight, but on bringing down any large game, ere the body had grown cold these birds midst be seen rising above the horizon and slowly sweeping toward us, intent upon their share of the prey. Xor in the absence of the hunter will his game be exempt from their rav- enous appetite, though it be carefully hidden and covered by shrubbery and heavy branches ; as I have known these marau- ders to drag forth from its concealment and devour a deer within an hour. Any article of clothing thrown over a carcass ZOOLOGY. 129 will shield it from a vulture, though not from the grizzly hear, who little respects such flimsy protection. My coat, used on one occasion to cover a deer, was found on our return torn by bruin to shreds, and the game destroyed. The Californian vulture joins to his rapacity an immense muscular power, as a sample of which it will suffice to state that I have known our of them, jointlv, to drag off, over a space of two hundred yards, the body of a young grizzly bear weighing upward ot one hundred pounds." The turkey-buzzard, or turkey-vulture {Cathartes aura), specifically the same with the bird known by that name m the Atlantic states, is found in all parts of Califorma. From the tip of the bill to the end of the tail it is about thh'ty mches loner, and six feet from tip to tip of the outstretched wmgs. The head and neck are bare, covered with a bright-red wrm- kled ^kin The pluma^re commences below that, with a circu- lar ruff of projecting feathers. The color of the plumage is black, with a purplish lustre, many of the feathers having a pale border. The bill is yellowish in color. 8 97 The Eagle Family.-The golden eagle {Aquila can- adensis) inhabits Cahfornia, and indeed all parts of Xorth America. Its len-th is thirty or forty inches ; its color on the head and neck is^yellowish brown, white at the base of the of the tail, and brown, varying to purplish brown, and black elsewhere. i i <. • The bald eao-le {Halmtus lexicocephalos) was abundant m Cahfornia ten years ago, and is still often seen along the Sac ramento, San Joaquin, and Klamath Rivers. It frequents rap- ids for the purpose of catching fish, which seem to iurnish the larger part of its food. It is from thirty to forty mches long, white on the head and at the base of the taU, and brown- ish black on the breast, wings, and back. The fish-hawk {Payidion carolinensis) is found along all our lar-e rivers. It is from twenty to twenty-five inches long. The head and under parts are white, with pale yellowish-brown spots on the breast. The back, wings, and tail are dark brown. 6* 130 RESOUECES OF CALIFORNIA. The goshawk {Astitr atriccqyUlus) is of the same size with the lish-hawk, and in color is dark — a bluish-slate above, and mottled-white and light ashy-brown beneath. There are seventeen other hawks in the state, most of them small and rare. § 98. Olds. — California has nine species of owls, namely: the barn, great-horned, screech, long-eared, short-eared, great gray, saw-whet, burrowing, and pigmy owls. All of them are found extensively on the continent, beyond the limits of our state, and all save the last two are common east of the Mis- sissippi. The burrowing owl [Athene cunicularia) is ten inches long, ashy-brown above and whitish-brown beneath, variegated by spots and bauds of w^hite and dark-brown. Dr. Xewberry says : " The burrowing owl is found in many parts of Califor- nia, where it shares the burrows of Beechey's and Douglas's spermophiles. We usually saw them standing at the entrance of their burrows. They often allowed us to approach within shot, and, before taking flight, tw^isting their heads about, bowed with many ludicrous gestui-es, thus apparently aiding their imperfect sight, and getting a better view of the intruder. When shot at and not killed, or when otherwise alarmed, they fly with an irregular, jerking motion, dropping down much like a woodcock at some other hole." The pigmy owl ( Glaucidium gnoma) is seven inches long, and inhabits the wooded districts. It flies about actively in the daytime, and appears to subsist chiefly on sparrows, which it catches in dayhght. The general color is brownish-olive above and brownish- white beneath. § 99. Road-runner. — ^The paisano, or road-runner ( Geococcyx californiam(s), is one of the most remarkable birds of the state. It lives almost entirely upon the ground, very rarely flies, and frequents the highways, along which it will run from any one approaching. Its speed is nearly equal to that of a common horse, and it often furnishes an exciting chase to the sohtary i-ider. It is abundant in the valleys and low hills, and makes ZOOLOGY. 131 its home among the bushes. The bird is akin to the cuckoo, and its generic name signifies " ground-cuckoo."' Its length is from twenty to twenty^three inches, of which twelve are taken up by the tail. The general color is olive-green above and white beneath ; the central tail-feathers are olive-brown, the others dark-green — all edged and (except the central two) tipped with white. Dr. Heerman says : " I have not witnessed the following feat, but am assured by many old Califoruians that tliis bird, on perceiving the rattlesnake coiled up asleep, basking in the sun, will collect the cactus and hedge liim around with a circle, out of wiiich the reptile, unable to es- cape, and enraged by the prickly points opposing him on every side, strikes himself, and dies from the eflects of his self-inocu- lated venom." § 100. Woodpeckers. — There are eleven species of wood- pecker in the state ; of which two, the Californian (Jlelanerpes formicivorus) and Lewis's [Ifela^ieipes torquatus), are w^orthy of special mention. , The Californian woodpecker is called by the Spanish Cali- foruians the carpi/itero, or carpenter, because he is in the habit of boring holes with his beak in the bark of the nut-pine, red- wood, Californian white oak, and Western yellow pine, and then storins: acorns in them for his winter use. The holes are just large and deep enough to hold each an acorn, which is hammered in so that there is no danger of its falling out. The acorns on the northern side of the trees, where they are pro- tected from the rains, which come from the southward, often keep good for years. The bark of the nut-pine is preferred, probably being softer and more regular in grain than other bark. The holes are bored to within two or three feet of the ground, and to a height of fifty feet — sometimes, but rarely, in the hmbs as well as the trunk. From thirty to fifty holes are often found in a square foot. In seasons when or places where acorns are rare, the woodpecker will put away hazel-nuts in the same manner. The squirrels often plunder the stores, and then the birds attack the thieves, darting down upon them and peck- 132 KESOUECES OF CALIFOEXIA. ing them with their beaks. When the squirrel sees the prop- erty-owner coming, he hurries to a hole, or gets under a limb, where the woodpecker cannot conveniently strike him. Some- times Indians and even white men are glad to avail themselves of the woodpecker's stores as a protection against starvation. The length of the bird is nine inches ; the anterior part of the body above and the tail are black ; the belly, rump, a patch on the forehead, and a collar on the neck, white; and the crown, and a short occipital crest, red. Dr. Newberry says : " This beautiful bird, the rival and representative of the red- headed woodpecker [of the Atlantic slope of the continent], is an inseparable element of the scenery of the Sacramento val- ley. While we were encamped under the wide-spreading oaks of that region, I had a very good opportunity to study their habits, as they would come into the trees in the shade of which I was lying. They are not shy, and frequently came round in considerable numbers. Their manners are the very counter- part of the Eastern ' red-head,' and their rattling cry is not unhke his. Like the ' red-head,' I have seen two or three of them amuse themselves by playing 'hide and seek' around some trunk or branch ; and like the ' red-head,' too, they de- light to sit on the end of a dry limb, and fly off in circles for the insects which come near them." Lewis's woodpecker is in color dark glossy green above and gray beneath, with dark-crimson patches on the sides of the head and belly. The feathers on the under part are bristle-like. It prefers an elevated home, and is found ten and twelve thou- sand feet above the sea. § 101. Himvining -Birds. — There are four humming-birds in California, all different from those found in the Atlantic states. The white-throated swift, a bird resembling the swallow, but smaller, is common ii; the Colorado Basin. We have a whip- ])Oor-will different from the one known in the Eastern states. Two night-hawks are found in our state, one of them appear- ing on this slope of the continent only in the vicinity of the Colorado, and on the other slope not extending for beyond the ZO OLOGY. 133 Rio Grande. The belted king-fis]ier {Ceryle alcyon) is at home in California as well as in all other j^arts of the conti nent. § 102. Fly-catGher.~^\i^ family of %-catchers {Colopteri- d(B\ which connects the non-melodious with the true singing birds, is represented in CaUfornia bj eleven species, most of which are not seen in the Atlantic states. They are small birds, from five to nine inches in length, and their colors are usually dull. Most of them have their upper mandible bent down abruptly at the tip ; and they always have twelve feath- ers in the tail. One of the most common and the best-known of the fly-catchers is the bird called the "pewee." § 103. Si7igers.—The zoological sub-order called Oscines, or smgers, has one hundred and nine species in our state, inclu- ding two mocking-birds, three thrushes, two blue-birds, three robins, three larks, five black- birds, eleven finches, six wrens, six swallows, six warblers, one martin, one buntinir, six tit- mouses, one snow-bird, two grosbeaks, one cow-bird, one ori- ole, one crow, three ravens, three jays, one water-ouzel, two magpies, and so on. Some of these birds are not called " sing- ers" in common language, but they all belong to the Oscines sub-order, which is marked by a peculiar muscular apparatus for smgmg, composed of five pairs of muscles in the throat. Though there are many species of Oscines in the state, yet the bn-ds are not so numerous, so melodious, nor are they heard so often, as the feathered songsters in the Eastern states. The traveller may proceed for days in the Sacramento Basm, durin- the summer season, without hearing more than a few chirps'' Our singing-birds have been multiplying very rapidly of late' because of the settlement and cultivation of the land, Avhereby then- supply of wholesome and palatable food is much increased, and their enemies the hawks are driven away. Most of our swallows, one mocking-bird, one black-bird, and one raven, found in California, are also seen east of the Mississippi ; but aU our jays, robms, blue-birds, and magpies, and our oriole, are of species not found in the Atlantic states. The majority 134 BESOURCES OF CALIFORNIA. of the Oscines indifrenous on this coast are unknown in the older states. Our inocking-birds are never domesticated, and are not to be compared to the mocking-bird of Virginia. § 104. Scratchers. — The ornithological order oi Rasoi'es, or scratchers, is represented in California by eleven sjDecies, name- ly: one pigeon, two doves, three grouse, two quails, one par- tridge, and one sand-hill crane. The pigeon, partridge, grouse, quails, and one of the doves, are specifically different from the birds known by the same name east of the Mississippi. The wild-turkey is not found in our state. The most abundant and prominent of our scratchers, the Californian quail {Lophortyx californicus)^ is found in all the valleys of California and Oregon. Its breast and upper parts are lead-colored, with an olive-brown gloss on the back and wings ; the chin and throat are black, with a white line run- ning backward from the eye ; the forehead is brownish-yellow ; the belly is pale-buff, with an orange-brown round spot in the middle, changing to white at the sides ; the feathers on the back and sides have a central streak of white, and those on the top and sides of the neck have black edgings. The head bears a crest numbering from thi*ee to six feathers, usually five, about an inch and a half long. The shafts are bare, very slender, and, though all are in a straight line on the longitu- dinal medial line of the head, they are so near together as to look like but one shaft, more especially as the fine, fur-hke bushes at their tops all combine to form a compact little plume. These feathers are usually erect, the plume leaning forward when the bird is trying to look its best in the presence of com- pany ; but when running about in the grass, and not thinking of its appearance, the crest is lowered, falling forward over the bill. The Californiau quail has two notes — the song and the call. The song of the Atlantic quail is in two notes — the well-known whistle, sounding like "Bob-White." The song of the Cali- fornian quail has but one note, beginning like the " Bob" and (.nding like the " White" of its Eastern relative. The calls of ZOOLOGY. 235 the Atldutic and Pacific quails are nearly alike, and may be represented by the syllables " hi-re-he."— » As a game-bird" says Dr. Newberry, "the Californian quail is inferior to the Eastern one, though perhaps of equal exceUence for the table. It does not lie as weU to the dog, and does not afford a ^ood sport. It also takes a tree more readily than the Atlantic quail. Like its Eastern relative, the cock-bird is very fond of sitting on some stump or log projecting above the grass and weeds which conceal his mate and nest or brood, and espe- cially in the early morning, uttering his peculiar cry." The plumed quail {Oreortyx pictus), likewise called the - mountam quail," while the Lophortyx calif amicus is often styled the " valley quail," is peculiar to this coast, and is one of the most beautiful features of its ornithologv. It is a partrido-e ten inches long, very plump in shape, handsome in color, ma- jestic in its bearing, and graceful in motion. Its head is sur- mounted by a crest of two straight feathers, three and a half inches long, which hang backward, one immediately over the other. The breast and neck are lead-colored, the upper parts generally olive-brown ; the throat, and head beneath the eyes, orange-chestnut; the abdomen white. There are numerous variegations of white, black, and minor shades, on the plumage, all contributing to heighten its beauty. The mountain partridge lives in 'the hills and mountains, from the Tejon Pass to the Columbia River. Its song sug- gests the sound represented by the word " whoit," whistle^cl fuller and louder than the song of the Californian quail. It roosts upon the ground ; and if bushes be near, in which to hide, it wm rather run than fly from its enemies. It seldom flies more than two hundred yards at a time. The cock is equaUy attentive with the hen to the young brood, which usu- ally varies from eight to twelve in number. The families seem to be much attached to each other, and if they are scattered, they are very uneasy until all are collected again. In such cases, the hunter can entice them to come to him by imitating the call of either old or young. They are easily domesticated 136 RESOURCES OF CALIFORNIA. — more readily than their brethren of the valley. The moun- tain i^artridge hates the quail, and when brought into its pres- ence always attacks it; the smaller bird makes no resistance. Gambel's quail {Lorphortyx gamhclli) is a bird differing from the Californian quail only in having duller colors, and is per- haps specifically the same, the difference in color being a mere accident of climate. Occasionally, white quails, very similar in form and size to the Lophortyx calif ornicus^ are found near Humboldt Bav. The sage-cock, or cock of the plains ( Centrocercus urophasi- anv.s)^ the largest of the American grouse, often weighing five or six pounds, inhabits the dry plains in the vicinity of Pit Kiver. It is sometimes twenty-nine inches long, and forty-two inches across from tip to tip of outstretched wings. Its color above is variegated with black, brown, brownish-yellow, and vv-hitish-yellow ; its breast is white, its belly black. The male has bare, flame-colored patches of skin on the neck, which are ordinarily hidden by the feathers, but which are plainly visible when he struts about before the hen, with his neck puffed out like a pouter pigeon's. The sharp-tailed grouse {Pedioccetes pliasianeTlas) is also found in the northeastern corner of the state. It is eighteen inches long, light brownish-yellow above, varied with black, a;nd white beneath, the feathers on the breast and sides having brown marks shaped like a V. The tail is long and sharp, the central feathers and the others growing gradually shorter as they approach the sides ; there are eighteen feathers in the tail. The dusky grouse {Tttrao ohscurus) inhabits the coniferous forests of the Sierra Nevada, in the northeastern part of the state. The cock, according to common report, is the hand- somest of all the American grouse. It is twenty inches long, dark-brown above, mottled with lead-color, and lead-color be- neath. There are twenty feathers in the tail, which is broadly tipped with a light slate-color. T!ie band-tailed pigeon ( Columha fasciata), the only wild ZOOLOGY. 