ANTIQUITIES IN THE MUSEUM—STATUE OF CHARLES IV.—CONDITION OF THE MUSEUM—FEATHERED SERPENTS—VICEROY'S PORTRAITS—CORTÉZ—PORTRAIT—ARMOR—PEDRO DE ALVARADO—IMAGES—VASES—TEZCOCO—PALACE—TROUGH—MASSIVE MOUNDS—TESCOCINGO—HILL—ITS ANCIENT ADORNMENTS—ANCIENT BELLEVUE AND RESERVOIR—TEZCOCAN SPLENDOR—BOSQUE DEL CONTADOR—PONDS—LAKES—ARBORS—PYRAMIDS OF TEOTIHUACAN—HOUSES OF SUN AND MOON—PATH OF THE DEAD—CARVED PILLAR—PILLAR AT OTUMBA—PYRAMID OF XOCHICALCO—HILL OF XOCHICALCO—ITS STRUCTURES.
THE largest collection of the moveable antiquities of Mexico, belonging to the Aztec and probably to the Toltec period of the occupation of the valley or adjacent country, is found in the Museum which occupies two or three rooms and part of the court yard of the University building. In the centre of the quadrangle around which this edifice is erected is the fine bronze statue of Charles IV., cast in the capital by a native Mexican. It is an admirable work, and before the revolution stood in front of the cathedral in the plaza or great square. The Spanish sovereign is habited in an antique Roman dress, and is seated on horseback. His right hand, holding a baton, is stretched forward, in an attitude of command and the folds of a massive robe fall gracefully from his neck, over the hind limbs of his horse. His brow is bound with a laurel wreath, and a Roman blade rests on his thigh, whilst the animal is represented in the act of advancing slowly and treading on a quiver of arrows.
This statue is, of course, liable to some just criticism, founded on the bad models for horses which the artist had recourse to in Mexico whilst engaged in his task; and although a due degree of strict adherence to historical portraiture did not permit him to exalt too much the personal characteristics of the king, he has nevertheless contrived to infuse a great deal of power into the statue so as to entitle it to a fair comparison with some of the best European equestrian works in bronze. All the minor parts of the figures and their decorations are finished with the utmost neatness, and another
proof is given, in this statue of the genius possessed by the natives for the imitative arts. It was the work of Tolsa, and was first opened to public view on its pedestal in the plaza, in the year 1803, under the viceroyal government of Iturrigaray.
In a corner of this court yard, on the left of the portal, amid a quantity of ancient lumber and relics, are the sacrificial stone and the gigantic idol statue of Teoyaomiqui, described in the first volume of this work. Here, too, are the huge serpent images, carved from basalt, which are presumed to have been used in the worship of Quetzalcoatl—the "feathered serpent,"—the "god of the air."
After an examination of the massive relics which lie in the court yard of the University, we ascend by a broad stone staircase to the corridor surrounding the quadrangle on the second floor. The lower story of this edifice is occupied by the college chapel and the hall or recitation room, whose lofty ceiling and windows, gloomy walls, and carved oaken seats and pulpit, remind the stranger of the fine old monastic chambers in similar institutions in Europe.
The apartments of the second floor open upon the broad corridor under a light and tasteful arcade, and several rooms on the northern side are devoted to the national collections, which, at the period of our visit to Mexico in 1841 and 1842 were badly arranged and classified. The salary devoted to the curator was scarcely adequate to support him, and he probably paid more attention to the politics of the present day than to the antiquities of the past. Nevertheless, we found him to be an intelligent gentleman, fond of the relics, images and legends of the Aztecs. He would, doubtless, have organized the valuable collection had he been suitably aided, recompensed, or enabled to devote the whole of his time to the archaiology of his country.
The first apartment on this side of the building is a sort of Spanish lumber room, the wall of which is friezed with a series of the viceroys, whilst, in a corner, stand the fragments of a throne, waiting, perhaps, the order for their reconstruction upon the ruins of the presidential chair. Hard by this royal relic, in appropriate contrast, is an unfinished bas relief of a trophy of liberty; and above the sculpture, suspended against the wall in a rough pine coffin, hangs an Indian mummy, which was exhumed in the fields of Tlaltelolco north of the capital. Another side of this saloon is occupied by full length portraits of Ferdinand and Isabella. In the next chamber, west of this, the mass of the smaller Aztec relics has been collected and preserved in cases. A small library, containing some ancient manuscripts, and the splendid work of Lord
Kingsborough on Mexican antiquities, are preserved in this apartment, while on the surrounding shelves, are deposited specimens of the pottery, vases, pipes, idols, images, bows, arrows, axes, masks, sacrificial instruments, beads and altars of the Aztecs.
