History of the State of California

"The coast has not been surveyed, nor has its outline been correctly ascertained. There are many rocks above and below the water-line, and small islands not mentioned or indicated on any chart, which render navigation near the land, especially at night, extremely dangerous.

"An accurate survey of the coast, to commence at the most important points, the construction of lighthouses, and the placing of buoys in proper positions, are objects of much importance, and, it is not doubted, will attract the early attention of Government."

We come now to that which has built up so rapidly this empire of the Pacific – the metallic and mineral wealth of California. As to the extent of the region, and indications of the existence of the gold, together with the attendant geological formations, the statements of Mr. King's report will not be, nor have not been, gainsayed; but as to the origin of the gold, whether in combination with quartz, or mixed with the sands of the ravines and streams, various opinions have been expressed by those who have spent considerable time in working and observing the different formations. That due weight may be given to both of the principal theories, we extract the observation and opinion of a person who favors the idea of the gold having been scattered over the country, by a tremendous volcanic eruption.

"The gold found in every placer in California bears the most indubitable marks of having, at some time, been in a molten state. In many parts it is closely intermixed with quartz, into which it has evidently been injected while in a state of fusion; and I have myself seen many pieces of gold completely coated with a black cement that resembled the lava of a volcano. The variety of form, which the placer gold of California has assumed, is in itself sufficient evidence of the fact, that it has been thrown over the surface while in a melted state. The earliest comparisons of the California gold were to pieces of molten lead dropped into water. The whole territory of the gold region bears the plainest and most distinct marks of being volcanic. The soil is of a red, brick color, in many places entirely barren, and covered with a flinty rock, or pebble, entirely parched in the summer, and during the rainy season becoming a perfect mire. The formation of the hills, the succession of gorges, the entire absence of fertility in many portions, distinctly exhibit the result of a great up-heaving during past times. But there is one phenomenon in the mining region which defies all geological research founded upon any other premises than volcanic formation. Throughout the whole territory, so generally that it has become an indication of the presence of gold, a white slate rock is found, and is the principal kind of rock in the mining region. This rock, instead of lying as slate rock does in other portions of the earth, in horizontal strata, is perpendicular, or nearly so; seeming to have been torn up from its very bed and left in this position. On the banks of the Middle Fork are several excavations, which can only be accounted for upon the supposition, that they were at some time volcanic craters. There is one of these on the mountain side, about five miles below the "Big Bar;" from which, running down to the base of the mountains, is a wide gorge entirely destitute of verdure, while the earth around it is covered with shrubbery. This, I am fully convinced, was the bed of the lava stream that was thrown up from the crater; and in searching for gold at the very foot of it, I found several pieces entirely covered with the black cement or lava, of which I have previously spoken. From all these evidences, I am fully satisfied that at some early date in the world's history, by some tremendous volcanic eruption, or by a succession of them, gold, which was existing in the form of ore, mixed with quartz rock, was fused and separated from its surrounding substances, and scattered through every plain, hill, and valley, over an immense territory. By its own gravity, and the continual washing of the rains, it sank into the earth until it reached a rock, or hard, impenetrable clay. It still continued washing and sliding down the hill-side, until it reached the rivers or ravines, and in the former was washed along with its current until it settled in some secure place in their beds, or was deposited upon their banks; and in the latter rested among the crevices of rocks."¹³

The following from Mr. King's report, presents the opposite theory, with its evidence in full. The two accounts are at variance both in regard to fact and theory. But that of Mr. King, who enjoyed every facility of obtaining information from observation, and from the statements of intelligent miners, is considered most reliable, in respect to matters of fact, and, therefore, of more dependence in forming a theory. He says —

"The principal formation, or substratum, in these hills, is talcose slate; the superstratum, sometimes penetrating to a great depth, is quartz. This, however, does not cover the entire face of the country, but extends in large bodies in various directions – is found in masses and small fragments on the surface, and seen along the ravines and in the mountains, overhanging the rivers, and in the hill-sides in its original beds. It crops out in the valleys and on the tops of the hills, and forms a striking feature of the entire country over which it extends. From innumerable evidences and indications, it has come to be the universally admitted opinion, among the miners and intelligent men who have examined this region, that the gold, whether in detached particles and pieces, or in veins, was created in combination with the quartz. Gold is not found on the surface of the country presenting the appearance of having been thrown up and scattered in all directions by volcanic action. It is only found in particular localities, and attended by peculiar circumstances and indications. It is found in the bars and shoals of the rivers; in ravines, and in what are called the 'dry diggings.'