137 pigeon found on the Pacific coast, bears a strong resemblance in form, size, and color, to its' congener in the Atlantic states, and has similar habits, but is not numerous. Small flocks mi- grate through the state every spring and autumn, and some of them spend the summer here. The white-winged dove {2Idop1ieUa leucoptera) has been seen in the southern part of the state, but is very rare. It has white spots on its wings, whence its common and technical names are derived. The common dove [Zenaidura caroliyiensis) of the Atlantic slope is found on the Pacific slope as w^ell. The sand-hill crane (Grus canadensis) are found from the meridian of Cincinnati to the Pacific, and are not rare in Cali- fornia. They spend the winters in our valleys, and in the spring migrate to the Klamath Lakes and farther north, where they spend their summers and breed. Subsisting upon vege- table food exclusively, they are themselves good to eat, and are frequently seen in the San Francisco market. § 105. Waders. — The order of waders (^Grallatores) is rep- resented in California by forty-one species of birds, namely : one crane, two herons, two bitterns, one fly-up-the-creek, one ibis, six plovers, one oyster-catcher, tv/o turnstones, one avoi- set, three phalaropes, one stilt, one willet, one godwit, one curlew, five snipes, five sand-pipers, one sanderling, three rails, and one coot. The oyster-catcher, one turnstoue, one plover, and one heron, are the only species in the list not found east of -the ^Mississippi, and none of them have such value or pecu- liarities as would give interest to a particular descrijjtion of til em. § 106. Swimmers. — California has sixty-six species of the order of swimmers {Natatores) : of these there are two swans, six geese, twenty-two ducks, four albatross, two petrels, seven gulls, four terns, three pehcaus, three cormorants, four guille- mots, one loon, and various miscellaneous species. One swan, all the albatrosses, five gulls, the two petrels, the loon, and one guillemot, are found onlv on this coast. 138 r. E S 0 U Pw C K S O F C A L I F O R N I A . The trumpeter-swaii [Cygnus huccinator) is a very large bird, measuring five feet from the point of the bill to the end of the tail, and six feet across from tip to tip of the outstretched Avings. The plumage is snowy- white in color, its legs and bill black. The name of "trumpeter" is given to it because of its clarion-like scream, which is heard as it flies. It frequents the lakes in the northern and northeastern parts of the state, and is sometimes seen in the rivers. It is a shy bird, and is rarely killed. The American swan, found also on the Atlantic slope of the continent, is similar in appearance and size to the trumpeter, but lacks its loud voice, and is otherwise distinguishable from it chiefly by having an orange-colored spot on its bill in front of the eye, whereas the bill of the Cygnus huccinator is en- tirelv black. Wild geese are very abundant in California during the spring and fall, when they pass through on their migrations. Among them are the Canada goose {Bernicla canadensis)^ the snow-goose {Atiser hy2:)erhoreiis)^ the white-footed goose, or " speckled belly" [Anser erythropus)^ Hutchins's goose {^Ber- nicla Iiutchinsii), and the black brandt {Bernicla nigricans). Hutchins's goose is more abundant than any of the others. Some of them, while in the state, get all their food in the tules ; others in the spring resort to the fields of young grain, where they pasture. Dr. Xewberry says : " I was much interested in noticing the perfect harmony of intercourse which seemed to ex- ist among the smaller species. They intermingled freely while feeding, and when alarmed arose without separation ; and I have seen a triangle flying steadily high over my head, com- posed of individuals of three species, each plainly distinguish- able by its plumage, but each holding its place in the geomet- rical figure, as though it was composed of entirely homogene- ous material ; perhaps unequal members of the darker species, with three, four, or more pure snow-white geese flying togeth- er somewhere in the converging lines." Among the ducks of California are the mallard and canvas- ZOOLOGY. 139 back. The meat of the latter has not so fine a flavor as in the Eastern states, probably because it does not here find the wild celery uj^on which it feeds along the streams of the middle states. Many of the geese and ducks pass the winter in Califoruia, where they find an abundance of food in the grain-fields and tules. The murre, or foolish guillemot ( Zfria ringvin), is similar to the gulls, seventeen inches long, dark-brown above and white beneath, with transverse stripes of ashy-brown on its sides. Its throat is brown in sunmier and white in winter. It frequents the islands along the coast, and lays its eggs there on the bare ground or rocks. These eggs are wonderfully irregular in form, size, and color, but are generally about three and a half inches long, sea-green in color, with dark-brown spots of angu- lar shapes on them. Quantities of these eggs are obtained ev- ery year at the Farallones, and are sold in the San Francisco market at about half the price of hen's eggs per dozen, or, if taken by weight, at one-fourth. Their taste, however, is rank, and they are not used by those who can afibrd to buy the hen's eggs. Dr. Heermanu says : " At one o'clock every day during the iigg season, Sundays and Thursdays excepted (this is to give the birds some little respite), the egg-hunters meet on the south side of the island. The roll is called, to see that all are present, that each one may have an equal chance in gathering the spoil. The signal is given, every man starting off at a full run for the most productive egging-grounds. The gulls [Larus occide7itaUs, Western gull), understanding, apparently, what is about to occur, are on the alert, hovering overhead, and await- ing only the advance of the party. The men rush eagerly into the rookeries ; the aff'righted murres have scarcely risen from their nests, before the gull, with remarkable instinct, not to say almost reason, flying but a few paces ahead of the hunter, alights on the ground, tapping such eggs as the short time will allow, before the egger comes up with him. The broken 140 RESOURCES OF CALIFORNIA. eggs are passed by the men, Avho remove only those which are sound. The gull, then returning to the field of its exploits, procures a plentiful supply of its favorite food." § 107. Fishes. — The fishes of the coast and rivers of Califor- nia are all different from those of the Atlantic side of the conti- nent, with the exception, perhaps, of one sj^ecies of the halibut. The cod and shad, two of the most important fishes of the sea of the Eastern shore, and the lobster among crustaceans, are here wanting, as also the cat-fish kind in the rivers. Otherwise our waters are probably as rich in game for the fisherman as those of any country. § 108. Salmon. — The most important fish of California is the quinnat salmon [Salmo quinnat\ a species found from Point Conception to the Columbia River. Its color aboA^e is oliva- ceous brown, changing to salmon-color beneath. The largest one ever caught weighed sixtj-two pounds ; the common size is from ten to thirty pounds. The salmon are born in the rivers, but go down to the sea, where they spend part of every year. They commence to enter the bay of San Francisco in N'ovem- ber, and continue to come in for three or four months. They ascend the Sacramento and San Joaquin Rivers and some of their smaller tributaries, deposit their spawn, and in .June go out to sea again. They come in lean and go out lean, but in the late winter and early spring they are fat. There are two com- mon popular errors, that the salmon do not eat after leaving the sea, and that they never get back alive. The former error is owins^ to the fact that no laro-e articles of food are found in its stomach, and the latter to the fact that when going out all are lean, and that many are found dead along the banks of salmon-streams. But the salmon find their chief food in mi- nute animalculce, and not in fish, for catching which they seem to be so well fitted, with their large mouths and sharp teeth. It is well known that the salmon bite like trout, and furnish excellent sport in clear vv ater to the skilfid fisherman with the fly. They dislike the mud with which the streams emptying into San Francisco Bay are filled by the miners, and therefore ZOOLOGY. 141 do not go far from the sea or ascend the small tributaries ; but elsewhere the}- ascend every little brook, up to points where there is scarcely enough water for them to swim ; and in these expeditions they are so much exhausted and bruised that they soon die ; but the number thus killed is as nothing compared with those which go out to sea again. The female salmon having found a suitable place, uses her nose to dig a trench in the sand about six feet long, a foot wide, and three inches deep, and having deposited her spawn in it, throws a Uttle sand over it wdth her tail, and departs, leaving her eggs to be hatched and the offspring to be fed as best they can. In the month of May the young salmon are found on their way to the sea, from three to six inches long. It is supposed that the salmon always return to the river in which they were born ; so that the salmon born in the lOamath River never enter San Francisco Bay, nor do those born in the Sacramento and San Joaquin Rivers ever enter Humboldt Bay. Although the sea- son in which salmon are abimdant in the rivers extends from November to June, yet some of them are found in the streams of California at all seasons, and they can be had fresh in the San Francisco market every day in the year. The quinnat is the chief salmon of all the streams and bays of California, but Gairdner's salmon {Fario gairdneri) is found in the Klamath River, and the stellatus salmon in Humboldt Bay and its tributaries. Gairdner's salmon has a silvery-gray back, sil\rery sides, and a yellowish-white belly. The body has numerous indistinct, blackish spots. The stellatus salmon is light-olive in the back, yellowish- white on the belly, and rarely exceeds two or three pounds in weight. § 109. Halibut. — There are two species of halibut on the coast of California, the Californian [Hijypoglossus californicus) and the common {Hippoglossus vulgaris). There is some doubt whether the latter species is properly named ; if it be, then we have one species of fish found on the Atlantic coast. The Cahfornian halibut is a slender fish, weighing at the largest twenty-five pounds, in color grayish-brown above and 142 RESOTTRCES OF CALIFORNIA. white below. The halibut prefer a colder climnte, and are not sufficiently abundant in this latitude to sustain a special fish- ery ; but a few are in our market throughout the year. They live in deep water, and in places where the bottom is rocky. They eat little fish and shell-fish, and bite readily at the hook. Their meat is very delicate. . §110. Tarhot. — The turbot [Pleiironychthys rugosus) is the only large flat-fish, excej)t the halibut, found along our shore. It sometimes grows to weigh twenty pounds, but the common size is from three to ten pounds. The turbot inhabits deep waters and rocky bottoms, eats fish, and bites readily at the hook. It is one of the best fish in our market. § 111. Sole. — We have four species of small flat-fish, com- monly called soles {Psettlchthys sordidus., Psettichthys inela- nostictus., Parophrys vetulus, and Platessa hilineata). They are so much alike, that they are not distinguished from one another by fishermen generally. The Platessa hilineata is the largest, sometimes weighing two pounds ; the others rarely exceed one pound. They frequent the shallow waters of the bay of San Francisco, and are caught abundantly in nets at all seasons of the year. The flat-fishes do not bury themselves in the mud here through the winter, as they do in the North At- lantic. The soles feed on Crustacea, little fishes, and marine animalculse. § 112. Mackerel. — The mackerel [Scotnher diego) is found north of Point Conception. It is good, but not more than half as large as the Atlantic mackerel. The Californian mack- erel rarely exceeds ten inches in length. It lies near the sur- face of the water at sea, and is not fond of entering bays or going very near the shore. Like its Eastern congener, it bites readily at any white rag or shining white substance jerked through the water. § 113. Rock-Fish. — The rock-fish furnish the main supply of fish in the San Francisco market. All belong to the genus iSebastes, of which there are eight species, the most important being the red {I'osacens)^ black {pielanops)., and wharf rock- ZOOLOGY. 14.'^ fish {auriculatus). The red rock-fish grows to weigh twenty pounds; the other species rarely exceed fi)iir or five. The wharf rock-fish is the only one caught in the bay ; the others lire out at sea, in deep Avater and on rocky bottoms : they eat crabs and shell-fish, and bite freely at hooks. They are always in market, and their meat is excellent at all seasons. § 114. Sturgeon. — We have three species of sturgeon, of w^hich the only important one is the Californian' sturgeon {Aci- peiiser hrachyrinthus), which sometimes grows to be seven feet long and to weigh two hundred pounds. The sturgeon is a sea-fish, which enters fresh water to spawn, but it is caught in the bay of San Francisco and tributaries at all sea- sons of the year ; whereas in the Eastern states there are sea- sons for sturgeon in the market, as there are for beans and peas. The sturgeon eats the slimy matter, both animal and vege- table, at the bottom of the sea. It never bites, its mouth being circular in form, and fitted only for sucking. It has a habit of shooting up from the bottom and springing out of water, and then falling flat upon its belly, making a loud splash — very diflerent from the porpoise, wiiich also darts out of the water, but always strikes head first, making little noise. Some ichthyologists suppose that the object of the sturgeon in thus falling on the water is to free itself from parasites ; others that it is merely a kind of pLay. The spawning-season is not known precisely, but it is probably from December to May. The meat of the sturgeon is coarse, and in the market is worth only about one-fourth or one-sixth of that of the better table fishes ; but the sturgeon-fishery is profitable, because of the abundance and large size of the fish. § 115. Jeia-Fish. — The Jew-fish {^Stereolepis gigas)^ one of the largest scale-fishes — weighing sometimes five hundred pounds — is abundant south of Point Conception, and rarely straggles as fiir north as San Francisco Bay. Only two have been caught near the Golden Gate, and one of them filled the city with wonder. It is a bottom-fish, living in deep and shoal 144 KESOUKCES OF CALIFORNIA. water, and frequenting lagoons and kelp. It often comes to the surface, and, according to report, goes to sleep there. It bites readily at the hook, and may be taken with harpoons. The meat is very good. §116. Sim-Fish — The sun-fish (Orthagoriscus analis) is found occasionally south of Point Conception, where it is seen fl(jating on the surface, in accordance with the habits of the genus everywlrere. It weighs from one to a hundred pounds. Its form suggests the idea that the body has been cut off near the broadest part, and the tail sewed on. § 117. Green- Fish. — The green-fish i^Opploraona pantheri- na)^ generally called cod in the San Francisco market, but having no relationship to the true cod, is abundant along the coast. It grows to be about two feet in length. The meat is coarse, and green in color; and the fish has little commercial value. § 118. SeaSass. — The sea-bass (Johnius nohilis) is a plaiu, oval fish, bluish-gray in color above, silvery below, weighing from fifteen to forty pounds. It is closely related to the weak- fish of the New York market. The meat is white and deli- cate, and always commands a high price in the market. It is a surface-fish, and sometimes enters the bays, but is not abun- dant anvwhere. It is caus-ht from March to November. § 119. Sheepshead. — The Californian sheepshead (Lahrus pulcher) is a black fish, with a broad, bright-red band sur- rounding the body, and weighs from one to twelve pounds. It has white, broad, projecting teeth, like those of a sheep. It has no relationship to the Atlantic sheepshead, but is a conge- ner of the black-fish of the New York market. The meat has a very fine flavor when fresh, but loses its delicacy after being dead a day or two. It is found south of Point Conception, on rocky and kelpy bottoms, from April to October. Its food is chiefly shell-fish. § 120. Smelts. — We have four species of fish called smelts [Atherinopsis californiensis., Atherinopsis affi?iis^ Osmerus 2Jreciosi(s, and Osmerus si7nilis). The Atherinoi^ses are not ZOOLOGY. 