Around the frieze of this room, as around that of the preceding, are portraits of Mexican viceroys, at the head of which is the picture of the conqueror Hernando Cortéz, from which the engraving in these volumes has been accurately copied. Its authenticity is unquestionable, for its history has been carefully traced to the period of the third viceroy, Don Gaston de Peralta, Marques de Falces. This portrait represents the hero of the conquest differently from any other picture we have found either engraved or in oil, and exhibits the mingled air of elevated veneration and command, of firmness and dignity, reflection and resolute action, which are the chief historical characteristics of this personage. In a corner, beneath the portrait, is a plain, unornamented suit of steel armor, which belonged to the hero. Its small dimensions convey no favorable impression of the hero's size or strength. The armor, and patent of nobility granted by Charles V. to Pedro de Alvarado, the companion of Cortéz, are also preserved in this saloon. The royal document is exceedingly interesting from the fact that it contains the autographs of the emperor and of Cortéz, who signed it as El Marques del Valle de Oajaca.[61] Near these relics of two of the leaders of the conquering army, preserved religiously under glass in a golden frame, is the crimson silken banner, bearing the image of the Virgin, crowned with a golden coronet and surrounded with twelve stars, under which that army is alleged by the antiquarians to have marched the second time against the Aztec capital.
In the apartment west of this, and facing on the plaza del Volador, are the collections in natural history, which have been chosen apparently, rather as curiosities than for scientific purposes. The specimens of birds, beasts and reptiles, are indifferently preserved and classified, and even the collection of minerals, which, in Mexico, ought to be of the most perfect character, scarcely deserves mention as an important illustrative cabinet.
The number of small images, which are usually called idols, contained in the cases of the principal saloon is very large, and specimens are presented from most parts of the territory comprised in the empire of the Aztec sovereigns, as well as from Mechoacan. Some of the finest of these, both large and small, are exhibited in the plates annexed to this section; and we do not describe them minutely or singly, because they depend for their interest upon their forms, which are better depicted in drawings than language. Most of these were carefully delineated and measured by the author of this work himself, and their accuracy may be confidently relied on.
Two of the most beautiful and rare objects comprised in this collection, are the terra-catta funeral vases, one of which is represented in the accompanying engraving. It was exhumed some years ago in the northern suburb of the capital, known as St. Juan Tlaltelolco, the neighborhood of the ancient site of one of the Aztec teocallis. It is one foot ten inches high, and one foot three and a half inches in diameter. Its upper portion was filled with human skulls, and the lower with bones of the rest of the frame, while the top was carefully covered with the circular lid, which is given in the plate. The Indian head, winged and crowned with a circlet of twisted bands and feathers, the graceful handles, and the semicircle of sunflowers and ears of corn, which curves beneath the central ornament, will give the reader an accurate idea of the reliefs with which this vase is adorned. Besides these symbols of eternity, fruition and fullness, the vessel still exhibits the brilliant colors of blue, vermillion, lake, yellow and brown, with which it was originally tinted.
Some beautiful specimens of the ancient musical instruments of the Aztecs, are also preserved in this museum, and correct drawings of their flageolets, whistles, drums and rattles, will be found in the engravings.
We turn naturally from the ancient capital of the Aztec empire to the remains of art and architecture which are yet found on the site of Tezcoco, the second city in the realm, and in its vicinity. It was in this place that Cortéz prepared for his second assault upon the city of Tenochtitlan or Mexico, and here he put together and launched on the lake the vessels which he had caused to be fashioned in Tlascala on the other side of the mountains that bound the eastern edge of the valley of Mexico. The spot where these vehicles of his troops across the waters of Tezcoco were first deposited in their proper element is still pointed out by the inhabitants, and is known as El Puente de las Brigantinas, though it is now more than a mile from the shore of the lake.[62]
In the north-west section of the modern town of Tezcoco, on the top of a shapeless mass of pottery, bricks, mortar and earth, which is thickly overgrown with aloes, there are several large slabs of basaltic rock, neatly squared and laid due north and south. According to the legends of the spot this is the site of one of the royal residences, and like most of the antiquities of Mexico, is connected with the name of the best known emperor, as the palace of Montezuma. When Mr. Poinsett visited Tezcoco in 1825, this heap had not been pillaged for modern architectural purposes, as much as it has been since that period. Among the ruins of the supposed palace he then found, a regularly arched and well built passage, sewer, or aqueduct, which was formed of square stones the size of bricks, cemented with the strong mortar which was so much used by the Indians in all their works. In the door of one of the rooms he noticed the remains of a "very flat arch," the stones comprising which were of prodigious size and weight. On this spot, some years ago, was found the sculptured basin, which, at the period of our visit, had been transferred to and preserved in the collection of the Ex-Condé del Peñasco in the city of Mexico.
