with grauwacke-slate is equally rich in metals in Mexico as in several parts of Germany. In this rock, the formation of which immediately preceded that of the secondary rocks, several of the veins of Zacatecas appear to be found. In proportion as the north of Mexico shall be examined by intelligent geologists, it will be perceived that the metallick wealth of Mexico does not exclusively belong to primitive formations and transition rocks, but extend also to those of secondary formation. I know not whether the lead which is procured in the eastern parts of the intendancy of San Luis Potosi is found in veins or beds; but it appears certain, that the veins of silver of the Real de Catorce, as well as those of the Doctor and Xaschi near Zimapan, traverse alpine limestone (alpenkalkstein); and this rock rests on pudding-stone, with silicious cement, which may be considered as the most antient of secondary formations. The alpine limestone, and the jura limestone (jurakalkstein), contain the celebrated silver mines of Tasco and Tehuilotepec, in the intendancy of Mexico; and it is in these calcareous rocks that the numerous veins which in this country have been very early wrought, display the greatest wealth. They are less productive in the strata of primitive slate (urthon-schiefer), which is as seen in the * Cerro de San Ignacio, serves for base to the The result of this general view of the We observe in the most celebrated mines of Europe, that the mining operations are either directed to a multitude of small veins, as in the primitive mountains of Saxony, or to a very small number of depositories of minerals of an extraordinary power, as at Clausthal, the Harz, and near Schemnitz in Hungary. The cordilleras of Mexico offer frequent examples of these two methods of operation; but the districts of mines of the most constant and considerable wealth, Guanaxuato, Zacatecas, and the Real del Monte, contain only one principal vein each (veta madre). The vein called halsbrükner spath, of which the extent is two metres*, and which has been traced for a length of 6200 metrest, is spoken of as a remarkable phenomenon at Freiberg. The veta madre of Guanaxuato, from which there has been extracted, during the course of the last ten years, more than six millions of marcs of silvert, is of the extent of from 40 to 45 metres §, and it is wrought from Santa Isabella and San Bruno to Buena-Vista, a length of more than 12,700 metres.|| In the Old Continent, the veins of Freiberg and Clausthal, which intersect mountains of gneiss and grauwacke, are visible in table lands of which the elevation above the level of the sea is only from 350 to 570 metres ; and this * 6 feet. Trans. † 20, 341 feet. Trans. § From 131 to 147 feet. Trans. | 41,665 feet. Trans. ¶ From 1148 to 1869 feet. Trans. 1 elevation may be regarded as the mean height of the most abundant mines in Germany. But in the New Continent the metallic wealth is deposited by nature on the very ridge of the cordilleras, and sometimes in situations within a very small distance from the limit of perpetual snow. The most celebrated mines in Mexico are at absolute heights of from 1800 to 3000 metres. * In the Andes, the districts of mines of Potosi, Oruro, Paz, Pasco and Gualgayoc, are in regions of which the elevation surpasses that of the highest summits of the Pyrenees. Near the small town of Micuipampa, the great square of which, according to my measurement, is 3618 metres † above the level of the sea, a depôt of silver ore known by the name of Cerro de Gualgayoc was found to yield immense wealth at an absolute height of 4100 metres. ‡ We have mentioned in another place § the advantage which in working the Mexican mines, is derived from the most important veins being in a middle region, where the climate is not unfavourable to agriculture and vegetation. The large town of Guanaxuato is placed in a ravin, the bottom of which is somewhat * From 5904 to 9842 feet. Trans. † 11,868 feet. Trans. 13,451 feet. Trans. § See vol. i. p..71., and vol. ii. p. 407. CHAP, XI.] KINGDOM OF NEW SPAIN. 137 lower than the level of the lakes of the valley of Tenochtitlan. We are ignorant of the absolute heights of Zacatecas and the Real de Catorce; but these two places are situated on table lands seemingly more elevated than the level of Guanaxuato. However, the temperate climate of these Mexican towns, which are surrounded with the richest mines in the world, is a contrast to the cold and exceedingly disagreeable climate of Micuipampa, Pasco, Huancavelica and other Peruvian towns. When in a district of small extent, for instance, in that of Freiberg in Saxony, we compare the quantity of silver annually coined, with the great number of mines constantly worked, we perceive, on the slightest examination, that this produce is derived from a very small part of the mining operations, and that nine tenths of the mines possess almost no influence on the total mass of ores extracted from the bowels of the earth. In the same manner, in Mexico, the 2,500,000 marcs of silver which are annually sent to Europe and Asia, from the ports of Vera Cruz and Acapulco, are the produce of a very small number of mines. The three districts which we have frequently had occasion to name, Guanaxuato, Zacatecas, and Catorce, supply more than the half of that sum. * 1,640,791 lb. troy. Trans. |