145 true smelts, but belong to the same genus with the sander- liiigs of the Atlantic, Avhich last are thrown away, or used only as bait ; whereas our Atlierinopses are valuable fishes. The Atherinopsis californiensis forms the great bulk of the smelts in our market. It is the largest of the Pacific smelts, some- times reaching a length of fifteen inches, and a pound in weight. The Osmerus species are small. All of them have bright silver bands along their sides. The smelts are more abundant here tlian on the Eastern coast, and are the best of our small fishes. They are caught at all seasons of the year ; in the bays mth nets — never at sea, or with hooks. § 121. Anchovies. — There are two anchovies [JEngraidis inordax and JEngrauUs nanus) on the coast of California. They are so nearly alike, that they are undistinguishable ex- cept by ichthyologists. Both are small, from four to six inches long, very delicate in flavor, but very bony. They are fully equal to the European anchovy for the table. They feed on minute animalculse, go in shoals, and are caught with nets in the bays at all seasons of the year. § 122. Sardine and Herring. — The sardine {3Ieletta cervr lea) is abundant from Humboldt Bay to San Diego. It grows to a length of eight or nine inches, and is therefore much larger than the Mediterranean sardine, to which it is fully equal in flavor. It is found along the coast from April to October, and is caught in the bays with nets. The herring ( Clupea rairabilis) is not so abundant as the Atlantic species, nor so large, but is equal in flavor. It comes in the spring, and goes in the autumn. § 123. Yiviparoiis Fishes. — The viviparous or embiotocoid fishes of this coast are a peculiar feature of its ichthyology. They constitute, perhaps, the most remarkable natural group of fishes in the world, and their discovery caused a marked sensation among zoologists. Other viviparous fishes had been previously known, but their young are brought forth in a very immature condition ; Avhereas the little embiotocoid fishes are born with a fulness of development similar to that of warm- 7 146 RESOURCES or CALIFORNIA. blooded animals, and the moment after they leave the mother they are seen swimming and taking care of themselves. There are seventeen or eighteen specids belonging to the several genera, amonir which the embiotoca and holconotis are promi- nent. All are marine fishes save one, which is found in fresh water. They weigh from half a pound to three pounds, and most of them are grayish brown above and silvery beneath. They are abundant in the market at all seasons of the year, and are called " perch" by the fishermen, though they have no relationship to the true perch. The meat is not good. The young are born from April to August. § 124. Fresh -Water Fishes. — Among the fresh-water fishes the most important is the brook-trout (Salar iridea), which is fomid in all the mountain- streams of the state, and offers fine sport for fly-fishing. It not unfrequently growls to weigh two pounds, and, if report is to be believed, sometimes reaches ten and twelve pounds. In appearance and flavor it is similar to the trout of other countries. A fish called the salmon-trout {Ptychocheilus grandis)^ but not related to the salmon, the trout, or the salmon-trout, is found in all the large rivers and lakes of California. It grows to weigh thirty pounds. Its teeth are not in the mouth, but in the throat, where it crushes such shell-fish as it feeds upon. It bites voraciously, and is caught with the hook and with nets. The meat is poor, bony, and insipid. It is brought to the market in winter. The small ones are called pikes. A chub {Tygoma crassicauda), and two suckers (Catosto- onus lahicitus and Catostomiis occidenfalis), never weighing more than three pounds, are also found in our rivers. They are not valuable. § 125. Shell-Fish and Crustaceans. — We have five species of shell-fish valuable for the table : one oyster, two muscles, one cockle, and a soft-shelled clam. The oysters are small, not finely-flavored, nor abundant. We have no lobster, but a prawn [PaUnuris), very similar to the lobster in size, color, flavor, habits, and general appearance, except that it lacks the ZOOLOGY. 147 large claws. Crabs are abundant. The abelone or aulone (Kaliotis) is found as far north as Point Reyes, and abounds south of Point Conception. It is a mollusk with one shell, from five to seven inches across ; the shells are beautifully iridescent, and are much used in the arts for buttons, knife- handles, inlaying, &c. Many vessels are engaged in fishing for them. The abelones stick to the rocks and to each other, collecting in some places in masses two feet thick ; the fisher- men break them ofi" from the rocks with a spade. When the abelones do not suspect danger, they loosen their hold and raise their shells from the rock, and then the fisherman may easily thrust his spade down along the surface of the stone ; but if he alarms the abelone beforehand, he finds the shells fastened down to the rock with great power, and all the strength of a man is scarcely sufficient to pry one of them off". The meat of the abelone is eaten by the Chinese, who dig them; the dried meat resembles horn in its color and hard- ness, and in shape looks as though it might be the hoof of a calf. The shrimp ( Crangon francisconim) is found in the bays of California, and was very abundant a few years ago, but lately is getting scarce, at least in San Francisco Bay. § 126. Rexjtiles. — The snakes of California are not large, numerous, nor remarkable. Only one of them, the rattlesnake, is poisonous. The scorpion is found in the warmer portions of the state, but is not abundant. Tarantulas are common in Calaveras, Mariposa, Fresno, and Tulare counties. They belong to the same genus with the spiders, but the body grows to be three inches long and an inch wide, and the entire length from end to end of out- stretched legs is five inches. The body and legs are covered with silky, brown hair. • The tarantula eats little insects of various kinds, but, unlike most other spiders, has no net. It lives in a hole in the ground not much larger than itself when pressed into the smallest compass, and the hole is covered by [ 148 RESOURCES OF CALIFORNIA. a little door on a binge, which closes by its own weight or by a spring. In the top of the door are several little holes, into which the tarantula can insert its claws when it w^ishes to en- ter ; and so quick are its motions when terrified, that it often disappears suddenly under the eyes of men pursuing it, and they have great difficulty in finding its hiding-place-. The door fits tightly, and is larger on the X)utside, so that it never sticks fast. The bite of the tarantula is poisonous, but not fatal— or at least has never, so far as I know, proved fatal in California. It rarely bites men, and generally flees when it discovers their approach. The tarantulas have dangerous enemies in several species of wasps, the females of which kill them by thrusting eggs into their bodies. When the larvae of the wasp are hatched, they make food of the carcass. So soon as the taran- tula dies, the wasp drags it to her hole, usually the deserted burrow of a spermophile, where she may collect twenty or thirty dead tarantulas in one season. There are three differ- ent species of these w^asps; one kind is blue, another yellow. Sometimes the wasp darts dowm repeatedly upon the taran- tula, and does not touch him except wath her egg-planter, de- positing an egg at every thrust. On other occasions the two grapple, and the wasp continues to insert her eggs until the tarantula dies. The editor of a newspaper of Mariposa thus describes the killing of a tarantula : " Some of our readers may have heard of the tenacity with which the venomous tarantula is pursued by an inveterate enemy, in the form of a huge wasp —invariably resulting in the defeat and death of the former. We were an eye-witness to one of these conflicts last week, Avhile on a ramble among the adjacent hills. This is the se.i- Bon when the poisonous tarantula leaves his well-fashioned abode to perambulate the dusty roads and smooth paths so often trod by the industrious miners, and about their haunts a dozen or so may be seen any day, of this hideous enlargement of the spider-race, within a circuit of a few yards, leisurely wending their way along the roads and by-ways. Often have ZOOLOGY. 149 we marked, with attentive curiosity, his awkward gait while lifting his long, unwieldy legs above the short blades of grass, and wondered for what uses and purposes this ugly little mon- ster was placed upon this beautiful globe. Vriiile attentively watchinjT the motions of one of these insects durinof our walk, we were much surprised to see the object of our attraction suddenly stop short in his wanderings and raise itself up to its full hei^^ht, as thouc^h watchinsr the cominsf of some unwelcome visitor. We at first supposed that it had just espied us, and was expecting danger at our hands ; but upon our retreating a few steps, he quickly crouched behind a tuft of dried grass, and remaining very quiet, seemed to make himself as small as pos- sible. A slight buzzing was heard in the air, and in a moment a wasp passed near, hovering on the wing over his trembling victim, the much-dreaded tarantula. Like some bird of prey, the was^) remained thus poised a moment, and then, quick as thought, darted down upon the enemy, and stung him many times with great rapidity. The tarantula, smarting under the pain, began a retreat, with all the speed of which he was ca- pable ; but the wasp hung over him with wonderful tenacity, and again and ao^ain struck him with his venomous stinsr. Gradually the flight of the tarantula became slower and more irregular, and at length, under the repeated thrusts of his con- queror, he died, biting the grass with his terrible fangs." Locusts and grasshoppers are abundant in the valleys ; mus- quitoes in the tules, and along the streams in the Sacramento Basin ; and fleas everywhere. § 127. Honey -Dew Aphis. — Among the noteworthy insects of the state is one which secretes a sweet liquid called " honey- dew," and deposits it on trees. It is transparent, thick like honey, and sweet, sometimes with a bitter after-taste, but more frequently having a flavor like parched corn. The leaves and twigs are covered with it, the deposit usually being nearly even, occasionally in spots or drops. The honey-dew is more frequently found on oak-trees than on any other tree or bush ; and oftener in dry seasons, and remote from the coast, than in 150 RESOURCES OF CALIFORNIA. wet weather or within the reach of the sea-fogs. A kinrl of molasses may be made by breaking off the twigs covered with the secretion, and boiling them in water. Honey-dew is found in most countries where the soil is bar- ren or the climate dry, and may be the same with the manna of the Hebrews. It is known, too, that various insects secrete jsweet liquids ; and some of the Aphis genus are kept as milch- cows by the ants, which stroke them down or tickle them witli their antennae, when they want some of the sweet milk, and the captive Aphis obligingly squeezes out the secretion tlirongh her sides, which is industriously gathered by the milk-ants. Note. — Nearly all the information about the quadrupeds and birds of Cali- fornia, heretofore printed, may be found in the papers of Dr. J. S. Newberry and Professor S. F. Baird, in the United States Pacific Railroad Survey Ee- ports. Most of my information about the fishes and fisheries, and much even of the language, is derived from the conversation of Dr. W. 0. Ayres, of San Francisco ; and I hope that, as he is the most competent man, he will some day treat the subject in a special work. AGRICULTFEE. 151 CHAPTER YII. AGRICULTURE. § 128. General Remarks. — Of the 160,000 square miles in the area of California, about 60,000 may be tillable; of which 16,000 are in the coast valleys, 30,000 in the low lands of the Sacramento Basin, 12,000 in the Sierra Nevada, and 2,000 in the Klamath Basin : while the 25,000 square miles of the Great Bivsin, the 15,000 of the Colorado Desei*t within the limits of this state, 30,000 of the Sierra Nevada, 26,000 of the Coast Mountains, and 6,000 of the Klamath Basin, may be put do^vn as unfit for the plough. The 60,000 square miles of tillable land contain nearly 40,000,000 acres, but only 1,000,000 are cultivated in the state : of the remaining 39,000,000, one-fourth have a soil very thin, or not fertile because of the presence of alkaline substances ; one-half are too remote from market, even where the soil is good ; and a considerable portion is tied up in lawsuits, so that the ownership is doubtful, and the claim- ants dare not improve it for fear of losing the improvements. Only a small portion of the state is, therefore, fit for the plough. Not more than one acre in ten could now be tilled profitably, and I suppose that not more than one acre in four wiU be tilled during this century. As compared with the great agricultural states of the Mis- sissippi valley, in so far as relates to the proportion of rich land fit for the plough, California is at a great disadvantage, and is probably inferior in this respect to every state on the Atlantic slope of the continent. In Illinois and Indiana, nearly every foot of land has a rich soil and a level position. Again. Cali- 152 RESOURCES OF CALIFORNIA. fornia is at a great disadvantage as compared with her sister- states east of the Rocky Mountains, in the proportion of land fitted for growing a variety of crops. In the northern part of the Mississippi valley, nearly every acre will produce all the main articles of cultivation — fruits, maize, potatoes, and gar- den vegetables, as well as wheat and oats. In this state, how- ever, of the 40,000,000 tillable acres, at least 30,000,000 are so dry, that they cannot, because of the want of moisture, and the impossibihty of irrigation, be made to produce any crop save small grain ; and of the remaining 10,000,000 acres, three- fourths w^ill not yield fruits, maize, potatoes, pumpkim?, or gar- den vegetables, without irrigation. These are undoubtedly very serious drawbacks to the agri- culture of the state, but we have great advantages in many other points. The climate in the valleys, for instance, is so warm and the sky so clear through the Avinter, that vegetable life upon moist ground is almost as active in January as in July ; and our trees and shrubs have nearly tmce as much time to grow and mature as in the free states of the East, where frost reigns from October to May. It is a well-known fact that California has produced larger specimens of garden vegetables, more thrifty growth and rapid development of fruit-trees, and larger crops of small grain to the acre, than any state in the Union, and many persons have supposed our soil to be richer. This supposition is erroneous, as I am satis- fied ; the superiority of the Californian productions is owing to the more favorable climate. I am not aware that any com- parison of our soils has been made by chemical analysis with those of Illinois, Missouri, Indiana, and Ohio ; but the proba- bility is, that the latter are more fertile. The loam is deeper ; the vegetation has been gi*eater, and it has enriched the soil by the accumulation of its decomposed remains through thou- sands of years ; whereas in the valleys of California, the vege- tation is comparatively scanty, and the air is too dry to permit a decomposition of wood or grass to enrich the soil. The bot- tom-lands of the Sacramento and San Joaquin are far inferior AGRICULTUKE. 153 in depth, blackness, and fertility of loam, to tlie valleys of the Miami, Wabash, and Illinois Rivers. § 129. Agricultural Districts. — Let us now consider the dif- ferent districts in the state suitable for agriculture. These dis- tricts, as I have said before, compose only a small part of Califor- nia, and have strongly-marked boundaries. They are nearly all valley-land, shut in by mountains. The Great Utah Basin has very little tillable land in the state ; there are small patches of fertile soil, but too slight to deserve special mention. The Colorado Basin is in about the same condition. It is possible that a considerable tract of land will be rendered fit for tillage by turning the Colorado into the low part of the desert ; but this is a remote contingency, and we have no accurate infor- mation about the character of the soil vvhich it is proposed to irrigate in this manner. In a few little valleys, however, just at the eastern foot of the Coast Range, the soil is fertile, and the climate so warm, that fruits ripen six weeks earlier than on the western side. The laro-est tracts of tillable land in the Klamath Basin are the Scott and Shasta valleys, each about thirty miles long and four w^de. They are elevated from three to four thousand feet above the sea ; the winters are severe, and frosts common in spring and autumn, and not rare in summer. Most of the soil is a gravelly clay, with a rich, sandy loam, along the im- mediate borders of the streams. Wheat, oats, apples, and potatoes, do Avell ; but maize, peaches, melons, tomatoes, and sweet-potatoes, require a warmer climate. There is some level land in the eastern part of the Klamath Basin, near the Kla- math Lakes, but the soil is barren, and the vegetation like that of a desert. Del Xorte county, which may be said to belong to the Klamath Basin, has 44,117 acres of land, of which 15,240 are covered with redwood, 7,277 with spruce, 19,204 are prairie, 2,400 are sand-ridges, and 4,712 are in la- goons. Most of the redwood land is level and fertile, but the timber is dense almost beyond example, and could not be cleared profitably, because all the redwood stumps thi-ow out 154 RESOURCES OF CALIFORNIA. sprouts, which grow up to trees. Much of the prairie-laud is tfeitile and suitable for cultivation, but it is remote from the market. Klamath and Trinity counties are almost destitute of valley-land. Both, however, have numerous small spots of rich soil in their mountains, and both have a mining popula- tion who must be fed, and have the means and disposition to pay well for the necessaries and delicacies of life. The farms mu«t be small, but the farmers are protected by the rugged mountains from the competition of those in the large valleys. Hay -Fork valley, one of the best little tracts of tillable land in Trinity county, is three thousand six hundred feet above the sea-level. The largest tract of level land in the plateau of the Sierra Nevada is the valley of Suisun River and Honey Lake, about sixty miles long and ten wide. The elevation is about four thousand five hundred feet above the sea; much of the soil is sandy and alkaline, with no indigenous vegetation save the worthless wild sage. Portions of the soil, however, are fertile, and there are a number of farms under cultivation. Honey Lake valley has the advantage of proximity to Washoe, and good roads for communication. There are 115,000 acres in the valley, of which 20,000 are swampy, at least in w^et sea- sons. Eagle Lake valley is about one-third the size of Honey Lake vallev, and of similar soil. All along the western slope of the Sierra Nevada there are little spots of fertile soil, well suited for cultivation ; but with the exception of a few, they are too small to deserve special mention. The soil is usually a red clay or a black loam. The largest tillable spots on the western descent of the Sierra Ne- vada are in Plumas county. Sierra valley is forty-five miles long by six wide, and is drained by a tributary of Feather River. Much of the land is barren sand ; much is tule-swamp, and only a small portion is fit for tillage. No water flows from the valley after July. The Big Meadows contain 100,000 acres ; Beckworth's valley, 90,000 ; Indian valley, 20,000 ; Mountain Meadows, Red Clover valley, and Mohawk valley, AGKICULTURE. 