OF THE WEST INDIA ISLANDS.
On the evening of the 7th of February we took our departure from Caracas. Since the period of our visit to that place, tremendous earthquakes have changed the surface of the soil. The city, which I have described, has disappeared; and on the same spot, on the ground fissured5 in various directions, another city is now slowly rising. The heaps of ruins, which were the grave of a numerous population, are becoming anew the habitation of men. In retracing6 changes of so general an interest, I shall be led to notice events which took place long after my return to Europe. I shall pass over in silence the popular commotions10 which have taken place, and the modifications12 which society has undergone. Modern nations, careful of their own remembrances, snatch from oblivion the history of human revolutions, which is, in fact, the history of ardent13 passions and inveterate14 hatred15. It is not the same with respect to the revolutions of the physical world. These are described with least accuracy when they happen to be contemporary with civil dissensions. Earthquakes and eruptions of volcanoes strike the imagination by the evils which are their necessary consequence. Tradition seizes on whatever is vague and marvellous; and amid great public calamities16, as in private misfortunes, man seems to shun17 that light which leads us to discover the real causes of events, and to understand the circumstances by which they are attended.
I have recorded in this work all I have been able to collect, and on the accuracy of which I can rely, respecting the earthquake of the 26th of March, 1812. By that catastrophe18 the town of Caracas was destroyed, and more than twenty thousand persons perished throughout the extent of the province of Venezuela. The intercourse19 which I have kept up with persons of all classes has enabled me to compare the description given by many eye-witnesses, and to interrogate20 them on objects that may throw light on physical science in general. The traveller, as the historian of nature, should verify the dates of great catastrophes21, examine their connection and their mutual22 relations, and should mark in the rapid course of ages, in the continual progress of successive changes, those fixed23 points with which other catastrophes may one day be compared. All epochs are proximate to each other in the immensity of time comprehended in the history of nature. Years which have passed away seem but a few instants; and the physical descriptions of a country, even when they offer subjects of no very powerful and general interest, have at least the advantage of never becoming old. Similar considerations, no doubt, led M. de la Condamine to describe in his Voyage a l’Equateur, the memorable24 eruptions of the volcano of Cotopaxi,* which took place long after his departure from Quito. I feel the less hesitation25 in following the example of that celebrated26 traveller, as the events I am about to relate will help to elucidate27 the theory of volcanic reaction, or the influence of a system of volcanoes on a vast space of circumjacent territory.
[* Those of the 30th of November, 1744, and of the 3rd of September, 1750.]
At the time when M. Bonpland and myself visited the provinces of New Andalusia, New Barcelona, and Caracas, it was generally believed that the most eastern parts of those coasts were especially exposed to the destructive effects of earthquakes. The inhabitants of Cumana dreaded28 the valley of Caracas, on account of its damp and variable climate, and its gloomy and misty30 sky; whilst the inhabitants of the temperate31 valley regarded Cumana as a town whose inhabitants incessantly32 inhaled33 a burning atmosphere, and whose soil was periodically agitated34 by violent commotions. Unmindful of the overthrow36 of Riobamba and other very elevated towns, and not aware that the peninsula of Araya, composed of mica-slate37, shares the commotions of the calcareous coast of Cumana, well-informed persons imagined they discerned security in the structure of the primitive38 rocks of Caracas, as well as in the elevated situation of this valley. Religious ceremonies celebrated at La Guayra, and even in the capital, in the middle of the night,* doubtless called to mind the fact that the province of Venezuela had been subject at intervals40 to earthquakes; but dangers of rare occurrence are slightly feared. However, in the year 1811, fatal experience destroyed the illusion of theory and of popular opinion. Caracas, situated41 in the mountains, three degrees west of Cumana, and five degrees west of the volcanoes of the Caribbee islands, has suffered greater shocks than were ever experienced on the coast of Paria or New Andalusia.
[* For instance, the nocturnal procession of the 21st of October, instituted in commemoration of the great earthquake which took place on that day of the month, at one o’clock in the morning, in 1778. Other very violent shocks were those of 1641, 1703, and 1802.]
At my arrival in Terra Firma, I was struck with the connection between the destruction of Cumana on the 14th of December, 1797, and the eruption3 of the volcanoes in the smaller West India Islands. This connection was again manifest in the destruction of Caracas on the 26th of March, 1812. The volcano of Guadaloupe seemed in 1797 to have exercised a reaction on the coasts of Cumana. Fifteen years later, it was a volcano situated nearer the continent (that of St. Vincent), which appeared to have extended its influence as far as Caracas and the banks of Apure. Possibly, at both those periods, the centre of the explosion was, at an immense depth, equally distant from the regions towards which the motion was propagated at the surface of the globe.