In the southern part of Tezcoco, are the massive remains of three vast pyramids, whose forms are still remarkably perfect. They succeed each other in a direct line from north to south, and, according to our measurement, are about four hundred feet in extent, on each of their fronts, along the base line. They are built partly of burned and partly of sun dried bricks, mixed up with fragments of pottery and thick coverings of cement, through which neat canals had been moulded to carry off the water from the upper terrace. Bernal Diaz del Castillo informs us, that the chief teocalli of Tezcoco was ascended by one hundred and seventeen steps; and, from the quantity of obsidian fragments, images, vessels and heads of idols we found upon the sides of these structures, it is not unlikely, that they, like the teocallis of the capital were devoted to the same bloody and impious rites. In some of the private houses of this town, many larger idols or images cut from basalt are still preserved, and in 1825, Mr. Poinsett saw at the residence of the commandant several of these figures, which were better formed and designed than most of the Indian statues he had previously encountered in his Mexican travels.
About three miles across the gently sloping levels which spread out east of the town of Tezcoco, a sharp, precipitous conical mountain rises abruptly from the plain, which is stripped of the forests that once probably clothed its sides, and is now only covered with a thick growth of nopals, bushes and aloes. From the quantity of Indian remains found on this elevation and in its vicinity, there is no doubt that it was the site of an Aztec palace, or was connected with the adjacent plain by some architectural works that have been destroyed in the centuries that have elapsed since the conquest. The traveller climbs this steep mountain with great labor, and finds nearly every part of it covered with the débris of ancient pottery and obsidian; and, in many parts of his ascent, he is aided by the remains of the spiral road, cut in the solid rock, which evidently once wound from its base to its top. Fifty feet below the summit, looking exactly north, the massive stone of the mountain has been cut into seats surrounding a recess leading to a steep wall which is said to have been covered with a Toltec or Aztec calendar. The sculptures upon the rock have, however, been destroyed by the Indians, who cut through it as soon as they found the spot an object of interest to strangers. These simple and superstitious beings imagined that the quest of gold, alone, could induce travellers to leave the capital, cross the lake, and toil up to the summit of this elevation, and, accordingly they bored through the carved rock to obtain the buried treasure, until they have formed a hole in the mountain, which is now the hiding place and probably the home of a large number of squalid wretches. On the absolute top of the mountain no traces of an edifice are now observable; but as the Spaniards supposed it had been desecrated by Indian rites in the olden time, it has been sanctified by the erection of a cross, from whose feet the whole valley of Mexico, with its lakes, plains, towns and majestic panorama of encircling mountains, bursts on the sight of the wearied traveller.
Returning to the recess from the summit, and winding thence by a spiral path down the eastern slopes of the hill, we find the road suddenly ended by a wall which plunges precipitously down the mountain for about two hundred feet. At this termination of the pathway, cut in the solid rock, we found another recess, surrounded with seats, while, in the centre of the area, was a circular basin, a yard and a half in diameter, and three feet deep, into which water was formerly introduced, through the small aperture in the square pipe which is delineated in the engraving.
This basin has, of course, been also connected with the fame of the emperor, and is known as "Montezuma's bath." Its true use, however, is perfectly evident to those who are less fanciful or antiquarian than the generality of visiters. The picturesque view from this spot, over a small plain set in a frame of the surrounding mountains and glens which border the eastern side of Tescocingo, undoubtedly made this recess a favorite resort for the royal personages at whose expense these costly works were made. From the surrounding seats, they enjoyed a delicious prospect over the lovely but secluded scenery, while, in the basin, at their feet, were gathered the waters of a neighboring spring, which, whilst refreshing them after their promenade on the mountain, gurgled out of its stony channel and fell in a mimic cascade over the precipitous cliff that terminated their path. It was to this shady spot that they no doubt retired in the afternoon, when the sun was hot on the west of the mountain, and here the sovereign and his court, in all probability, enjoyed the repose and privacy which were denied them amid the bustle of the city. Antiquarianism would be greatly assisted in its researches and conjectures, if it recollected that the nature of civilized men is the same in all ages, and that it is easier to judge the architectural remains of our ancestors by this standard than by the fanciful or classical rules, which they are dramatically disposed to conjure up in order to interpret the past.
The hill or mountain of Tescocingo is connected with another hill on the east by a tall embankment about two hundred feet high, upon whose level top,—which may be crossed by three persons abreast, on horseback,—are the remains of an ancient aqueduct, built of baked clay, the pipes of which are now as perfect as on the day they were first laid. The water was brought hither by a canal around the hill to which it is connected by the embankment; while, east of this, and uniting the last hill with another elevation, there is a second aqueduct raised on an embankment, which was fed by other aqueducts and canals that formerly conducted the water from the eastern mountains about three leagues distant.