"The rivers, in forming their channels, or breaking their way through the hills, have come in contact with the quartz containing the gold veins, and by constant attrition cut the gold into fine flakes and dust, and it is found among the sand and gravel of their beds at those places where the swiftness of the current reduces it, in the dry season, to the narrowest possible limits, and where a wide margin is, consequently, left on each side, over which the water rushes, during the wet season, with great force.

"As the velocity of some streams is greater than that of others, so is the gold found in fine or coarse particles, apparently corresponding to the degree of attrition to which it has been exposed. The water from the hills and upper valleys, in finding its way to the river, has cut deep ravines, and, wherever it has come in contact with the quartz, has dissolved or crumbled it in pieces.

"In the dry season, these channels are mostly without water, and gold is found in the beds and margins of many of them in large quantities, but in a much coarser state than in the rivers; owing, undoubtedly, to the moderate flow and temporary continuance of the current, which has reduced it to smooth shapes, not unlike pebbles, but has not had sufficient force to cut it into flakes or dust.

"The dry diggings are places where quartz containing gold has cropped out, and been disintegrated, crumbled to fragments, pebbles, and dust, by the action of water and the atmosphere. The gold has been left as it was made, in all imaginable shapes; in pieces of all sizes, from one grain to several pounds in weight. The evidences that it was created in combination with quartz are too numerous and striking to admit of doubt or cavil. They are found in combination in large quantities.

"A very large proportion of the pieces of gold found in these situations have more or less quartz adhering to them. In many specimens, they are so combined they cannot be separated without reducing the whole mass to powder, and subjecting it to the action of quicksilver.

"This gold, not having been exposed to the attrition of a strong current of water, retains, in a great degree, its original conformation.

"These diggings, in some places, spread over valleys of considerable extent, which have the appearance of an alluvion, formed by washings from the adjoining hills, of decomposed quartz and slate earth, and vegetable matter.

"In addition to these facts, it is, beyond doubt, true that several vein-mines have been discovered in the quartz, from which numerous specimens have been taken, showing the minute connection between the gold and the rock, and indicating a value hitherto unknown in gold-mining.

"These veins do not present the appearance of places where gold may have been lodged by some violent eruption. It is combined with the quartz, in all imaginable forms and degrees of richness.

"The rivers present very striking, and, it would seem, conclusive evidence respecting the quantity of gold remaining undiscovered in the quartz veins. It is not probable that the gold in the dry diggings, and that in the rivers – the former in lumps, the latter in dust – was created by different processes. That which is found in the rivers has undoubtedly been cut or worn from the veins in the rock, with which their currents have come in contact. All of them appear to be equally rich. This is shown by the fact that a laboring man may collect nearly as much in one river as he can in another. They intersect and cut through the gold region, running from east to west at irregular distances of fifteen to twenty, and perhaps some of them thirty, miles apart.

"Hence it appears that the gold veins are equally rich in all parts of that most remarkable section of country. Were it wanting, there are further proofs of this in the ravines and dry diggings, which uniformly confirm what nature so plainly shows in the rivers."

It is an interesting inquiry – what was the amount of the golden treasure collected during the years 1848 and '49? The satisfaction of this inquiry will enable us to form some faint conception of the value of the gold region, and the dependence which may be placed upon its yield for a commercial return. Premising that the gold was first discovered in May, 1848, and that intelligence of it was not received in the United States till late in the following autumn, Mr. King, in his report, proceeds in making an estimate of the quantity accumulated till the close of 1849:

"No immigration into the mines could, therefore, have taken place from the old States in that year. The number of miners was, consequently, limited to the population of the territory, some five hundred men from Oregon – Mexicans, and other foreigners, who happened to be in the country, or came into it during the summer and autumn – and the Indians, who were employed by or sold their gold to the whites.