From the beginning of 1811 to 1813, a vast superficies of the earth,* bound by the meridian42 of the Azores, the valley of the Ohio, the Cordilleras of New Grenada, the coasts of Venezuela, and the volcanoes of the smaller West India Islands, was shaken throughout its whole extent, by commotions which may be attributed to subterranean43 fires. The following series of phenomena seems to indicate communications at enormous distances. On the 30th of January, 1811, a submarine volcano broke out near the island of St. Michael, one of the Azores. At a place where the sea was sixty fathoms44 deep, a rock made its appearance above the surface of the waters. The heaving-up of the softened46 crust of the globe appears to have preceded the eruption of flame at the crater47, as had already been observed at the volcanoes of Jorullo in Mexico, and on the appearance of the little island of Kameni, near Santorino. The new islet of the Azores was at first a mere48 shoal; but on the 15th of June, an eruption, which lasted six days, enlarged its extent, and carried it progressively to the height of fifty toises above the surface of the sea. This new land, of which captain Tillard took possession in the name of the British government, giving it the name of Sabrina Island, was nine hundred toises in diameter. It has again, it seems, been swallowed up by the ocean. This is the third time that submarine volcanoes have presented this extraordinary spectacle near the island of St. Michael; and, as if the eruptions of these volcanoes were subject to periodical recurrence49, owing to a certain accumulation of elastic50 fluids, the island raised up has appeared at intervals of ninety-one or ninety-two years.*
[* Between latitudes51 5 and 36° north, and 31 and 91° west longitude53 from Paris.]
[* Malte–Brun, Geographie Universelle. There is, however, some doubt respecting the eruption of 1628, to which some accounts assign the date of 1638. The rising always happened near the island of St. Michael, though not identically on the same spot. It is remarkable54 that the small island of 1720 reached the same elevation55 as the island of Sabrina in 1811.]
At the time of the appearance of the new island of Sabrina, the smaller West India Islands, situated eight hundred leagues south-west of the Azores, experienced frequent earthquakes. More than two hundred shocks were felt from the month of May 1811, to April 1812, at St. Vincent; one of the three islands in which there are still active volcanoes. The commotion11 was not circumscribed56 to the insular57 portion of eastern America; and from the 16th of December, 1811, till the year 1813, the earth was almost incessantly agitated in the valleys of the Mississippi, the Arkansas river, and the Ohio. The oscillations were more feeble on the east of the Alleghanies, than to the west of these mountains, in Tennessee and Kentucky. They were accompanied by a great subterranean noise, proceeding58 from the south-west. In some places between New Madrid and Little Prairie, as at the Saline, north of Cincinnati, in latitude52 37° 45′, shocks were felt every day, nay59 almost every hour, during several months. The whole of these phenomena continued from the 16th of December 1811, till the year 1813. The commotion, confined at first to the south, in the valley of the lower Mississippi, appeared to advance slowly northward60.
Precisely61 at the period when this long series of earthquakes commenced in the Transalleghanian States (in the month of December 1811), the town of Caracas felt the first shock in calm and serene62 weather. This coincidence of phenomena was probably not accidental; for it must be borne in mind that, notwithstanding the distance which separates these countries, the low grounds of Louisiana and the coasts of Venezuela and Cumana belong to the same basin, that of the Gulf64 of Mexico. When we consider geologically the basin of the Caribbean Sea, and of the Gulf of Mexico, we find it bounded on the south by the coast-chain of Venezuela and the Cordilleras of Merida and Pamplona; on the east by the mountains of the West India Islands, and the Alleghanies; on the west by the Andes of Mexico, and the Rocky Mountains; and on the north by the very inconsiderable elevations65 which separate the Canadian lakes from the rivers which flow into the Mississippi. More than two-thirds of this basin are covered with water. It is bordered by two ranges of active volcanoes; on the east, in the Carribee Islands, between latitudes 13 and 16°; and on the west in the Cordilleras of Nicaragua, Guatimala, and Mexico, between latitudes 11 and 20°. When we reflect that the great earthquake at Lisbon, of the 1st of November, 1755, was felt almost simultaneously66 on the coasts of Sweden, at lake Ontario, and at the island of Martinique, it may not seem unreasonable68 to suppose, that all this basin of the West Indies, from Cumana and Caracas as far as the plains of Louisiana, should be simultaneously agitated by commotions proceeding from the same centre of action.