Such are some of the remains of Tezcocan sumptuousness, in the neighborhood of the ancient capital of this region; and, together with the ancient grove of cypresses, known as El Bosque del Contador, lying across the levels north-west of Tezcoco, may be regarded as the most remarkable relics of the princes and people of the Tezcocan monarchy. The grove of the Contador is formed by double rows of gigantic cypresses, about five hundred in number, arranged in a square corresponding with the points of the compass and enclosing an area of nearly ten acres. At the north-western point of this quadrangle another double row of lordly cypresses runs westwardly towards a dyke, north of which there is a deep oblong
tank, neatly walled and filled with water. From the soft spongy character of the soil in the centre of the great quadrangular grove—which it is impossible for any one to cross without danger of being mired in the unsubstantial morass,—it is supposed that the vast area was once occupied by a lake, whose waters were probably forever renewed by the hydraulic works we have already described in the neighborhood of Tescocingo. Along the raised banks, and beneath the shadows of the double line of majestic trees, were the walks and arbors in which Nezahualcoyotl and his courtiers amused themselves. The ponds and lakes were filled with fish and frequented by the wild fowl that now cover the margins of the Mexican lakes; while the same benignant sky and delicious climate that bless the descendants of the Spaniards, reigned then, as now, over the dusky children of the soil.[63]
A ride on horseback of about three hours at a pleasant pace, will bring the traveller from Tezcoco to the village of St. Juan, lying in an extensive level bordered on all sides by ridges and mountain spurs, except towards the east, where a depression in the chain leads into the plains of Otumba, upon which Cortéz fought so remarkable a battle when pursued by the victorious Aztecs. In the centre of the levels of St. Juan are the two remarkable pyramids of Teotihuacan,—the Tonatiuh-Ytzagual, or "house of the sun," and the Meztli-Ytzagual, or "house of the moon." These vast masses first break upon the sight as the ridge is crossed. At that distance the foliage and bushes that cover them are not easily discerned, and the perfect figure of the original structure seems to be revealed in all its freshness. As the objects are approached, however, the work of time upon the monuments becomes evident. The sharp pyramidal lines are all broken. Aloes, nopals, magueys, mesquite and parasites crawl and cling over every part of the ruined heaps; and the whole mass resembles a crumbling but gigantic pile of rocks and earth, which is scarcely distinguishable from the adjacent hills until its structure is closely examined.
Ascending the one hundred and twenty-one feet of the house of the Sun, we reach a level platform on the summit, whence a charming prospect extends for many miles to the south and east over cultivated fields. At the southern base of this pyramid, which measures six hundred and eighty-two feet, there are four small mounds, and beyond these there is a range of lesser tumuli running towards an elevated square of mounds lying between the stream west of Teotihuacan and the present road to Otumba. On the west front, five tumuli surround an oval mound whose centre is depressed, and all of these jut out westwardly towards a line of similar grave-like elevations lying on both sides of the avenue that leads to the house of the Moon. This road is the Micoatl, or path of the dead, which the ancient writers locate in the valley of San Juan.
The other pyramid, or house of the Moon is smaller, and like its neighbor is composed of rock, stones, pottery and cement,—covered with the debris of obsidian and terra-catta images which lie scattered from the top to the base amid the tangled aloes and creepers that have struck their roots deeply into the crevices. The house of the Sun is not known to have any cavity within its body, but in the house of the Moon, between the second and third terraces, a narrow passage has been detected, through which two wells or sunken chambers, about fifteen feet deep, may be reached by crawling on hands and knees over an inclined plain for a distance of about eight yards. The walls of this cryptic entrance, and of the sunken chamber are made of the common sun dried bricks, but there are no remains of sculpture, painting, or bodies to reward an antiquarian for groping through the dark and dusty aperture.
South of this pyramid of the Moon, is the Micoatl or path of the dead, to which we have already alluded. Two elliptical elevations rise at the south-east and south-west corner of the Teocalli, upon each of which there are three mounds, whilst their diameters are bisected by other rectilinear elevations upon each of which there are five similar mounds. Four circular and one square mound lie within the area of this inclosure, and the whole appears to form a massive portal of tumuli to the majestic pyramid. A long double line of minor mounds stretches away to the south on the sides of the avenue, until all traces of them are lost in the field in front of the temple of the sun with whose groups of tumuli this path was in all likelihood formerly united. The student will obtain a better idea of the localities of these remains by examining the plan which was carefully prepared by the author, on the spot, in 1842. At B, on the plan, there is a large globular mass of granite measuring nineteen feet eight inches in circumference, upon which there is some rude carving which has been found to bear some resemblance to the Aztec figure of the sun;—and in the semicircular enclosure among the tumuli, at C, is placed the sculptured granite stone, represented in the annexed cut. It lies due east and west. The dark shadow at B, represents a sink or hollow three inches deep at the sides, and six at the top and bottom. This is known as the "fainting stone," as it is alleged that all who recline on its surface are sure to experience lassitude, or loose animation for a while!