155 10,000 acres each ; and American valley, 5,000. In all of tliera the soil is very sandy, but not barren. They are from three to five thousand feet above the sea ; all shut in by high moun- tains; and all containing a considerable portion of swampy land. The low land of the Sacramento Basin comprises 20,000 square miles — about 3,000,000 acres. The Sacramento valley has several benches. The lowest bench is about twenty feet above the low-water mark of the river, and has a soil of sandy loam, richer immediately along the stream than farther off. The next bench, very irregular in height and width, has a soil of red, gravelly clay, which extends back to the mountains. In some places this clay becomes very soft in wet seasons — so soft, that weak cattle may mire down in it and be unable to extricate themselves. I knew a case where a team of weak oxen, exhausted by hard driving and scanty food, sank down in a wet gravel-ridge, so that only their heads and a little of their necks and shoulders appeared above-ground ; and passing the place some months later, when the ground had become as hard as clay and gravel ever are, I saw the six bare skulls of the oxen resting with their chins on the earth where they had sunk down, and behind them were the projecting spines of the back-bone, with the yokes still on the necks of each pair of oxen. This gravel is seldom cultivated at present, but in many places it will produce good crops of barley. It forms at least one-half of the Sacramento valley. Yery little of it can be irri- gated ; and the general belief is, that no corn, potatoes, garden vegetables, fruit, or grapes, can be grown on it without irriga- tion. The sandy loam produces large crops of wheat, barley, and oats, without irrigation. Fruit-trees and grape-vines thrive without it after they grow to be tt.ree or four years old, but in most places require it till they have taken a good start. Garden vegetables cannot be grown witliout irrigation, unless planted very early, and of such kinds a,s ripen before July. In the level valley there are no springs, nor are there any artesian wells ; so the onlv method of gettino: water is by pumping it 156 RESOURCES OF CALIFORNIA. up from common wells, for which purpose windmills are ex- tensively used, and thus most of the water used for irrigation is obtained. A large part of the valley, especially of that near the rivers, is subject to overflow; and about once in five years a flood comes, sweeping away houses, fences, and cattle, de- stroying gardens, and covering the earth with a thick clay, which, instead of enriching the soil, is far poorer than the an- cient deposits of sandy loam, made before the miners had com- menced to tear down the mountains for their golden treasures. In these times of flood, so much of the valley is covered with water, that it looks like a great lake, and the pilots of the river steamers know the channel only by the rows of trees along the banks, for the banks themselves are completely hidden from sight. The flood rarely comes earlier than January or later than March. The bottom-lands along the Feather River are considered richer than those near the banks of the Sacramento. Tribu- tary to Sacramento valley on the western side is Cache Creek valley, about twenty miles long by five wide ; and connected with it is Clear Lake valley, a basin nearly circular in shape, and twenty miles across, surrounded by mountains. The lake is about one thousand feet above the sea. South of Cache Creek, and also tributary to the Sacramento valley, is Putah Creek, which drains Berreyesa valley, twenty miles long by two wide. These little valleys have very rich land ; and being shut in by near mountains, the soil is much moister than out in the open plain. The nearer to the coast and the farther north, the greater the moisture as a general rule ; and it may almost be said that the value of the land depends upon the moisture. In the northwestern corner of the Sacramento Basin, alonir the banks of Cottonwood Creek, there are some beautiful, moist, and fertile little vales. The Sacramento valley has very few trees, save along the banks of the streams and stream- beds, where oaks, sycamores, laurels, willows, buckeyes, birch, and Avild grape, are the principal growth, marking in summer AGEICULTTJEE. I5l the places where the Avater rnns in winter. The only trees growing away from the watercourses are oaks, which are usually found in groves, and almost invariably without under- growth. . In the Sacramento valley there are about two hundred square miles, or one hundred and twenty-eight thousand acres, of tule-land, most of it above high tide, and covered by water only in times of flood. Very httle of it has been drained or cultivated, and therefore we do not know its value. All the tule-land is covered five or six feet deep with water in times of flood. The northern part of the San Joaquin valley is much like the southern part of the Sacramento valley. When the San Joaquin River approaches within fifty miles of Suisun Bay, it divides into three channels, which are separated from one an- other by islands of low tule-land. In times of high flood, the river spreads out and covers a space fifteen or twenty miles wide. There is less gravel and clay but more sand in the San Joaquin valley than in the Sacramento valley ; the soil is drier, and contains more of alkaline substances, and the vegetation is more scanty. From Pachecos Pass across to Firebaugh's Ferry, a distance of about fifty miles, there is not a tree, and in the autumn the country looks like a desert. At Fresno City the soil is nearly a pure sand, and the river at low water is not more than six or eischt feet below the surface of the plain. From the bend of the San Joaquin River, southward, a district sixty miles wide by one hundred and fifty long, most of the soil is a barren sand, in many places covered with an alkaline efflorescence. The country about Kern River is very desolate, and be- tween that river and the Tejon Pass is a desert plain, covered with a scanty and useless vegetation. East of Tulare Lake, however, there is some rich soil, particularly in the " Four- Creek country," where the Cahuilhi River, issuing from the mountains, divides into half a dozen streams, which spread out over a space twelve miles wide, and then unite again, filling a 158 RESOURCES OF CALIFORNIA. large tract of fertile land with abundant moisture. Tulare Lake is fifty-seven feet above Fresno City, and might be drained, and its land converted into cultivated fields, but whether with a profit is a question now unanswerable. This country is so remote from the main centres of population, that probably the chief occupation for residents here must be the breeding of sheep and cattle. Turning our attention now to the valleys in the Coast Moun- tains, we find that in all the low land between latitudes 39° 30' and 40° 40', the soil is a rich and moist loam, very favorable for j^asture and for maize, but not so well suited for small grain. In some valleys the season is six Aveeks later than it is across the mountain in the Sacramento valley. Russian, River valley produces more maize than all the remainder of the state. Lying between the bend of Russian River and the head of Petaluma valley is Santa Rosa plain, which has a soil of rich sandy loam, excellent for grain, and probably favorable for the grape. Near the mouth of Russian River is the plain of Bodega, the best place in the state for potatoes. The soil is a light, sandy loam, which is kept moist by the sea-fogs. Peta- luma valley is the chief dairy district of the state. The soil is a rich, moist loam. Sonoma valley has a soil of red gravelly clay near the mountains, and a warm, sandy loam near the creek. This is the chief gi'aj^e district in the northern half of the state. Much of the soil is too thin to produce good crops of wheat. The grape is grown without irrigation, the distance from the ocean (about twenty-five miles) not being so great as entirely to cut ofi:' the fogs. The bed-rock is in some places trap, in othei'S sandstone, and in others magnesian limestone. The latter is supposed to be particularly favorable to the growth of the grape. Next to Sonoma valley is Napa, which has a deep, clayey soil, the strongest in the state, and therefore the best for wheat. In proportion to its size, it produces more wheat than any other part of the state. The upper part of the valley has a great deal of gravel, and may be good for grapes. A larger AGRICULTURE. 159 proportion of the land is cultivated in ISTapa valley than in any other part of the state, and the cultivation is more thorough. Suisun valley has a rich, sandy loam, good both for barley and wheat. Yaca valley, a small vale near Suisun, has a very warm, fertile soil, and is shut in by the hills from the wind. It will be an excellent place for fruit, and every thing will ripen early there. South of the straits of Carquiuez is Diablo valley, which has an excellent soil for w^heat and barley. So also has San Ramon valley, but the fruit has been badly nipped by frost during tlie last three or four years. Amador valley has a soil of rich sand at the sides and strong loam in the centre, all of it moist and fertile. Livermore valley, which may be consid- ered as the eastern half of Amador, is a bed of gravel, of little value for tillage. Suiiol valley has a rich, sandy loam. The Alameda plain, on the eastern side of San Francisco Bay, from San Pablo to San Jose, is one of the richest agricultural dis- tricts in the state ; the soil is fertile — in some places clay, in others sand. The soil on the western side of the bay is similar in character, but there is not so much of it. The lower part of Santa Clara valley has a fertile, black, sandless loam, changing to sand and then to gravel, which last is abundant toward the head of the valley, where very little of the land is tilled. The principal fruit district in the state is in the vicinity of San Jose. The plain east of Monterey Bay, in Santa Cruz county, has a fertile soil, and a climate peculiarly favorable to beans ; excel- lent crops of wheat and barley are also grown here. The soil of Pajaro valley is one of the richest and strongest in the state, and its crops of wheat and potatoes are unsurpassed. The Sa- linas has a rich, sandy loam in the lower part of its valley and near the river, but the sides and head of the vale contain much oravel ; the climate and soil are very dry, and only a small por- tion of the land is cultivated. The Cuyama, Santa Inez, and Santa Clara River valleys, are sandy and dry, and have but little tillage ; the last-named valley has a soil that is in places almost pure sand, too thin to secure a covering of grass in a 160 RESOURCES OF CALIFORNIA. wet winter. Most of the level land in Los Angeles, San Blt- nardino, and San Diego connties, is sandy and dry, and very little of it is cultivated. Irrigation is necessary for fruit, vines, and vegetables. Wheat and barley do not produce well. Los Angeles is the principal graj^e district in the state ; the largest vineyards are planted in the bottom-lands of the Los Angeles, S.in Gabriel, and Santa Ana Rivers, where the soil is almost pure sand : and yet vineyards which have been in bearing twenty-five years, and have never been manured, are now as productive as ever. Allow a stream of water to run twenty- four hours through a field, and at the end of that time the bot- tom of the ditch will contain nothing but white sand, all the earthy particles in the soil having been dissolved and carried away. At the Monte the San Gabriel River sinks, and, after flowing two or three miles under-ground, reappears. The place where it sinks is very moist, covered with abundant vegetation, and, after Russian River vaUey, is the best district in the state for maize. § 130. Agricultural Produce. — California has 1,000,000 acres of land in cultivation, about six-tenths of which are used for growing grains and roots employed as food for men and do- mestic animals. Of these grains and roots in 1860 (the agri- cultural statistics for which year were more fully reported than those of 1861) the following amounts vrere grown, namely: 5,700,000 bushels of barley; 5,000,000 of wheat; 1,500,000 of oats; 1,500,000 of potatoes; 500,000 of maize; 65,000 of beans; 55,000 of peas; 55,000 of sweet potatoes; 50,000 of buckwheat, and 40,000 of rye, making an aggregate of 14,- 470,000 bushels — an average of twenty-four bushels to the acre, and, estimating the population of the state at 400,000, an average of thirty-eight bushels to the person. I purposely omit the consideration of all articles not enumerated in the list, either because we have no statistics, or because the inser- tion would serve rather to confuse than to instruct. We grow very few roots of the turnip kind as food for cattle. Examining, then, the amounts of the crops above mentioned AGRICULTURE. 161 in their proportion to the total 14,470,000 bushels, we find that arley forms 39 per cent., wheat 34 per cent., oats 10 per cent., potatoes 10 per cent., maize 3 per cent., and peas, beans, sweet potatoes, buckwheat, and rye, about one-half of one per cent, each. This proportion will be found to differ greatly from that of any other country. Compare our state with Ohio, which may fairly be considered as a representative of the free agricultural states of the Union. Ohio has 10,000,000 acres under cultivation — that is, ten times as much as California — and, according to the census of 1850, in the previous year pro- duced 92,644,000 bushels of the above-mentioned articles, six times as much as California. The population of Ohio was then 1,980,000 ; so the yield was an average of forty-six bushels to the person. Coming down to particulars, we find that in 1849 Ohio produced 59,000,000 bushels (or 63 per cent.) of maize; 14,000,000 bushels (15 percent.) of u'heat ; 13,000,000 bushels (14 per cent.) of oats; 5,000,000 bushels (5 per cent.) of pota- toes; 638,000 bushels (one-half of 1 per cent.) of buckwheat; 425,000 bushels of rye, 354,000 of barley, 187,000 of sweet potatoes, and 60,000 of peas and beans. Comparing the pro- portion of the several items to the total of the crops, we find that California grows eighty times as much barley as Ohio, twice as much wheat and potatoes, tw^elve times as much peas and beans, and only one-twentieth as much maize. The pro- portion of oats, buckwheat, and rye, is about the same in the two states. § 131. Rotation of Crops. — Rotation of crops, as the phrase is understood in the Atlantic states and Europe, receives very little attention from the farmers of California, and indeed is im- possible on the greater part of the land, because its dryness will not permit the growth of roots or common grasses. The soil is too dry for corn, potatoes, turnips, clover, and timothy or herd's grass. Peas and beans yield well in only a few lo- calities. Alfalfa or lucerne will thrive, but it needs several years to get deep root and make a thick sod. Horses and cattle find food in the open plains and hills throughout the 162 n K S O U R C E S OF CALIFORNIA. year; and the wild oat is cut for hay. The formers generally are anxious to make as much money as possible, and as soon as possible, without regard to the future value of the land. Some of them are not permanent residents of the state, and intend to leave it so soon as they can get a certain number of dollars together ; others are farming land the title of which is in dispute, and, as they feel uncertain about its ownership, they are indifferent to its exhaustion. Many of them come from the Western states, where the land had not, previous to their migration, become poor ; and as rotation of crops had never been a necessity within their experience, they have never adopted it. The soil of California is not exhausted ; much of it will con- tinue tc produce large crops of small grain without interrup- tion and without manure for a score of vears to come. Pre- vious to 1853, the valleys w^ere filled Avith cattle, and their manure had contributed for a long time — along the southern coast for half a century — to enrich the soil. The prominence of barley in Californian farming is owing to the facts that it is an almost certain crop, j^roduces largely, can be grown on all the cultivated land in the state, yields good volunteer crops, is excellent food for horses, can be kept for years, and always commands a market abroad. § 132. Ploughing. — Ploughing commences with the first heavy rain. The heat and drought of summer and autumn bake the ground, and render it too hard for the plough ; so the farmer must wait for the rains. The sooner they come, after the first of October, the more convenient for him, and the more work he can do. The rain must be sufiicient to wet the earth down six or eight inches deep ; a little shower will not suffice. The soils of loam and clay are so hard, that no ordi- nary plough is strong enough to break through them ; and ploughing would do no good, because the earth would be iu large clods, which would furnish little nutriment to the grain. § 133. Adva?2tages, etc. — The Californian firmer has a great advantage over those of the ISTorthern Atlantic states, in the AGRICULTURE. 