"It is supposed there were not far from five thousand men employed in collecting gold during that season. If we suppose they obtained an average of one thousand dollars each – which is regarded by well informed persons as a low estimate – the aggregate amount will be $5,000,000.

"Information of this discovery spread in all directions during the following winter; and, on the commencement of the dry season in 1849, people came into the territory from all quarters – from Chili, Peru, and other States on the Pacific coast of South America; from the west coast of Mexico, the Sandwich Islands, China, and New Holland.

"The immigration from the United States came in last, if we except those who crossed the Isthmus of Panama, and went up the coast in steamers, and a few who sailed early on the voyage round Cape Horn.

"The American immigration did not come in by sea, in much force, until July and August, and that overland did not begin to arrive until the last of August and first of September. The Chilenos and Mexicans were early in the country. In the month of July, it was supposed there were fifteen thousand foreigners in the mines. At a place called Sonoranian Camp, it was believed there were at least ten thousand Mexicans. They had quite a city of tents, booths, and log-cabins; hotels, restaurants, stores, and shops of all descriptions, furnished whatever money could procure. Ice was brought from the Sierra, and ice creams added to numerous other luxuries. An inclosure made of the trunks and branches of trees, and lined with cotton cloth, served as a sort of amphitheatre for bull-fights. Other amusements, characteristic of the Mexicans, were to be seen in all directions.

"The foreigners resorted principally to the southern mines, which gave them a great superiority in numerical force over the Americans, and enabled them to take possession of some of the richest in that part of the country. In the early part of the season, the Americans were mostly employed on the forks of the American, and on Bear, Uba, and Feather Rivers. As their numbers increased, they spread themselves over the southern mines, and collisions were threatened between them and the foreigners. The latter, however, for some cause, either fear, or having satisfied their cupidity, or both, began to leave the mines late in August, and by the end of September many of them were out of the country.

"It is not probable that, during the first part of the season, there were more than five or six thousand Americans in the mines. This would swell the whole number, including foreigners, to about twenty thousand the beginning of September. This period embraced about half the season, during which gold may be successfully collected in the rivers.

"Very particular and extensive inquiries respecting the daily earnings and acquisitions of the miners lead to the opinion that they averaged an ounce per day. This is believed by many to be a low estimate; but, from the best information I was able to procure, I am of opinion it approaches very near actual results. The half of the season, up to the 1st of September, would give sixty-five working days, and to each laborer, at $16 per ounce, $1,040. If, therefore we assume $1,000 as the average collected by each laborer, we shall probably not go beyond the mark.

"This would give an aggregate of $20,000,000 for the first half of the season – $15,000,000 of which was probably collected by foreigners. During the last half of the season, the number of foreigners was very much diminished, and, perhaps, did not exceed five thousand. At this time, the American immigration had come in by land and sea, and the number of our fellow-citizens in the mines had, as was estimated, increased to between forty and fifty thousand. They were most of them inexperienced in mining, and it is probable the results of their labors were not so great as has been estimated for the first part of the season, and experienced miners. Assuming that the average of half an ounce per day ought to be considered as reasonable, it would give an aggregate of about $20,000,000. If from this we deduct one-fourth on account of the early commencement of the wet season, we have an estimate of $15,000,000; at least five of which was collected by foreigners, who possessed many advantages from their experience in mining and knowledge of the country.

"These estimates give, as the result of the operations in the mines for 1848 and 1849, the round sum of $40,000,000; one-half of which was probably collected and carried out of the country by foreigners.

"From the best information I could obtain, I am led to believe that at least $20,000,000 of the $40,000,000 were taken from the rivers, and that their richness has not been sensibly diminished, except in a few locations, which had early attracted large bodies of miners. This amount has principally been taken from the northern rivers, or those which empty into the Sacramento; the southern rivers, or those which flow into the San Joaquin, having been, comparatively, but little resorted to until near the close of the last season. These rivers are, however, believed by those who have visited them, to be richer in the precious metal than those in the northern part of the gold region."