It is an opinion very generally prevalent on the coasts of Terra Firma, that earthquakes become more frequent when electric explosions have been during some years rare. It is supposed to have been observed, at Cumana and at Caracas, that the rains were less frequently attended with thunder from the year 1792; and the total destruction of Cumana in 1797, as well as the commotions felt in 1800, 1801, and 1802, at Maracaibo, Porto Cabello, and Caracas, have not failed to be attributed to an accumulation of electricity in the interior of the earth. Persons who have lived long in New Andalusia, or in the low regions of Peru, will admit that the period most to be dreaded for the frequency of earthquakes is the beginning of the rainy season, which, however, is also the season of thunder-storms. The atmosphere and the state of the surface of the globe seem to exercise an influence unknown to us on the changes which take place at great depths; and I am inclined to think that the connection which it is supposed has been traced between the absence of thunder-storms and the frequency of earthquakes, is rather a physical hypothesis framed by the half-learned of the country than the result of long experience. The coincidence of certain phenomena may be favoured by chance. The extraordinary commotions felt almost continually during the space of two years on the banks of the Mississippi and the Ohio, and which corresponded in 1812 with those of the valley of Caracas, were preceded at Louisiana by a year almost exempt69 from thunder-storms. The public mind was again struck with this phenomenon. We cannot be surprised that there should be in the native land of Franklin a great readiness to receive explanations founded on the theory of electricity.
The shock felt at Caracas in the month of December 1811, was the only one which preceded the terrible catastrophe of the 26th of March, 1812. The inhabitants of Terra Firma were alike ignorant of the agitations70 of the volcano in the island of St. Vincent, and of those felt in the basin of the Mississippi, where, on the 7th and 8th of February, 1812, the earth was day and night in perpetual oscillation. A great drought prevailed at this period in the province of Venezuela. Not a single drop of rain had fallen at Caracas or in the country to the distance of ninety leagues round, during five months preceding the destruction of the capital. The 26th of March was a remarkably73 hot day. The air was calm, and the sky unclouded. It was Ascension-day, and a great portion of the population was assembled in the churches. Nothing seemed to presage74 the calamities of the day. At seven minutes after four in the afternoon the first shock was felt. It was sufficiently75 forcible to make the bells of the churches toll76; and it lasted five or six seconds. During that interval39 the ground was in a continual undulating movement, and seemed to heave up like a boiling liquid. The danger was thought to be past, when a tremendous subterranean noise was heard, resembling the rolling of thunder, but louder and of longer continuance than that heard within the tropics in the time of storms. This noise preceded a perpendicular77 motion of three or four seconds, followed by an undulatory movement somewhat longer. The shocks were in opposite directions, proceeding from north to south, and from east to west. Nothing could resist the perpendicular movement and the transverse undulations. The town of Caracas was entirely78 overthrown79, and between nine and ten thousand of the inhabitants were buried under the ruins of the houses and churches. The procession of Ascension-day had not yet begun to pass through the streets, but the crowd was so great within the churches that nearly three or four thousand persons were crushed by the fall of the roofs. The explosion was most violent towards the north, in that part of the town situated nearest the mountain of Avila and the Silla. The churches of la Trinidad and Alta Gracia, which were more than one hundred and fifty feet high, and the naves80 of which were supported by pillars of twelve or fifteen feet diameter, were reduced to a mass of ruins scarcely exceeding five or six feet in elevation. The sinking of the ruins has been so considerable that there now scarcely remain any vestiges81 of pillars or columns. The barracks, called el Quartel de San Carlos, situated north of the church of la Trinidad, on the road from the custom-house of La Pastora, almost entirely disappeared. A regiment83 of troops of the line, under arms, and in readiness to join the procession, was, with the exception of a few men, buried beneath the ruins of the barracks. Nine-tenths of the fine city of Caracas were entirely destroyed. The walls of some houses not thrown down, as those in the street San Juan, near the Capuchin Hospital, were cracked in such a manner as to render them uninhabitable. The effects of the earthquake were somewhat less violent in the western and southern parts of the city, between the principal square and the ravine of Caraguata. There, the cathedral, supported by enormous buttresses84, remains85 standing63.
It is computed86 that nine or ten thousand persons were killed in the city of Caracas, exclusive of those who, being dangerously wounded, perished several months after, for want of food and proper care. The night of the Festival of the Ascension witnessed an awful scene of desolation and distress87. The thick cloud of dust which, rising above the ruins, darkened the sky like a fog, had settled on the ground. No commotion was felt, and never was a night more calm or more serene. The moon, then nearly at the full, illumined the rounded domes88 of the Silla, and the aspect of the sky formed a perfect contrast to that of the earth, which was covered with the bodies of the dead, and heaped with ruins. Mothers were seen bearing in their arms their children, whom they hoped to recall to life. Desolate89 families were wandering through the city, seeking a brother, a husband, or a friend, of whose fate they were ignorant, and whom they believed to be lost in the crowd. The people pressed along the streets, which could be traced only by long lines of ruins.