163 mildness of the winters. Here we have no snow or ice, and no time is lost because of cold. Neither are our frosts so se- vere as those east of the Mississippi. But, on the other hand, firmers in other parts of the Union have a great advantage over us in the security of title and the equal division of the land among the tillers of the soil. Here most of the titles are in dispute, and much of the land held under undoubted title is owned in large tracts by a few persons. Barns are not used in California. The grain, after cutting, is put into a stack, or thrown into a heap, until a threshing- machine can be obtained, and the grain is then placed in the granary. Between harvest and threshing-time there is little danger of rain; and to such slight danger as there is, every farmer exposes himself. Barns in other countries are necessi- ties ; here thev could not be used if we had them. Not unfre- quently the grain, within two weeks after cutting, is stored in a warehouse in San Francisco ; often it is left lying in sacks ujDon the field until it is sold — a period of months. In August and September, the square piles of white sacks in the stubble- fields are a common and prominent feature of the Californian landscape in the farming districts. The straw, elsewhere saved, is usually burned here; and a most improvident practice it is. Not more than a dozen or two of farmers save the straw. The others burn it after the first rain, when there is no danger of the fire spreading ; and the columns of smoke rising all over the country make a sin- gular aj^pearance. Farms in California are usually larger than those in the East- ern states, and manv of the ranches — containing; from ten to fifty thousand acres — are large enough for principalities. As our valleys are not covered with sod, so the first plough- ing is nearly as easy as any of the subsequent ones ; and the severe task of breaking prairie, so common in the states of the upper Mississippi valley, is unknown here. § 134. Fences. — In the matter of fences, the Californian farmer is at a disadvantage, as compared with his Eastern 164 RESOURCES OF CALIFORNIA. brethren. Throiigliout tlie United States, the system has pre- vailed of permitting horses, cattle, sheep, and hogs, to run at large, with no right of indemnity for any damage which they might do in cultivated fields, unless surrounded by a " lawful fence." This may be a good system for the pioneer, who tills little land, and wishes his horses and cattle to have a wide range ; and it was well suited to the pastoral life of the Span- ish Californians previous to the American conquest : but it is of doubtful policy as applied to the present condition of affairs, at least in the principal agricultural valleys, where all the land is under plough. For instance, in the Alameda plain, along the eastern shore of San Francisco Bay — a district fifty miles long by three wide, and containing one hundred and fifty square miles, of which one hundred and twenty-five are culti- vated— there are five hundred farms, and probably two hun- dred miles of fencing, made at a cost of one hundred thousand- dollars. This is a severe tax upon farming, and it is levied chiefly to protect the grain and fruit-trees from the depreda- tions of horses and cattle belonoins^ to neio^hbors and strano^ers. A farmer would rarely go to the expense of fencing his own cattle and horses out : it would be much cheaper for him to keep them in a yard or stable. The legislature has prescribed what kind of a fence is "law- ful ;" and if any domesticated animal breaks through a lawful fence, its owner is liable for the damage done in the enclosure ; and if the trespass be repeated by any neglect of the owner of the animal, he is liable for double damages. The farmer may take up the trespassing animal as an estray ; but if he injure or kill it, he becomes responsible to the owner. The require- ments of lawful fence are not the same in all parts of the state. In the counties of Butte, Amador, Tuolumne, Calaveras, San Diego, Nevada, San Bernardino, Colusi, Placer, Santa Barbara, Yuba, Shasta, Klamath, Trinity, and Siskiyou, " every enclo- sure" (I quote the words of the statute) " shall be deemed a lawful fence vrhich is four and a half feet high, if made of stoiie ; and if made of rails, five and a half feet high ; if made AGRICULTURE. 1G5 upon the enibarikinent of a ditch, three feet high from the bot- tom of the ditch, the fence shall be two feet high ; said fence to be substantial and reasonably strons;, and made so strong: that stock cannot get their heads through it, and if made to turn small stock [sheep, goats, hogs, &c.], sufficiently tight to keep such stock out. A hedge-fence shall be considered a law- ful fence, if five feet high and sufficiently close to turn stock." In other counties the requirements are so complex and lengthy, that I shall not try to describe them all. In Marin, Alameda, Sacramento, San Francisco, Stanislaus, Yuba, Santa Clara, Yolo, San Mateo, Santa Cruz, San Joaquin, San Bernardino, Sutter, Santa Barbara, San Luis Obispo, Los Angeles, Tuolumne, Te- hama, Colusi, Butte, Xapa, Humboldt, Merced, Trinity, Mon- terey, and Solano, hogs are not permitted to run at large ; or at least any person finding them trespassing upon his " prem- ises"— which means land, whether enclosed or not — may take them up, keep them at the expense of the owner, and treat them as est rays. Board-fences are the best. They are usually made fiye feet high, with redwood posts set eight feet apart, and fiye spruce boards six inches wide and an inch thick in each panel. Such a fence, well made, costs fiye hundred dollars a mile. Worm and post-and-rail fences are common near the redwood districts — for instance, in Sonoma, Mendocino, Humboldt, Marin, Xapa, San Mateo, Santa Clara, and Santa Cruz counties. The farmers generally make their own fences of these kinds, and the cost is of time, not money. When the work is done by the job, it costs from three to six hundred dollars a mile, according to the distance and position of the timber, and the quality of the wood ; the price increasing in proportion as the trees are far off, or situated in deep canons, and as the wood is tough antlnct witn the advance of years. Tn the fall there is another season of rodeos, to brand such calves as may have escaped notice at the spring rodeos, or may have been too small to be branded. The rancheros sometimes have a mark in addition to their brand, such as slitting the ear or cutting a notch in the dew- lap. A drawing of the mark must be deposited in the county recorder's office. It is contrary to law to cut off the end of the ear, or to cut it on both sides so as to bring it to a point ; for those modes of marking would give opportunities to cut away the marks of other people. The bull-calves are usually altered at the rodeos, as well as branded and marked. The cattle on many ranches are touched only twice in their lives by the hand of man — first, when they are branded ; and next, when they are slaughtered. § 160. Early Maturity of CaUfornian Cows. — The cows calve almost invariably before they are two years old, frequent- ly before they are eighteen months, and sometimes before four- teen months. They generally arrive at maternity a year sooner than in the Atlantic states. It is said that sucklins; heifers have been seen to take the bull. The Spanish rancheros have eight or ten bulls to a hundred cow^s ; the Americans usually four or five. The calves suckle from six to ten months ; that is, from January or February, when they are born, until No- vember, when the pasturage is very scanty. The Spanish cows have small udders, and yield little milk ; and notwithstanding their great number in the country, butter, milk, and cheese were very rarely seen on the table previous to the coming of I AGRICULTUPwE. 219 the Americans. American cows are the only ones nsed for the dairy, but many of them are now kept also for breeding alone, and, like the Spanish cows, they are never milked. § 161. Corral and Reata. — The corral is an important part of all cattle-ranchos, and on many of them it is the only enclo- sure. It is a pen, from thirty to fifty yards square, surrounded by a high, strong fence. It is used whenever horses or cattle are to be branded. The reata^ used for lassoing, is a rawhide rope, about five- eighths of an inch in diameter and thirty yards long. It is made of four strips of cowhide, from which the hair has been scraped ; and after plaiting, it is greased and dragged along on the ground after a saddle, to render it pliable. Rawhide is better than any other material, because it has just the proper weight and stiffness for the purpose. A running noose, which slips very easily, is arranged at one end. When the reata is to be used, the noose is made from four to six feet long ; one side of the noose and the reata just outside are taken in the right hand, so that while in the hand the noose will not slip ; the remainder of the reata is held coiled up in the left hand, ready to be let go. The vaquero swings the noose round his head, in such a way as to keep it open ; and when he has a good swing, he lets go, and away it will fly, its whole length. If it catches the object aimed at, the noose draws tight. It is not an uncommon thing for a vaquero to catch a cow at a dis- tance of thirty feet, while she and his horse are both running rapidly; but usually he will get within fifteen or twenty feet, if he can, before throwing his reata. A good vaquero, stand- ing in front of another man, can push the latter back, and the moment his foot leaves the ground, throw a reata under it, and thus lasso him by the leg. When cattle or horses are to be branded, they must be thrown down ; and this is generally accomplished by catching the head with one reata, and a hind- leg with another. § 162. Occasional Starvation. — Nineteen out of twenty of the cattle of California never get any food, save such as grows 220 RESOURCES OF CALIFORNIA. indigenously in the open country, and they always suffer for it. From IMarch to July the pasture is abundant and ex- cellent, and the cattle are fat ; from July to October, in ordi- nary years, the grasses and clovers, though dry and brown, are nutritious, and the cattle still remain in good condition ; but from October to January they grow lean rapidly, and almost every year a considerable number of them die by starvation. Either the grass may be all consumed, or it may be deprived of its nutriment. The first case happens when the grass is very scanty, because of a small fall of rain during the winter ; the second occurs when a heavy rain, lasting a day or two, comes before New Year's day, and is followed by cold dry weather. The rain takes away the palatable and nutritious qualities of the old grass, and the cold and dry weather pre- vents the starting of the new grass, and between the two the cattle suffer. In 1856, seventy thousand head of cattle died in Los Angeles county alone by starvation, one-third of the entire uumber in the county. The state has not one large cattle-ranch surrounded by fence, and therefore, if a man owns good pas- ture land, the cattle of other people come and eat the grass, and later in the season his own must suffer. It is impossible for the vaqueros to drive away the strange cattle, because they enter the ranch on every side eveiy day, and if the grass be much better than on adjoining ranches, they will, if driven away one day, return the next. The proper and profitable method of managing an extensive cattle-ranch, is to have it all fenced in and divided off into a few large fields, in which the cattle could be pastured at different seasons. It would also be a source of profit to have hay for them or green alfalfa in the early winter, so that there would be no danger of a reduction to skin and bone : for it costs thrice as much to replace as to preserve a pound of flesh. Spanish cattle, when slaughtered between September and February, are usually very thin, and in the Atlantic States it would be grossly impolitic to send such animals to the market. § 163. Imported Cattle. — The great majority of the cattle AGEIOITLTURE. 221 in the state are of pure Spanish blood, but there is a consider- able number of American cows and half-bloods, which are constantly increasing in number, while the Spanish cattle are decreasing. Most of the American cattle are in the Sacra- mento basin and the coast valleys north of Monterey, while along the southern coast they are very few in number. During the last four or five years about seventy-five pure- blood Durhams, twenty-five Devons, and four Ayrshire bulls and cows, have been imported across the Isthmus of Panama. The freight on the steamer and railroad, from Xew York to San Francisco, for a bull or cow, is two hundred and seventy-five dollars. The food is carried free of charge, but the owner must find a person to feed and take care of the animal during the voyage. Some of these imported animals are of the best English stock. The better the blood the larger the beeves grow, and the more readily and rapidly they fatten. The Spanish cattle are too uneasy ; they run about so much that they lose flesh. The half breed American cattle are more quiet, the full-blood Ameri- can still more quiet, and the Durham the best of all. But as our beef cattle get no food save such as they pick up in the open country, I doubt whether it will pay to import these pure-blood Durhams to improve the breed. The excellence of the Durham is caused by care in breeding, protection against the weather, and an abundance of good food ; and the excellence cannot be main- tained without a continuance of the same system of manage- ment. The Durham will, in a few generations, cease to be a Durham, if he gets no food save such as he can pick np in the valleys and hills ; but if carefully fed, he will, of course, do as well here as elsewhere. It is said that the Durham needs suc- culent food ; if so, the blood will soon degenerate on the dry grasses of California. The Devon stock, which has been praised by the importers of it as peculiarly fitted to thrive on our in- digenous grasses, has not found much favor. Our dairy cows are the only ones which are well taken care of; and therefore the Ayrshire blood is really more needed, and likely to be better preserved, than either the Durham or Devon. Roots 222 EESO URGES OF CALIFORNIA. are seldom cultivated for cattle ; hay, barley, and wheat-bran, are used for feeding them when kept in the yard. Beeves are never stall-fed in California. § 164. Dairies. — The chief dairy districts of the state are the valleys in the vicinity of the bay of San Francisco. The business is very profitable, but requires a considerable capital. The climate near the coast is very favorable for making butter and cheese. In 1860, according to the assessors' reports, Santa Clara county produced 220,000 lbs. of butter and 300,000 lbs. of cheese; Marhi, 226,000 lbs. of butter and 170,000 lbs. of cheese; Sonoma, 220,000 lbs. of butter and 103,000 lbs. of cheese; Sacramento, 148,000 lbs. of butter and 122,000 lbs. of cheese ; Yuba, 92,000 lbs. of butter and 5,745 lbs. of cheese ; and Alameda, 79,000 lbs. of butter and 103,000 lbs. of cheese. § 165. Sjxmish Horses. — California has about one hundred and fifty thousand horses, of which about one-third are Ameri- can ; one-third wild Sj^anish ; and one-third tame Spanish. The Spanish horses are of the old stock imported, sent early in the sixteenth century from Spain to Mexico, and thence brought to California about eighty years ago. Like the neat cattle, the Spanish horses run wild, and partake, to some extent, of the wild nature. They show their base blood by their colors — mouse color, dull duns of various shades, and calico color, or mixtures of white vvdth red or black, in numerous large spots or blotches, are common ; w^hile chestnut, bright sorrel, blood- bay, and dappled gray, are very rare among them. They are quick, tough, healthy, and unsurpassable for the uses of the rider and the vaquero; but small, lacking in weight, strength, and beauty, and unfitted for the heavy, steady work of the plough, cart, or wagon. They are w^anting in the docility, kindly disposition and steadiness of the well-bred horse ; and they have little of that kind of sense w^iich leads an American horse to be quiet and gentle, even in circumstances strange to him. For California, as it was in 1845, there were no better horses than the Spanish-Mexican. They have a wonderful tough- A a r. I c u L T u K E . 