Adopting the hypothesis that the gold found in these streams had been cut or worn away from the veins in the quartz through which they have forced their way, and considering the fact that they are all equally productive, we may conjecture what a vast amount of treasure remains undisturbed in the veins which run through the masses of rock over a space of forty or fifty miles wide, and near five hundred miles long. Such an estimate would almost defy our belief; yet, if the hypothesis is true, there is no reason to doubt that the value of the gold which that region will yield, is almost beyond calculation.

The quicksilver mines of California are believed to be numerous, extensive, and very valuable. The largest and most profitable one yet opened is situated near San José, and belongs to, or is claimed by, Mr. Forbes, of Tepic, in Mexico. The cinnabar ore, which produces the quicksilver, is easily procured, and machinery has been put in operation, which enables the proprietor to make an extensive profit. The value of the quicksilver mines, by being so near the gold region, is considerably increased; quicksilver being almost indispensable in gold mining.

Extensive beds of silver, iron, and copper ores are believed to exist in the territory, but their existence and value is not accurately ascertained, the allurements held out by the continued success of the gold-miners and the continued discovery of new and profitable placers being too strong to permit any search for the baser, but more useful metals. Respecting the propriety of the establishment of a mint in California, Mr. King makes the following observations —

"I have already alluded to the propriety of establishing a mint in California. This is important in many respects. At this time, there is not coin in the country to supply a currency. Much difficulty is experienced in procuring enough to pay the duties on imported goods. The common circulating medium is, therefore, gold dust, which is sold at $15 50 to $16 per ounce. In the mines, it is frequently sold much lower. The miners, the laboring men, are the sufferers from this state of things.

"Those who purchase and ship gold to the Atlantic States make large profits: but those who dig lose what others make.

"I have estimated that there will be $50,000,000 collected during the current year. At $16 per ounce, that sum will weigh 3,125,000 ounces.

"Gold, at the United States mint, is worth $18 per ounce, making a difference in value on that quantity, between San Francisco and New York, of $6,250,000, which would be saved to the miners by the establishment of a mint.

"I have also suggested its importance as a means of promoting and increasing our trade with the west coast of Mexico and South America.

"It is not doubted that the construction of a railway across the Isthmus of Panama, and, perhaps, the establishment of other lines of communication between the two oceans, will give to the products and manufactures of the older States of the Union command of the market of California to the exclusion, in a great degree, of those of the west coast.

"A mint will, therefore, become of the utmost importance, to give such marketable value to silver bullion as to enable the merchants of those countries to keep up and increase the intercourse with our principal ports on the Pacific.

"The silver bullion shipped to Europe from the west coast of Mexico amounts to more than ten millions of dollars per annum. From the countries on the west coast of South America, probably an equal quantity. That from Mexico goes to pay for European importations into her ports on the Atlantic side.

"A market at San Francisco for this bullion will be the means of substituting American and Chinese fabrics for those of European manufacture in all those countries. This will greatly increase the trade between China and California."

A bill for the establishment of a mint at San Francisco was introduced into Congress, during the present session, (1849-50) and passed both houses; thus securing to California the advantages mentioned in the above extract, by Mr. King.

We have thus given a complete description of California, in respect to population, climate, soil, productions, commercial resources, and metallic and mineral wealth, as accurate and comprehensive as the most authentic sources could furnish, or as could be ascertained at the present time. Although the territory already contains a large population and has produced a great amount of treasure in the short duration of its existence; although it is already a large State, which has sprung into existence, as it may be termed, there is every evidence that this is but the "beginning of the end." "The greatest is behind." To what such commercial facilities, mineral and metallic resources, and an active and progressive population will conduct California, it is easy to imagine. They will build up a State, which, although the member of a confederacy, will be powerful enough to maintain itself, independent of the aid to be derived from the Union. Its ports will be the resort of the vessels of all nations, and its valleys and hill-sides will become the homes of an agricultural population, reaping the rich reward of their toil. Canals and railroads, the children of enterprise, will soon intersect the territory, transport the riches of one section to another, and increase the social communication of the inhabitants. Such a State will add greatly to the power of the confederated republic, and form an additional stimulus to the rapid filling up of the vast territory situated between California and her sister States.