This place is famous in the ancient history of Mexico, but no remains of importance have been found in its vicinity or within the limits of the village. When Mr. Poinsett visited it during his residence in Mexico as Envoy from the United States, he observed no relic of the past worthy of examination or record except the fragment of a pillar represented in the annexed drawing.
About eighteen miles south of Cuernavaca, in the State of Mexico, there is a cerro or hill, known as Xochicalco or the "hill of flowers," whose summit is occupied by the remains of an ancient stone pyramid. The traveller reaches this eminence after travelling over a wide plain intersected by deep barrancas, and almost entirely denuded of trees and shrubbery. The base of this hill is surrounded by the remains of a deep wide ditch, and its top is attained by five spiral terraces, supported by walls of stone joined with cement. At suitable distances from each other, along the edge of this winding path are the remains of bulwarks fashioned like the bastions of a fortification. On the summit there is a wide extensive level, the eastern part of which is occupied by three truncated cones, resembling the smaller mounds found among the pyramids of Teotihuacan. On the other three sides of the esplenade there are other masses of stones, which may have also been portions of similar tumuli. The stones of which these lesser mounds were constructed have evidently been nicely shaped and covered with a coat of stucco.
Passing upward, amid tangled trees and vines, along the last terrace, and through the cornfield which is cultivated on the plain at top by an Indian ranchero, the traveller at length stands before the remains of the elegant structure that once crowned the summit with its carved and massive architecture. The reports of engineers who visited this pyramid in years long past, and the legends of the neighborhood, declared that it originally consisted of five stories, placed upon each other at regular intervals and separated by narrow platforms. But of all these, nothing now remains except portions of the first body, which is formed of cut porphyry and covered with the singular emblems which are accurately represented in the annexed plate of the north-western angle.
Amid the neglect of the viceroyal government, and the revolutionary disturbances subsequent to the rebellion against Spain, this beautiful monument of ancient art, seems to have been entirely forgotten, save by the neighboring haciendados or planters, who used it as a quarry, from which they might supply the wants of their estates without the trouble or expense of a stone cutter. In the middle of the eighteenth century the fine terraces were yet perfect. But, as the country became settled in the neighborhood, the farmers began to pilfer from the mass, and, not long before we visited it in 1842, an adjacent land owner had carried off large loads of the sculptured stones to build a dam in a neighboring ravine, for the use of his cattle.
The story of this pyramid that has been thus far spared, is rectangular; and, facing north, south, east and west, in exact correspondence with the cardinal points, it measures sixty-four feet on its northern front above the plinth, and fifty-eight on the western. The distance between the plinth and frieze is about ten feet, the breadth of the frieze is three feet and a half, and the height of the cornice one foot and five inches. The most perfect portion is the northern front; and, here, the carving in relief, which is between three and four inches deep, is most distinctly visible. The massive stones,—some of which are seven feet eleven inches long, by two feet nine inches wide; five feet two inches long, and two feet six inches broad, and five feet long, two feet seven inches high, and four feet seven inches broad,—are all laid upon each other without cement, and kept together simply by the pressure and gravity of the general architecture. These dimensions of the fragments of so splendid an edifice will give the reader an idea of the labor and ingenuity which were employed in its construction. For it must be remembered, that not only was the Indian skill taxed in the design and shaping of the stones in the immediate neighborhood, but that the weighty materials were drawn from a considerable distance, and borne up a hill three hundred feet in height, without the use of horses. The terraces supporting the spiral path, and their bastion-like bulwarks, were subjects of equal labor; while the broad deep ditch, surrounding the whole, was in itself a work exacting the most patient industry. Few nations have probably devoted more time and toil to a work which was perhaps partly religious and partly defensive.
These are the external works upon the Cerro of Xochicalco, but it appears from good authority, and from the report of the neighborhood, that the hill itself was partly hollowed into chambers. Some years since a party of gentlemen, under the orders of government, explored these subterranean retreats, and, after groping through dark and narrow passages, whose side walls are covered with a hard and glistening gray cement, they came to three entrances between two enormous pillars cut from the rock of which the hill is formed. Through these portals they entered a chamber, whose roof was a cupola of regular shape, built of stones placed in circles, while at the top of the dome was an aperture, which probably led to the surface of the earth or the summit of the pyramid. Nebel, who visited the ruins some years ago, relates an Indian tradition, that this aperture ascended immediately above an altar placed in this chamber, and that the sun's rays fell directly on the centre of the shrine when that luminary was vertical!