223 nest;, and some of their exploits in ths way of travelling are un- surpassed in the annals of the turf. A number of instances are on record where Californian horses have carried a rider one hundred miles in a day, and that with no food save grass. Sixty miles a day is not an uncommon ride, nor is it considered a severe one Fremont, on one occasion, rode four hundred miles in four days, riding different horses, but driving them -before him from the beginning to the end of the journey. More than half of the brood-mares of the state are wild Spanish ; that is, they live entirely in the open plain, are un- broken, and manv of them have never been touched save when they were to be branded. They are in bands called manadas^ numbering from thirty to sixty mares, which are under the guidance of one stallion or garaiion. He knows every one of his baud, keeps them together, conducts them to what he considers the best pastures, and drives away geldings, stallions, mules, and whatever animals he may dislike. When a vaquero tries to drive the manada into a corral for the purpose of catch- ing some of the band, the garanon will frequently divide them and scatter them about, and render it impossible for the vaquero to get them together ; for while he drives in one place, the stallion is equally busy at another, and the mares fear his teeth and heels as much as the swineing^ reata of the horseman. The garaiion is usually from five to nine years of age. He guards his manada with the most jealous care. It sometimes hap- pens that one garanon tries to take away a mare from tlie band of another, and then a fight ensues, in which the weaker has to suffer a severe bitins: and kicking^, and then lose the ob- ject of the battle too. The manada keeps together for year after year, but when it gets too large, the vaquero will divide it and give a portion to the charge of another garaiion. All the mares foal before they are three years old, whereas in the Atlantic States they seldom foal until a year later. They also breed more regularly than elsewhere, for when mares are kept in stables, they frequently pass seasons without breeding. The foals are branded at the age of three or four months, and 224 RESOURCES OF CALIFORNIA. are weaned at the asre of ei^rht or ten months. The fillies con- tinue to run with the manada, and become part of it. The colts are altered when branded, and continue to run with the manada until they are three or four years of age, when they are broken and put into the caballada^ or herd of broken horses. The Mexicans never broke their mares, and considered it dis- creditable and a mark of great poverty to ride one. § 166. Horse-breaking. — The ]SIexican system of breaking horses is peculiar. They are broken only to the saddle ; for horses were never used before wagons by the Spanish-Califor- nians. The horse having run free all his life, is too wild to be caught Avithout a lasso, or to be approached at first while he is on his feet. He is therefore caught by the neck with one reata, by a hind-foot with another, and then thrown down by pulling the reatas in different directions. A vaquero goes to the horse as he lies down and puts a jdquiraa^ or a kind of halter, on his head. The jaquima is provided with a piece of leather, which can be pulled over the eyes so as to blind the horse, but it is first lifted to let him see. The reatas are taken from the neck and leg of the prostrate horse, and a long rope having been fastened to the jaquima, he is allowed to rise. This is the first time he has been haltered and he dislikes the restraint, but he exerts himself in vain to get loose. After he has tired himself in vain efforts, the vaquero goes up for the purpose of pulling down the blind. The horse is terrified at so near an approach of a man, and trembles with excitement. If he pulls back hard the vaquero sees there is little danger, and slowly advancing and putting his hand to the blind pulls it down over the horse's eyes. But if the horse stand up, it is probable that he w^ill rear up when the vaquero comes near, or strike at him with a fore-foot. Such animals are very dangerous, and are usually allowed to tire themselves by standing without food, or else they are drawn up to a fence or tree, behind which the vaquero can protect himself. So soon as the bhnd is down, the horse is perfectly quiet. He can be rubbed, and saddled, and mounted without a motion. The first thins: after blind- AGRICULTUEE. 225 ing is to put a saddle on him. It is fastened well, the blind is raised, and the full length of the rope given to him. He does not understand the saddle. It may be a carnivorous beast for all he knows. He is terrified at it. He jumps, and snorts, and kicks, rears and pitches, throws himself down, worries himself out, and falls into an agony of despair. After an hour or so of such work, the vaquero advances again, puts down the blind, and the horse stands trembling with fear and exhaus- tion. He is now to be ridden. The rope is fastened under the chin, so that it can be used for a bridle-rein ; the horse's ears are pushed down under the upper part of the jaquima, so that he shall be deaf as well as blind; the saddle-girth is tightened, and the rider mounts. Over the saddle he has a second girth, which is loose enough to allow him to get the point of his knee, bent at right angles, under it. This girth ties him upon the horse. The more he presses the knee outward, the tighter the girth holds him ; whereas by turning his knees inward and straight- ening his legs, he can be free in an instant. Having put his knees under the girth (he does not care for the stirrups and cannot use them) he reaches forward, takes the ears out from under the jaquima, and raises the blind. The horse, as soon as he sees the man on his back, is stricken with a new terror. He immediately commences to jump stitf-legged. He springs up into the air and comes down on his fore-feet with his legs stiff. This is the way in which horses try to shake off panthers, and they resort to the same method with men. The shock would be severe»if the man were not tied down to the saddle, but he moves with the horse and is not hurt with the shock. Some- times a horse will jump thus for hour after hour, and the rider is very well satisfied, for there is no danger in the jumping, and it is very tiresome to the animal. Some horses, after jumping for a few minutes, will commence to run. To this the rider makes no opposition, but practises the horse with the reins to accustom him to guidance. The most dangerous horses are those which rear up and fall backward. In such case the vaquero must be ready to throw off the girth from his knees, 10* 226 RESOURCES OF CALIFORNIA. and aliglit upon his feet as tlie horse falls. After riding for a couple of hours, the vaquero reaches forward, pushes the blind down over the horse's eyes and dismounts. To dismount with- out first putting down the blind would be very dangerous, for the horse would |)robably kick him. He takes oif the saddle, hoists the blind, ties him to a fence or a tree with his head up, and gives him neither food nor water. The next morning he is very stiflf and hungry. The vaquero does not feed him, but pulls down the blind, puts on the saddle, mounts him again, and the scenes of the previous day are re-enacted, though the jumping is less furious. After a couple of hours of exercise, the horse is tied where he can get water and grass. Every day he is ridden. In five or six days he quits jumj^ing. In three months the blind is laid aside. In four months a bit is put in his mouth. This is strange to him, and he jumps stiflF-legged. If the first bit used is American, he will jump again when the liarsher Spanish bit is used. When any thing is wrong he jumps stifi*-legged. During the first month or two his nose will be very sore where the jaquima or halter crosses it, caused by the pulling of the halter in holding and guiding the animal. At the end of a couple of months he learns to follow the guidance of the jaquima almost as readily as afterward the bit. After he has been ridden daily for six months, he has become tame and quiet, and he commences to fatten up again ; for during the first three or four weeks he worries himself so much, with his vain plungings, that he loses flesh rapidly. The Californian horse, when once broken, is kindly in disposition. JHe rarely bites or kicks, no matter how roughly he may be used. After having been broken to the saddle, he must be taught the uses of the reata. The vaquero always carries his reata with him, and the horse soon learns to see it swinging about the rider's head. The reata is first thrown at small calves and then at larger ones, and the horse gradually learns that he can best hold a lassoed animal by presenting his head toward it, and bracing himself back with his fore-feet. The reata is fast- ened to the horn of a saddle, strong enough to hold a bull. AGllICULTUEE. 227 Tlie horse learns to watch the reata ; if it catches, he slackens his pace, or stops suddenly ; if it does not catch, he continues at full speed, while the vaquero pulls up the reata and prepares to throw it again. Tlie saddle and bridle are both peculiar, and necessary to the trade of the vaquero. The saddle-tree, or fuste^ is made of four pieces of wood, two of which are longi- tudinal and rest on the sides of the horse : one forms a hio-h back ; aud the fourth is a fork, which rises in a laro^e strongr horn. The pieces are strongly fastened together, and the whole framework is covered with wet rawhide, which shrinks when dry, and contributes much to its strength. A good fuste is stout enough to hold the strongest bull. The girth is four inches wide, and is made of a number of little ropes of horse- hair, connecting two iron rings four inches in diameter. One of these rings is fastened on the right side of the saddle, by straps running over the front and back of the fuste ; and a similar rino- is fastened in like manner on the left side of the fuste. In this latter ring is a rawhide strap three feet long. When the saddle is to be fastened, this stra^^ runs through the ring at the loose end of the girth, then through the upper ring, then down to the girth ring again ; and the vaquero pulls, and usually draws so tightly that the wide girth cuts into the horse's belly and evidently displaces its contents. When a vaquero is preparing for a day of lassoing, there is no danger that the saddle will slip. The girth has no buckle ab'^ut it, and is made wide to give it strength and to prevent it from hurting the horse. It is placed farther back than in American saddles, and rarely cuts the skin, just behind the fore-legs. Sometimes in lassoing, the animal caught will get oif sideways from the horse, and the saddle must be so firmly in its place, that it cannot move ; and sometimes the vaquero will drop his reata after having caught his cow or horse, and then while his horse is going at full speed he must reach down, supporting himself with one hand on the horn of the saddle and with the other seize the reata. For such feats, the girth must not be loose. The stirrups are of vrood, about three inches wide, and 228 RESOUKCES OF CALIFORNIA. are covered in front with pieces of thick leather, called tapa^ deras, which prevent the feet from slip])ing through. The fuste is usually covered by large flaps of leather called mochilas^ and along the stirrup-straps are pieces of leather called suda- dcras, to protect the legs of the rider from the sweat of the horse's side. Cruppers and martingales are never used by the Spanish-Californians. The bridle is so made that a hard pull on the rein hurts the horse, and a severe jerk will throw him back on his haunches. The bit has an arm projecting about two inches up in the mouth. On ordinary occasions this arm lies flat on the tongue, but when the rein is pulled it rises and presses against the roof of the mouth. The slightest pull, therefore, on a Spanish bridle is felt by the horse, and he will stop instantaneously, though at full speed, if the reins be jerked severely. It may be cruel to the horse, but it is very conve- nient to the rider, and necessary to the vaquero. The common gait of the Californian horse under the saddle is the gallop. He never paces or racks, and rarely tries a sharp trot, but rests himself with a walk or a slow trot. His gallop has an easy motion which does not tire the rider in fifty miles. He has an excellent speed for a race of a quarter a mile, but he cannot run two-mile heats with the thoroughbred, though for a gallop of a hundred miles he has probably no superior. Many of the Californian horses have of late years been bro- ken to the wagon and the plough, and they do very well for farm work, though not equal to American horses. § 167. JBlood-horses. — The American horses, that is the com- mon stock of horses brought from the Atlantic States within the last twelve years, and their oftspring, are large, fine animals, not so healthy and tough as the Californian horses, but lai-ger, more active, stronger and more handsome in shape and color. A large number of stallions and mares of fine blood have been imported, including about fifty thoroughbreds or English racers, two dozen Morgans or American trottei's, and a dozen Clydesdale and Flemish, or heavy cart and truck horses. Some of these horses are valued as hicrh as ten thousand dollars AGRICULTUEE. 229 apiece. The Clydesdale and Flemish are considered the most valuable for crossing with the Californian mares, the offspring being large, strong farm-horses, worth twice as much in the market as the pure Californian. The thoroughbred horses in California are of the purest blood, and some of them have few superiors in speed in any country. § 168. 3Iides. — Xearly all the farm work of California, where drauijht animals are necessary, is done with horses. Mules are too dear and oxen are too slow. A great number of mules and horses are used in packing merchandise in those districts where there are no good wagon-roads. For the or- dinary uses of the farm the mule is preferable to the horse, being longer-lived, more healthy, not so much injured physi- cally or morally by ill-treatment, and contented with much cheaper and simpler food. But the mule is not considered handsome, and the small farmer wants a horse which he can ride, and with which he can take his family out, so he never gets a mule. Mules are now used on very few farms, but I think they will oTadually srain in favor. Few mules are bred in the state at present, but there are some excellent jacks in Contra Costa county and in the San Joaquin valley. § 169. Camels. — Some camels have been introduced into CaHfornia, but they are as yet few in number, and have been here but a short time. Our experience with them is therefore small, and we do not know what value they are to have in the future. They are healthy, increase, thrive on our wild pas- tures, are strong^ and active, olimb our rusfojed mountains as well as horses or mules, carry loads of one thousand pounds each, go three or four days at a time without water, and are readily manas-ed ; but thev have not been tried in a resrular business way, and such trial is necessary before we can tell what they are to be. § 170. Sheep. — The climate of California is peculiarly favor- able to the growth, increase, and health of the sheep. Our mild winters permit them to grow throughout the year ; and it is an accepted principle mong those familiar with the sub- 230 EESOUiiCES OF CALIFOIINIA. ject, tliat a slieep, born and bred in California, is, at two years of age, usually as large and heavy as one of three years, born and bred in tlie Atlantic States. The ewes produce twins and triplets more frequently here than east of the Rocky Moun- tains. The health of the herds is better. No fatal disease has ever prevailed to any serious extent. The " scab" exists in many herds, but in a mild i'orm, and few have died of it. It is the general opinion of sheep-breeders that the sheep bred in California will produce more wool than those of other states. The heaviest unwashed fleece on record, is that of " Grizzly," a French Merino buck. It was fourteen months old, Aveighed forty-two pounds, and was sheared by Flhit, Bixby & Co., in Monterey county, in 1859. Sheej) in California are never kept imder shelter, and except a few of line blood, seldom get any food save such as they can pick up on the open hills and plains. Sometimes lambs are lost with cold, but this is very rare when they are well managed. At night the herds are driven into corrals or pens, to protect them against the coyotes, and to keep them from being lost. On the large sheep ranches, one herdsman is em- ployed for a thousand sheep. There are a few shepherd-dogs in the state, some brought from Australia, others from Scot- land. The word " corral" is understood by these dogs, and when they hear it, they immediately drive the herd to the corral. At the sight of a wolf, they hastily collect the sheep into a dense body, with their tails out and the lambs in the centre. If a sheep turns his head out, the dog bites his knees and makes him turn about. The dog seems to understand that the wolf cannot do much harm by biting the rump of a sheep, but w^ould soon kill it after catching its throat. In most other sheep countries, the sheep-breeder is at great disadvantages as compared with California ; the land is dear ; it must be cultivated ; the sheep must be fed by hand every day during a considerable part of the year ; the herds must be under shelter in the winter ; four or five men are required, on an average, to attend to a thousand sheej) ; the herds are not AGRICULTUEE. 231 SO healthy, do not increase so rapidly, do not grow so large within the first two years, and do not produce so much wool. The land of the sheep ranches in California is not worth more than five dollars per acre, on an average probably not more than three dollars. It follows that sheep-breeding should be very profitable here, and so it is. The ewes, when properly taken cai-e of, have lambs before they are a year old — increase one hundred per cent, every year. The cost of keeping large herds is variously estimated from thirty-seven to fifty cents per head annually, exclusive of the interest of the land used for pasturage. The wool of a good sheep will pay twice the cost of keeping it ; and the wool and lamb together, of a fine- blood ewe, are worth eight or ten times the cost. It is the present custom to sell the wethers for mutton when a year old, but this is bad policy, save with the poorest sheep. The old missions had large herds of sheep, but after the manasrement of those larg^e establishments was taken from the priests and given to civil ofticers, in 1833, the sheep were neglected and most of them were killed. Twenty years later very few were left in the state, but there was a demand for mutton, so lar<]:e herds were driven from New Mexico. These were a very poor stock, but they were for a long time the only sheep that could be had, and they now form the great majority of the sheep in the state. The first attempt to breed sheep as an exclusive business in California, since the Ameri- can conquest, was commenced in 1853, by a poor man who had nothing save nine hundred ewes ; and they increased so rapidly and proved so pi'ofitable, that now, if rei)ort be true, he has ten thousand sheep, sixteen thousand acres of land, and other property to the value of one hundred thousand dollars. Within the last three years many sheep of fine Vjlood have bean imported, and these will gradually swallow up the Mexican stock. The imported kinds are American, Southdown, Aus- tralian Merino, French Merino, and Spanish Merino. Of the two latter varieties there are few save bucks. The prices of sheep fluctuate, but the relative prices of the different breeds 232 RESOURCES OF CALIFORNIA. remain a1)oiit the same. Thus when a Mexican ewe is worth about three dollars, an American is Avorth five dollars, a half- Merino six dollars, a Southdown six dollars, and an Australian Merino twelve dollars. The Mexican sheep produces on an average two pounds of wool per year, worth from five to seven cents per pound ; the American four pounds, worth from fifteen to twenty cents ; the half-Merino six pounds, worth from eighteen to twenty-four cents; the Southdown five pounds, worth twenty or twenty-one cents ; the Australian Merino 'seven pounds, worth twenty or twenty-one cents. These weights indicate the weights of the unwashed fleeces, and the prices paid in this market for unwashed wool. The Californian wool, especially that grown in the southern part of the state, is filled with grease, dust, and sand. In one case, a fleece vreighing sixteen pounds was reduced by washing to six pounds. The finer the wool, and the farther south it is grown, the greater the proportion of dirt. The wool grown in the northern part of the Sacramento valley, is cleaner than that of Alameda county, and that of the latter place is superior to the wool of San Luis Obispo. There are a few Chinese sheep in the state, and much value was for a time attached to them, because the ewes very frequently produce triplets, but it re- quires a good ewe to suckle two lambs well, and twins are sufliciently abundant among American sheep. Sheep-growers are divided in opinion as to w^h ether the French or Spanish Merino be the best sheep for the state. The French Merino grows large, and averages more wool to the sheep than any other kind, but it is said that the Spanish Merino, though smaller, will produce more wool to the acre. About a thou- sand sheep are kept in a herd. One sheep-owner in Monterey county has 30,000 head ; and others have 15,000 and 20,000 head each. The largest sheep county is Monterey, which has about 150,000 ; Solano has nearly as many, and after these come Los Angeles, San Bernardino, and San Luis Obispo. There are about 900,000 sheep in the state, and their number is rapidly increasing. One of the drawbacks of wool-growing AGRICULTURE. 