STATE OF MECHOACAN—BOUNDARIES—ELEVATIONS—VOLCANO OF JORULLO—THEORIES OF HUMBOLDT AND LYELL—PRESENT CONDITION—RIVERS OF MECHOACAN—CLIMATE—HEALTH—INDIANS—DEPARTMENTS—AGRICULTURE—TOWNS—MINES—JALISCO—BOUNDARIES—POPULATION—RIVERS—LAKES—DIVISIONS—MANUFACTURES—AGRICULTURE—FACTORIES—GUADALAJARA—TOWNS—SAN JUAN DE LOS LAGOS—TEPIC—SAN BLAS—MINES—ISLANDS—MINING REGION—INDIANS—CHARACTER AND HABITS—CHURCH AND SCHOOL—EDUCATION—BISHOPRIC—TERRITORY OF COLIMA—EXTENT—CLIMATE—PRODUCTIONS—TOWNS.
THE State of Mechoacan is the old Spanish Intendencia of Vallodolid, and includes a great part of the ancient Indian Kingdom of Mechoacan, or Mechoacan of the Tarascos. It is bounded on the north by Guanajuato, north-easterly of Querétaro, south-easterly by Mexico, westerly by Jalisco, and south-westerly, for a short distance, by the Pacific.
This State lies chiefly on the western slope of the Cordillera, and is cut up by hills and genial vallies. The highest point within its limits is the Peak of Tancitaro, which, in all probability, is an extinct volcano. East of this, and south of the village of Ario, the Volcano of Jorullo burst forth on the night of the 29th of September, 1759.
The great region to which this mountain belongs has been already described in our account of the geological structure of Mexico. The plain of Malpais forms part of an elevated platform, between 2,000 and 3,000 feet above the level of the sea, and is bounded by hills composed of basalt, trachyte, and volcanic tuff, clearly indicating that the country had previously, though probably at a remote period, been the theatre of igneous action. From the era of the discovery of the New World to the middle of the last century, the district had remained undisturbed, and the space, now the site of the volcano, which is thirty leagues distant from the nearest sea, was occupied by fertile plains of sugar cane and indigo, and watered by the two brooks, Cuitimba and San Pedro. In the month of June, 1759, hollow sounds of an alarming nature were heard, and earthquakes succeeded each other for two months, until, in September, flames issued from the ground, and fragments of burning rocks were thrown to prodigious heights.
"Six volcanic cones, composed of scoriæ and fragmentary lava, were formed on the line of a chasm which ran in a direction from N. N. E. to S. S. W. The least of these cones was 300 feet in height, and Jorullo, the central volcano, was elevated 1,600 feet above the level of the plain. It sent forth great streams of basaltic lava, containing included fragments of rocks, and its ejections did not cease till the month of February, 1760.
"Humboldt visited the country more than forty years after this occurrence, and was informed by the Indians, that when they returned, long after the catastrophe, to the plain, they found the ground uninhabitable from the excessive heat. When he himself visited the place, there appeared around the base of the cones, and spreading from them, as from a centre, over an extent of four square miles, a mass of matter of a convex form, about 550 feet high at its junction with the cones, and gradually sloping from them in all directions towards the plain. This mass was still in a heated state, the temperature in the fissures being on the decrease from year to year, but in 1780 it was still sufficient to light a cigar at the depth of a few inches. On this slightly convex protuberance, the slope of which must form an angle of about 6° with the horizon, were thousands of flattish conical mounds, from six to nine feet high, which as well as large fissures traversing the plain, acted as fumeroles, giving out clouds of sulphuric acid and hot aqueous vapor. The two small rivers before mentioned disappeared during the eruption, losing themselves below the eastern extremity of the plain, and reappearing as hot springs at its western limit. Humboldt attributed the convexity of the plain to inflation below; supposing the ground, for four square miles in extent, to have risen in the shape of a bladder to the elevation of 550 feet above the plain in the highest part. But this theory is by no means borne out by the facts described; and it is the more necessary to scrutinize closely the proofs relied on, because the opinion of Humboldt appears to have been received as if founded upon direct observation, and has been made the ground work of other bold and extraordinary theories. Mr. Scrope has suggested that the phenomena may be accounted for far more naturally by supposing that lava flowed simultaneously from the different orifices, and principally from Jorullo, united with a sort of pool or lake. As it poured forth on a surface previously flat, it would, if its liquidity was not very great, remain thickest and deepest near its source, and diminish in bulk from thence towards the limits of the space which it covered. Fresh supplies were probably emitted successively during the course of an eruption which lasted a year; and some of these, resting on those first emitted, might only spread to a small distance from the foot of the cone, where they would necessarily accumulate to a great height.
"The showers, also, of loose and pulverulent matter from the six craters, and principally from Jorullo, would be composed of heavier and more bulky particles near the cones, and would raise the ground at their base, where, mixing with rain, they might have given rise to the stratum of black clay which is described as covering the lava.