233 in California is, that in the summer the wool gets full of the little burs of the bur-clover, which gives much trouble in wash- inof and cardinG:. Bv sheerius: earlv this trouble is to some extent avoided. Of course the sheep grow lean in the late fall, as do the horses and neat cattle, and some of them die of starvation. The same remarks may apply to high-blood sheep as to other high-blood animals — they must degenerate if they get no cultivated food ; but the stock may be kept up by cross- ing with high-fed bucks of pure blood. § l7l. Sicine. — Swine are not favorite animals in Califor- nia. They increase rapidly and are healthy, and their meat commands a high price, but they do not thrive upon the dry pastures ; they are not permitted to run at large in many coun- ties ; the mast is scanty in the agricultural counties, and grain suitable for feed is dear. It is probable that in a few years great numbers of swine will be bred in the tules, the roots of which they like to eat ; but the tule-lands at present are in wide undivided tracts, and the swine which have access to them soon get lost. The present number of swine in the state is about six hundred thousand. § 172. Poultry. — Poultry command very high prices in this state, but all attempts to breed them on a large scale, have proved unprofitable. Hens are worth from fifty to seventy- five cents each, and esrsrs from twentv-five to fiftv cents per dozen. Chickens are healthv and increase rapidlv in small poultry-yards or farms ; but when more than five hundred are collected a fatal epidemic appears, and they die ofi". The dis- ease seems to be a kind of apoplexy, for it attacks the fattest chickens, and they die suddenly. One large hennery, on the French plan, has been established about eight miles from Oak- land, and it contains one thousand five hundred hens, with accommodations for five thousand. The poultry-yard covers four acres of ground, and one acre of it is separated from the remainder. The hens lay in the lower story of a frame house, which is open on one side. The nests are in a long trough, a foot square, open on top, and separated into nests by partitions. 234 rESOX'P. CES OF califoexia. Each nest has soiiil; hay in it and a mock egg of i^orcelam. Several times in the course of a day, the eggs are taken out and placed in a covered box near at hand. Four or five hens may use the same nest in the course of a day, and if the eggs were left in the nest the warmth might start the development of the chick, and injure the egg for either hatching or eating. It is considered bad policy to let a hen sit on eggs while lay- ing, even if she is to hatch them herself, for some will be far- ther advanced in incubation than others, and then the propor- tion of loss will be great. Over the laying department is the roosting place, which is eighteen feet high, and has the perches so fixed that the droppings of one hen do not fiill on another A stairway leads up from the ground to the roosting chamber In the lower story of another house is the hatching depart- ment, with nests for six hundred hens. The nests are about a foot square, with a door in front, opening on a level with the floor. They are numbered and divided into sections, each of Avhicli has one door, and has hens which commenced sitting at the same date. The hens are fed by sections ; ten, twenty or thirty being let out at a time, and called to eat. When first called they do not understand it, and after they have eaten, they have difficulty in finding their places ; but in three or four days they come out immediately as soon as the door is opened, and when the signal for closing is given, they go to their places without the least confu-ion. About a dozen eggs, usually not more than four, and never more than ten days old, are given to each sitting hen, and of this dozen, nine or ten are hatched on an average. Every nest has snuff in the bottom of it to keep out the lice. When the hen has hatched out her brood, she and they are transferred to the "young-chick room," over the hatching room, where every hen is put in a pen. During the first twenty-four hours the little chicks get nothing to eat ; then they are fed twice on fine bread, after that on boiled rice and corn-meal. They are fed four times a day. When five days old, the chicks, with their motlier, are placed in the Bmaller enclosure of the poultry yard, which has several AGPvICULTUEE. 235 Streams of clear water running througli it, bushes and mustard- plants for shade, and boxes into which the hens can retire for protection against the cold and rain. When the young brood enters the yard, the older occupants, or some of them, make war on it, and one chick in a dozen is slain in these hostilities. After the hen has proved by fighting her right to be there, peace is restored, and she and her little ones are ready to make war on any subsequent intruders. After the chickens are three months old, they are turned into the large yard, where tbey have to struggle for their food and lives, with all the old hens and cocks on the place. In the large yard the chickens are fed twice a day, and four ounces to each chicken per day. The food is wheat, rice, oats, barley, raw meat, cabbage-leaves, sorrel, chalk, oyster-shells, and green mustard. Regularity in the time of feeding is considered a matter of much import- ance. There should be one cock to a dozen hens. The hens commence laying when about eight months old and lay most in their second year. They will continue laying till their fifth or sixth year, but thev are usuallv killed about the end of the fourth vear. Hens that eat esfcrs and that crow are killed. Hens which want to sit when their services are not needed in tliat way, are shut up in the callaboose, kept there one or two days, with no food save green vegetables, ducked several times in cold water and then let out cured. In eio;ht or ten da^s they are ready to commence laying again. A hen will lay fifteen or eisfhteen erecious metal might all be carried off. Quicksilver is not used in the ground-sluice. After the dirt has all been put through the ground-sluice, it is cleaned up in a short board-sluice, or a tom. 190. Long Tom. — The tom or long torn, an instrument ex- tensively used in the Caiifornian mines in 1851 and 1852, but 258 EESO URGES OF CALIFORNIA. now rarely seen, is a wooden trough about twelve feet long, eighteen inches wide at the upper end, and widening at the lower to thirty inches, with sides eight inches high. It is used like a board-sluice, but has no riffie-bars, and at the lower end its bottom is of sheet-iron, perforated with holes half an inch in diameter. This sheet-iron is turned up at the lower end, so that the water never runs over there, but always drops down through the perforated sheet-iron or riddle, into a little riffle- box, containing transverse riffle-bars. A stream of water of about ten inches makes a " tom-head" — or the amount con- sidered necessarv for a tom — throug^h the tom, which has a grade similar to that of a board-sluice. The dirt is thrown in at the head of the tom, and a man is constantly employed in moving the dirt with a shovel, throwing back such pieces of clay as are not dissolved, to the head of the tom, and throw- ing out stones. From two to four m.en can work with a tom ; but the amount of dirt that can be washed is not half that of a sluice. The tom may be used to advantage in diggings where the amount of pay-dirt is small and the gold coarse. The riffle-box contains quicksilver, and as the dirt in it is kept loose by the water falling down on it from the riddle above, a large part of the gold is caught ; but where the j)articles are iine, much must be lost. § 191. Cradle. — The rocker or cradle is still less than the tom and inferior in capacity. It bears some resemblance in shape and size to a child's cradle, and rests upon similar rockers. The cradle-box is about forty inches long, twenty wide, and four high, and it stands with the upper end about two feet higher than the lower end, which is open so that the tailings can run out. On the upper end of the cradle-box stands a hopper or riddle box twenty inches square with sides four inches high. The bottom of this riddle-box is of sheet-iron, perforated with holes half an inch in diameter. The riddle- box is not nailed to the cradle-box, but can be lifted off with- out difficulty. Under the riddle is an "apron" of wood or cloth, fastened to the sides of the cradle-box and sloping down MINING. 259 to the upper end of it. Across the bottom of the cradle-box are two riffle-bars about an inch square, one in the middle, the other at the end of the box. The dirt is shovelled into the hopper, the " cradler" sits down beside his machine, and while with one hand with a ladle he pours water from a pool at liis side upon the dirt, with the other he rocks the cradle. With the water and the motion the dirt is dissolved, and carried down through the riddle, falling upon the apron which cari-ies it to the head of the cradle-box, whence it runs downward and out, leaving its gold, black sand, and heavier particles of sand and gravel behind the riffle-bars. The man who rocks a cradle learns to appreciate the fact, that the " golden sands" of California are not pure sand, but are often extremely tough clay, a hopperful of which must be shaken about for ten minutes before it will dissolve under a constant pouring of water. Many large stones are found in the pay-dirt. Such as give an unpleasant shock to the cradle, as they roll from side to side of the riddle-box are pitched out by hand, and after a glance to see that no gold sticks to their sides, are thrown away ; but the smaller ones are left until the hopper- ful has been washed, so that nothing but clean stones remain in the riddle, and then the cradler rises from his seat, lifts up his hopper, and with a jerk throw^s all the stones out. The w^ater and the rocking are both necessary. Without the w^ater, the dirt coidd not be washed ; and without the rocking, the dirt would dissolve very slowly, and the gold w^ould most of it be lost. The rocking keeps the dirt in the bottom of the cradle more or less loose, so that the particles of gold can sink down in it, whereas if the cradle stood still the sand there would almost immediately pack dowm into a hard floor, over which the gold would run almost as readi- ly as over a board. The w^hole business of washing with a cradle is a repetition of the process already described — some dirt, about one third or one-fourth of what the hopper w^ould hold, if full, is put into the hopper, and while the cradle is rocked with one hand, the other pours in the water. The 260 E E S O U R C E S O F C A L I F O E X I A . cradle is cleaned up two or four times in a day. The clean- ing up is done by lifting the hopper, taking out the apron, scraping up all the dirt in the bottom of the cradle with an iron spoon, putting it into a pan and washing out the dirt, so that only the gold will be left. This last process is called panning out, and will be described in the next section. Most of the gold collects above the upper riffle-bar, including all the larger lumps. If the apron be of rough woollen cloth, some of the fine gold will be caught there. In diggings where the gold is very fine, the hopper is sometime? placed over the lower end of the cradle, and the apron is made twice as long, and with a lower inclination than in the more common form of the rocker. The water for the cradle should be supplied by a little ditch, with a reservoir at the head of the cradle, to contain five or six gallons. The dipper should be of tin, shaped Hke a basin, hold about a gallon when full, and have a handle an inch and a half in diameter, and eight inches long. The difference of height betw^een the upper and lower ends of the cradle should not be more than two inches : a steeper in- clination will make the current runnmg through it too strong, and the gold will be carried off"; and, on the other hand, if the cradle be nearer a level it will be hard to rock, and the dirt in the bottom will pack more rapidly. The amount of dirt that can be washed in a day w^ith a cradle, varies from one to three cubic yards. The dirt is usually shovelled into a pan or bucket, from which it is throw^n into the hopper. The miners usually measure the amount of dirt washed by the number of "pans." One man working alone with a cradle ought to wash from seventy-five to one hundred and fifty pans in a day, and two men will wash twice as much. A pan may contain one-third or one-half of a cubic foot. Two men can work more conveniently with the rocker than one. There is enough work to give constant employment to a cradler and a shoveller. The latter has a couple of buckets or pans, which he fills alter- nately, always keeping one full and near the cradler, so that without moving his feet he can pick it up and empty it into MINING. 261 the riddle-box. If the rocker have only one man, he must stop rocking after washing every pan and get more dirt. This delay is injurious to the process of washing, because it allows the dirt in the bottom of the cradle to harden and pack, and some gold is always lost as a consequence. If the dirt and water be convenient not more than two men can work to a profit with a rocker. But sometimes it liappens that water cannot be led to the claim, and in such case the dirt must be carried to the water, a greater weight of which is used than of dirt. At least three times as much water as dirt is required for washing. If the distance from the hole to the water be not over ten or twenty feet, the miners will usually carry the dirt in buckets ; if farther they will use wheelbarrows ; and sometimes for greater distances pack-mules or wagons. The greater the distance, the more the men required for carrying the dirt. Sometimes, too, it happens that the claim is troubled by water, and then one man may be constantly employed in balino;. It is of great importance in mining with the cradle, to have the cradle j)laced within four or five feet of the hole from which the pay-dirt is obtained, and to have a good supply of water at the head of the cradle, and then to have a good de- scent below the cradle, so that the tailings may all be carried awav bv the water, so as not to accumulate. The rockei- washes about one-half the amount of dirt that can be washed by an equal number of men with the tom, one-fourth of what can be washed with the sluice, and one-hundredth of the amount that can be washed with the hydraulic process; but it is pecuharly fitted for some kinds of diggings. Many little gullies, containing coarse gold in their beds, cannot obtain water for washing except during rains, and then only for a few days at a time. In these guUies the cradle can be used to the best advantage, for it can easily be transported, and it is very good for saving coarse gold. While dirt that would pay from ten to twenty-five cents, was abundant at the surface of the earth in the California n mines, the cradle was extensively 262 RESOURCES OF CALIFORNIA. used, l)Ut now it has been abandoned by the whites, and is left to the Ciiinamen, who think themselves doing well if they make seventy-five cents or one dollar per day. The great difficulty in raining with the cradle, is that the sand will " pack," or make a hard mass on a level with the top of the ritfle-bars, and tlie gold then is lost. So long as the cradle is in motion the dirt does not pack, but when the rock- ing ceases, the mass hardens in a few minutes. If the miner leaves his cradle standing for fifteen minutes, he stirs up the dirt with his sj^oon before commencing again to wash. One device to prevent packing is to put a little block under each end of the rockers, so that at the end of every motion the cradle receives a shock. Quicksilver is sometimes used in cradles, but not usually. § 192. Pan. — The pan is used in all branches of gold min- ing, either as an instrument for washing, or as a receptacle for gold, amalgam, or rich dirt. It is made of stiflT tin or sheet- iron, with a flat bottom about a foot across, and with sides six inches high, rising at an angle of forty-five degrees. A little variation in the size or shape of the pan will not injure its value for washing. Sheet- iron is preferable to tin, because it is usually stronger and does not amalgamate with mercury. The pan is the simplest of all instruments used for washing auriferous dirt. Some dirt, not enough to fill it full, is put in, and the pan is then put under water. The water ought to be not more than a foot deep, so that the pan may rest on the bottom, while the miner inserts his fingers in and under the dirt and lifts it up a little, so that the whole mass is wet. If the water be deep, the pan may be held in one hand while the other is used to stir up the dirt, but it is more convenient to take both. The dirt having been filled with water, the miner catches the pan at the sides, raises that part toward his body, and lowers the outer edge a little, and commences to shake the pan from side to side, holding it so that all the dirt is under water, and so that a little of the dirt can escape over the outer edge. The earthy part of the dirt is rapidly dissolved by the w^ater, MIXING. 263 assisted by the shaking of the pan and the rolUng of the gravel from side to side, and*forms a mud wliicli runs out while clean water runs in. The light sand flows out with the thin mud, while the lumps of tough clay and the large stones remain. The stones collect on the top of the clay, and they are scraped together with the fingers and thrown out. This process con- tinues, the pan being gradually raised in the water, and its outer edge depressed, until all the earthy matter has been dis- solved, and that as well as the stones swept away by the water, while the gold remains at the bottom. Panning is not difficult, but it requires practice to learn the degree of shaking which dissolves the dirt and throws out the stones most rapidly without losing the gold. If the shaking be too mild and slow, the process consumes too much time ; whereas if it be too rajdd and violent, the gold is carried off with the stones. Sometimes the pan is shaken so that the dirt receives a rotary motion. This is the most rapid method of ^v ashing dirt, but also the most dangerous. The pan must always be used in cleaning up the dirt which collects in the cradle, in prospect- ing, and frequently in washing small quantities of dirt col- lected in other kinds of placer milling. Amalgam can be sepa- rated from dirt by washing, almost as well as gold. In panning out, it frequently happens that considerable amounts of black sand containing fine particles of gold are obtained, and this sand is so heavy that it cannot be separated from the gold by washing, wliile it is easily separated by that process from gravel, stones, and common dirt. The black sand is dried, and a small quantity of it is placed in a " blower," a shallow^ tin dish open at one end. The miner then holding the pan with the open end from him, blows out the sand, leaving the par- ticles of gold. lie must blow gently, just strong enough to blow out the sand, and no stronger. From time to time he must shake the blov.er so as to change the position of the particles, and bring all the sand in the range of his breath. The gold cannot be cleansed perfectly in this manner, but the Band contains iron, and the Uttle of it remaining is easily re- 264 RESOURCES OF CALIFORNIA. moTed by a mao^iet. The blower should be very smooth, and made of either tin, brass, or copper. § 193. Dry Washing. — Dry washing is a method of win- nowing gold from dirt. In many parts of the mining districts of California, water cannot be obtained during: the summer for mining purposes. The miner therefore manages to wash his dirt without water. He takes only rich dirt, and putting it on a rawhide, he pulverizes all the lumps and picks out the large stones. He then with a large flat basin throws the dirt up into the air, catches it as it comes down, throws it up again, and repeats this operation until nothing but the gold remains. Of course a pleasant breeze, that will carry away the dust, is a great assistance to the oi^eration. Sometimes two men have a hide or a blanket, with which they throw up the dirt. The process is very similar to the ancient method of separating grain from chaff. The miner who devotes himself to dry washing must be very particular to take only rich dirt, so he scrapes the bed-rock carefully. He never digs very deej) — not more then twenty feet ; and when he goes beyond seven or eight feet he " coyotes," or burrows after the pay-dirt. He may coyote into the side of a hill, or sink a shaft and coyote in all directions from it. This style of mining is named from the resemblance of the holes to the burrows of the coyote, or Californian wolf Coyoting is not confined to the dry wash- ing, but is used also by miners washing with the pan and cradle. One of the Congressmen elected some years ago to represent California at Washington, was a miner at the time of his nomination, and was so fond of coyoting, that he was a'enerallv known as " Covote Joe." § 194. Dry Digging. — Dry digging is that mining where the miner, after using the shovel to strip off the barren dirt, scrapes the pay-dirt over with a knife, picking out the particles of gold as he comes to them, and throwing away the earthy matter. This is a slow process, but in rich^ placers may be profitable. The miner is, of course, particular to examine all the crevices in the bed-rock ; and if the mateiial be slate, he MIXING. 265 digs up part of it, to see whether the gold has not found its way into cracks scarcely perceptible on the surface. "Dry digging," as a mode of mining, must not be confounded with " dry diggings," a kind of mining-ground which has been de- scribed near the beginning of this chapter. Knife-mining differs a little from dry digging. In the latter, a shovel is used to strip off the barren dirt ; whereas the knife- mining is practised in those places where the gold is deposited in crevices in rocks along the banks of streams, without any covering of barren dirt, so that the knife alone is used in sera- ping out the dirt; and afterward the dirt, being placed in a pan, may be washed in water, which is never used in dry dio-- ging. § 195. Puddling-Box.—The puddhng-box is a rough wood- en box, about a foot deep and six feet square, and is^used for dissolving very tough clay. The clay is thrown into the box, with water, and a miner stirs the stuff with a hoe until the clay is all thoroughly dissolved, when he takes a plug from an auger-hole about four inches from the bottom, and lets the thin solution of the clay run off, while the heavier material, inclu- ding the gold, remains at the bottom. He then puts in the plug again, fills up the box with water, throws in more clay, and repeats the process again and again untU night, when he cleans up with a cradle or pan. The puddhng-box is used only in small mining operations, and never with the sluice, or in hydraulic claims. § 196. QuicJcsilver-Machine,—ThQ quicksilver-machme, or Burke rocker, is a cradle about seven feet long, two feet wide, and two feet high. In the bottom are a number of compart- ments, aU contaming quicksilver. One man rocks the machine without cessation. A constant stream of water pours into the machine at its head. The riddle extends the whole length of the machine ; and the stones, after being washed clean, fall off the riddle at the lower end. One man is employed constantly working with a shovel to keep the dirt on the riddle under the stream of water, and in throwing off the big stones. K the 12 266 RESOURCES OF CALIFORNIA. pay-dirt is very convenient, two men can shovel enough to keep the machine in operation. The Burke rocker was exten- sively used in California eight and ten years ago, but now it is a great rarity. § ]97. Tunnd-Mining. — A tunnel, in Californian mining, is an adit or drift entering a hill-side, or running out from a shaft. IMining-tunnels are usually nearly horizontal — those entering hill-sides having a slight ascent, for the double purpose of draining the mine, and to facilitate the removal of the pay- dirt. In a few hills the tunnels run downward at an angle of twenty degrees or more, to avoid veins or ledges of rock, which would have to be blasted through if the tunnel were cut horizontally ; but this can only be done with safety in hills which are drained by older horizontal tunnels. The mining-tumiel does not run through a hill, but only into it. The length of tunnels varies greatly ; the longest are about a mile. The usual height is seven feet, the width five feet. Ordinarily the top must be supported by timbers, to prevent it from falling in, and not unfrequently the sides must also be protected by boards. The cost of cutting a tunnel varies from two to forty dollars a longitudinal foot, according to the nature of the ground, the cost of getting timbers, &c. Tunnels are usually made by companies of eight or ten men, of whom one- half may be merchants, lawyers, physicians, or ofiice-holders, and the remainder laborino: miners. The latter class do the work ; the former furnish provisions and tools, and a certain amount of cash weekly until the pay-dirt is reached. Two or three men work at a time cutting a tunnel ; one or two to dig the dirt ; and one or two to haul it out. The dirt of the first fifty yards is hauled out in a wheelbarrow ; beyond that dis- tance a little tram-way or railroad is laid down, and the dirt is hauled out in cars, pushed by the miners. It is not customary to use horses. It is common to have tw^o relays of laborers — one set working from noon to midnight, the other from mid- night to noon. Work in a tunnel is as pleasant at night as in the daytime. When a company is rich, or has many laborers, it MINING. 267 may have three relays, each to work eight hours in the twenty- four. It is not uncommon for two companies, owning adjacent claims in a hill, to unite and cut a tunnel on joint account along the dividing line. They go in until they reach the pay-dirt, and then a surveyor is employed to run the line between their claims, and the tunnel is contiimed through the pay-dirt. The dirt from the tunnel is washed for the joint account of the two companies. After the di\dding line has been established, each company keeps on its own side, and each has its time to use the tram-way. They may also have a joint-stock sluice at the mouth of the tunnel — one company having the privilege of using the sluice one week, and the other the next. All tho dirt brought out in a week can readily be washed in a day. The work of taking out the pay-dirt after the main tunnel has been cut, is called " drifting ;" and the holes made by the men engaged in it are termed " drifts." The drifts are usually not so high as the tunnels. The large stones and barren dirt ob- tained in the drifts are piled up here and there to sustain the earth overhead. Sometimes wooden posts are likewise neces- sary. * § 198. Shafts. — Shafts are used in prospecting, and also in mining, where the claims are deep and cannot be reached by either the hydraulic process or the tunnel. The prospecting shaft is sometimes sunk into hills supposed to be auriferous, where the shaft is far less expensive than the tunnel. After the shaft demonstrates that the dirt is rich, and precisely the altitude at which it lies, a tunnel is cut to strike it. The shaft may be the cheaper for prospecting, but the tunnel is usually the cheaper if any large amount of dirt is to be taken out. The shaft is dug by one man in the hole, and one or two are employed at a windlass in hauling up the dirt. Mining-shafts in placer diggings are rarely over one hundred feet deep; but one was dug in Trinity county to the depth of six hundred feet, for the purpose of prospecting, but it found neither pay-dirt nor the bed-rock. 268 RESOUIiCES OF CALIFORNIA. § 199. River-Mining. — River-mining is mining for gold in the beds of rivers, below low-water mark. The only practi- cable method of doing this is by damming the stream, and taking the water out of its bed in a ditch or flume. It has been proposed by persons who never saw the mines, to get the gold by dredging, or with a diving-bell ; but such schemes are absurd in the eyes of miners. The rivers in which the gold is found are mountain-torrents, in which a canoe can scarcely float in suinmer, much less a dredgiug-machine ; and any large scoop working under water would miss the crevices and cor- ners in the rocks, where most of the gold is found. As the water is very seldom more than a couple of feet deep, a diving- bell would be of little service. The flume, the ditch, and the wing-dam, are the chief tasks of the river- miner. The ditch is rarely used, because the banks of the mining-streams are usu- ally so steep, high, rocky, and crooked, that a flume is cheaper. The wing- dam is not often used, because the river-beds are in most places too narrow. The flume is almost universally em- ployed. The work of river-mining can be done only during the sum- mer and fall, while the water is low, and while the miner can have confidence that it will not rise. It may be as low in Jan- uary as in August, but the winter is the season of rains ; and when the flood comes, it sweeps dams, flumes, and every thing before it. If the dam and flume be commenced too earlv in the season, they may be carried off" before they are finished ; and it frequently happens that they are destroyed in the fall just when the miners are commencing to reap the reward of their summer's labor. Kiver-mining has many disadvantages, as compared with other branches of mining. The miner cannot work at it more than half the year; he cannot j^i'ospect the dirt which is hid- den under water ; he must erect expensive dams and flumes, which can be used for only a few months ; and then he is ex- posed to floods which may come and destroy all his work before he has commenced to wash. These disadvantages, and MIXING. 269 the exhaustion of most of the river-diggings in the state, have almost put an end to river-mining in California. In a few cases, extensive fluniing enterprises have proved profitable; but, as a general rule, river-mining in this state has cost more than it has produced. A river is seldom flumed for less than three hundred yards, and sometimes for a mile ; and the lum- ber and labor required to make so long a flume, and one large enough to hold all the water of a river, are very expensive. The dam will alwavs leak, and water will run into the bed from the adjacent hills and mountains, and this water must be lifted out by pumps driven by wheels placed in the flume. The river-beds are full of large rocks, weighing from one to ten tons, and these must be moved by machinery, to allow the dirt to be taken out. River-mining is now never undertaken by an individual, but always by large associations, generally called " fluming com- panies," sometimes composed of miners exclusively, sometimes of miners and all the principal business-men living near the place where the work is to be done. The lawyers, doctors, and ofiice-holders, pay their assessments in cash; the mer- chants furnish provisions, the lumbermen supply lumber, and the miners make the dam, and help the carjDenters build the flume. § 200. Jjeach-Minmg. — Beach-mining is the business of washinor the sands of the ocean-beach. Between Point Men- docino, in California, and the mouth of the Umpqua River, in Oregon, the beach-sand contains gold, and in some places it is very rich. The beach is narrow, and lies at the foot of a bluff* bank of auriferous 'sand. In times of storm, the waves wash against this bank, undermine it, sweep away the pieces which tumble down, leaving the gold on the beach. The gold is in very fine particles, and it moves with the heavier sand, which alters its position frequently under the influence of the waves and surf One day, the beach will have six feet depth of sand ; the next, there will be nothing save bare rocks. The sand diff'ers greatly in richness at various times : one day, it will be 270 RESOURCES OF CALIFOliNIA. full of golden specks ; a few days later, at the same place it ■will be barren. The sand in the mean time has been moved by the waves, and replaced by other sand. It is a very difficult matter to know where the sand is rich and where it is not. The companies employed in mining on the beach number about ten men ; and there is a foreman who rides out early every morning, following the beach about two miles to the northward and two miles to the southward of the camp, for the purpose of finding where the sand is the best. So changeable is the sand, that a new examination is made every day ; and only three or four men are supposed to be good judges of the quaUty of sand, from its appearance. When the foreman has selected a place, he orders all the men to it, and they go with twenty pack-mules, which carry the sand in alforjas^ or rawhide sacks, to the place of washing, which is up on the bluff, probably a mile or more distant from the spot where the sand is obtained. It happens occasionally that the foreman rides long distances on the beach, and some- times he will order the sand to be obtained ten miles from the w^ashing-place. The sand must, of com*se, be very rich, to pay for such transportation, but the beach-sand at times in the sun- light is said to be actually dazzling yellow with gold. The purpose of going upon the bluff to wash it is to get fresh water for washing ; foi the sea-water is not so good, nor can it be obtained conveniently. The richest dirt is that the farthest down on the beach, so still weather and low tide are the best times for getting it. When a rich place is discovered low down on the beach, great exertions are made to get as much of the sand as possible before the tide rises. When high tide and storm come together, little can be done. The sand, hav- ing been separated from all clay and soluble matter by the action of the sea, is very easily washed, and all collected in a month can be washed in two days in a sluice. § 201. Mining-Ditches. — The placer-mines of California would yield very little gold, were it not for the numerous ditches which supply them with water for washhig. The au- MIXING. 271 riferous districts are very dry in summer,