"The small conical mounds called 'hornitos' or little ovens may resemble those five or six small hillocks which existed in 1823 on the Vesuvian lava, and sent forth columns of vapor, having been produced by the disengagement of elastic fluids heaving up small dome-shaped masses of lava. The fissures mentioned by Humboldt as of frequent occurrence, are such as might naturally accompany the consolidation of a thick bed of lava, contracting as it congeals; and the appearance of rivers is the usual result of the occupation of the lower part of the valley or plain by lava, of which there are many beautiful examples in the old lava currents of Auvergne. The heat of the 'hornitos' is stated to have diminished from the first; and Mr. Bullock, who visited the spot many years after Humboldt, found the temperature of the hot spring very low,—a fact which seems clearly to indicate the gradual congelation of a subjacent bed of lava which, from its immense thickness, may have been enabled to retain its heat for half a century. The reader may be reminded, that when we thus suppose the lava near the volcano to have been, together with the ejected ashes, more than 500 feet in depth, we merely assign a thickness which the current of Skaptar Jokul attained in some places in 1783.
"Another argument adduced in the support of the theory of inflation from below, was, the hollow sound made by the steps of a horse upon the plain; which, however, proves nothing more than that the materials of which the convex mass is composed are light and porous. The sound called "rimbombo" by the Italians, is very commonly returned by made ground when sharply struck, and has been observed not only on the sides of Vesuvius and of other volcanic cones where a cavity is below, but also in plains, such as the Campagna di Roma, composed in a great measure of tuff and other porous and volcanic rocks. The reverberation, however, may be assisted by grottoes and caverns, for these may be as numerous in the lavas of Jorullo as in many of those of Etna; but their existence would lend no countenance to the hypothesis of a great arched cavity, four square miles in extent, and in the centre 550 feet high.[64]
"Mr. Burkhart, a German director of mines, who examined Jorullo in 1827, ascertained that there had been no eruption there since Humboldt's visit in 1803. He, went to the bottom of the crater, and observed a slight evolution of sulphurous acid vapors, but the "hornitos" had ceased entirely to give forth steam. During the twenty-four years intervening between his visit and that of Humboldt, vegetation had made great progress on the flanks of the new hills, and the rich soil of the surrounding country was once more covered with luxuriant crops of sugar cane and indigo, and there was an abundant growth of natural underwood on all the uncultivated tracts."[65]
The State of Mechoacan is extraordinarily rich in rivers and streams. The Lerma, Balsas, Zitacuaro, Huetamo, Cluranúeco, Marquéz, Aztala, Tlalpujahua, and some smaller streamlets and brooks are found in its vallies; while the lakes and ponds of Cuizco or Aaron, Patzcuaro, Huango, Tanguato, and Huaniqueo afford supplies to numerous neighborhoods. The climate of Mechoacan is regular, not liable to extraordinary or sudden changes, and remarkably genial. On the Pacific coast and in its vicinity, as in the other middle and southern States of the Confederacy, agues and intermittent fevers prevail; but the population seems to have increased considerably since the beginning of this century, and even in a larger proportion than in some other parts of Mexico. In 1849, the number of inhabitants was estimated to be not less than 590,000. Three Indian tribes still dwell within its borders: 1st, the Tarascos; 2d, the Otomies; 3d, the Chichimecas. The whole southern half of the State is peopled with Indians.
Mechoacan is divided into 4 departments and 62 municipalities:
| 1. | Department | del Norte, with 14 municipalities. |
| 2. | " | del Oriente, with 15 municipalities. |
| 3. | " | del Sur, with 11 municipalities. |
| 4. | " | del Poniente, with 22 municipalities. |
These 4 departments contain the three cities of Morelia, Patzcuaro, and Tzintzoutzan;—the three towns of Zitacuaro, Zamora, and Charo;—256 villages, 333 haciendas, and 1,356 ranchos, which are divided among 83 parishes.
The agricultural productions of Mechoacan are similar in character to those of the other Western States of Mexico lying within the same longitude. The best sugar plantations are about 12 leagues from Patzcuaro. At the foot of Jorullo, cotton, indigo, cacao and sugar are planted; and mainoc or cassava, potatoes and yams are sown in genial spots, whilst maiz, wheat, barley and magueys are cultivated in the higher and cooler regions. The finest tropical fruits are raised in the warm portions of the State.
The capital of Mechoacan is Morelia, sometimes called Valladolid, or Valladolid de Mechoacan. Its modern title is derived from the name of the insurgent leader Morelos.
Morelia lies 6,398 feet above the level of the sea, in latitude 19° 42´ North, 103° 12´ 15´´ W. long. from Paris,—between the two streams which water the Valley of Olid. It is a small, but handsome town, possessing some fine churches, and a charming passeo and alameda. The climate is mild and wholesome, but snow falls occasionally during the winter.
Patzcuaro lies on the south-eastern bank of the lake of that name.
Tzintzoutzan is about 4 leagues from Patzcuaro, in a northerly direction, upon the banks of the same lake. It was once the capital of the ancient Indian Kingdom of Mechoacan, but is now only a small village of 2,000 inhabitants, who have nevertheless bestowed on it the title of—"City." Some relics of the Tarascan architecture are said to be found at this place, but we do not possess any authentic accounts or drawings of them.
Zitacuaro is the capital of the old mining district 7 leagues south of Angangueo, 6,451 feet above the sea, and contains about 2000 inhabitants. Many small Indian villages are also found in the neighborhood, but they do not require special notice.
Angangueo is a mining town 7 leagues south of Tlalpujahua, with about 1,900 inhabitants.
San Pedro y San Pablo de Tlalpujahua, also a mining village and district, 35 leagues north north-west from Mexico, eastward of Morelia, and about 6 leagues south of the left bank of the Lerma. It lies in a beautiful mountain region at the foot of the Cerro del Gallo, 8,386 feet above the sea. Two leagues north of Tlalpujahua, is the Hacienda de Tepetongo, remarkable for its warm springs, which rising amid volcanic rocks, maintain a temperature of 27° Reaumeur; and are freely resorted to by the neighboring Indians. Cuizco; Huaniqueo; Zamora; Tancuancicuaro; Tarecuato; Tlazazalca, Tanguato, are the remaining towns and villages in this part of the country deserving mention. In the Department del Norte, we find Sirisicuaro; Santa Anna; Araron; Copandaro; Teremendo; Pareachecuaro, and Tirepiteo. In the Department del Oriente lie San Felipé; Patambero; Enadio; Orocutui; Tusantla; Clirangangueo; Tichiqueo; Huetano Pungarahuato; and Cayuca. In the Department del Sur, are Ario; Tacambaro; Turicato; Churumuco; Santiago Coalcoman; Uruapan and Tancitaro. In the Department del Poinente, we find Chilchote, with about 4,700 inhabitants, and Tincuindui.
The mining districts of Mechoacan are Tlalpujahua, Angangueo, and Ozumatlan. Formerly, the mines of Zitacuaro, Ingnaran, and a few other districts were somewhat renowned for their value; but, at present, they are either entirely abandoned or only slightly worked.
The present State of Jalisco and former Intendency of Guadalajara, formed together with Zacatecas, the old Spanish kingdom of New Galicia. It is bounded on the north by Durango; on the north-west by Sinaloa; on the north and east by Zacatecas and Guanajuato; on the south and south-east by Mechoacan and the Territory of Colima; and on the west by the Pacific coast, for a distance of 160 leagues. The State stretches from 19° 5´ to 23° 55´ of north latitude; and from 103° 45´ to 108° 28´ 30´´ west longitude from Paris. Its population is estimated at about 700,000.
The greater part of Jalisco lies on the western slope of the Cordillera; and its table lands, which resemble those of the great plateau of Mexico, are somewhat cut up by mountain spurs. The upper regions consequently are comparatively sterile, whilst the lowlands are rich and fruitful.
The Sierras of Bayona, in the north-west end of Chalchihuitéc, in the north-east of the State, are its most remarkable mountain ranges. The Rio Grande de Santiago is the principal stream in Jalisco; but during the six months of the dry season, its waters are either extremely shallow or disappear altogether. The Bayona is a boundary between this State and Sinaloa.
The Lake of Chapala, lies about fifteen leagues from the city of Guadalajara, and forms a basin among the mountains of 36 to 40 leagues in length by 5 to 8 in breadth. Its usual depth is about six and a half fathoms. Its scenery is remarkably beautiful, and it supplies the neighborhood plentifully with fish and water-fowl.
Jalisco is divided into eight Cantons or Departments:—Guadalajara, Lagos, La Barca, Sayula, Etzatlan, Autlan, Tepic and Colotlan;—containing 8 large cities and towns, 318 small villages, 387 haciendas or plantations, and 2,534 ranchos or farms.
The agricultural productions of Jalisco combine those of the tierras calientas and the tierras templadas. On the upper plateaus, grain and agaves are chiefly planted, and on the coast, sugar and cotton. A small quantity of cochineal is also raised, and in the district of Autlan de la Grana, plantations of the cacao-tree have been made. All the fruits of the tropical and temperate zones are readily grown; sheep, mules, horses, goats, neat-cattle, are raised in great abundance, and not less than 10,000 head of cattle are found on many haciendas de Gañado.
The manufactures of Jalisco are chiefly confined to rude cotton fabrics or some fanciful articles of dress. The people are celebrated for their gold and silver embroidery upon leather which is used in the manufacture of saddles and horse equipage.
Nearly all the importations into this State come either by land from San Luis Potosi, the city of Mexico, or San Blas, which is the chief port of Jalisco on the Pacific. A large portion of the foreign wares are doubtless smuggled into the interior, or introduced through the corrupt connivance of custom-house officers along the line of the west coast.