All the calamities experienced in the great catastrophes of Lisbon, Messina, Lima, and Riobamba were renewed at Caracas on the fatal 26th of March, 1812. Wounded persons, buried beneath the ruins, were heard imploring90 by their cries the help of the passers-by, and nearly two thousand were dug out. Never was pity more tenderly evinced; never was it more ingeniously active than in the efforts employed to save the miserable91 victims whose groans92 reached the ear. Implements93 for digging and clearing away the ruins were entirely wanting; and the people were obliged to use their bare hands, to disinter the living. The wounded, as well as the invalids94 who had escaped from the hospitals, were laid on the banks of the small river Guayra, where there was no shelter but the foliage96 of trees. Beds, linen97 to dress the wounds, instruments of surgery, medicines, every object of the most urgent necessity, was buried in the ruins. Everything, even food, was wanting; and for the space of several days water became scarce in the interior of the city. The commotion had rent the pipes of the fountains; and the falling in of the earth had choked up the springs that supplied them. To procure98 water it was necessary to go down to the river Guayra, which was considerably99 swelled100; and even when the water was obtained vessels101 for conveying it were wanting.
There was a duty to be fulfilled to the dead, enjoined102 at once by piety103 and the dread29 of infection. It being impossible to inter7 so many thousand bodies, half-buried under the ruins, commissioners104 were appointed to burn them: and for this purpose funeral piles were erected105 between the heaps of ruins. This ceremony lasted several days. Amidst so many public calamities, the people devoted106 themselves to those religious duties which they thought best fitted to appease107 the wrath108 of heaven. Some, assembling in processions, sang funeral hymns109; others, in a state of distraction110, made their confessions112 aloud in the streets. In Caracas was then repeated what had been remarked in the province of Quito, after the tremendous earthquake of 1797; a number of marriages were contracted between persons who had neglected for many years to sanction their union by the sacerdotal benediction113. Children found parents, by whom they had never till then been acknowledged; restitutions were promised by persons who had never been accused of fraud; and families who had long been at enmity were drawn114 together by the tie of common calamity115. But if this feeling seemed to calm the passions of some, and open the heart to pity, it had a contrary effect on others, rendering116 them more rigorous and inhuman117. In great calamities vulgar minds evince less of goodness than of energy. Misfortune acts in the same manner as the pursuits of literature and the study of nature; the happy influence of which is felt only by a few, giving more ardour to sentiment, more elevation to the thoughts, and increased benevolence118 to the disposition119.
Shocks as violent as those which in about the space of a minute* overthrew120 the city of Caracas, could not be confined to a small portion of the continent. Their fatal effects extended as far as the provinces of Venezuela, Varinas, and Maracaibo, along the coast; and especially to the inland mountains. La Guayra, Mayquetia, Antimano, Baruta, La Vega, San Felipe, and Merida, were almost entirely destroyed. The number of the dead exceeded four or five thousand at La Guayra, and at the town of San Felipe, near the copper121-mines of Aroa. It would appear that on a line running east-north-east and west-south-west from La Guayra and Caracas to the lofty mountains of Niquitao and Merida, the violence of the earthquake was principally directed. It was felt in the kingdom of New Grenada from the branches of the high Sierra de Santa Martha* as far as Santa Fe de Bogota and Honda, on the banks of the Magdalena, one hundred and eighty leagues from Caracas. It was everywhere more violent in the Cordilleras of gneiss and mica-slate, or immediately at their base, than in the plains; and this difference was particularly striking in the savannahs of Varinas and Casanara.* In the valleys of Aragua, between Caracas and the town of San Felipe, the commotions were very slight; and La Victoria, Maracay, and Valencia, scarcely suffered at all, notwithstanding their proximity122 to the capital. At Valecillo, a few leagues from Valencia, the yawning earth threw out such an immense quantity of water, that it formed a new torrent123. The same phenomenon took place near Porto–Cabello.* On the other hand, the lake of Maracaybo diminished sensibly. At Coro no commotion was felt, though the town is situated on the coast, between other towns which suffered from the earthquake. Fishermen, who had passed the day of the 26th of March in the island of Orchila, thirty leagues north-east of La Guayra, felt no shock. These differences in the direction and propagation of the shock, are probably owing to the peculiar124 position of the stony125 strata126.
[* The duration of the earthquake, that is to say the whole of the movements of undulation and rising (undulacion y trepidacion), which occasioned the horrible catastrophe of the 26th of March, 1812, was estimated by some at 50 seconds, by others at 1 minute 12 seconds.]
[* As far as Villa127 de Los Remedios, and even to Carthagena.]
[* This is easily explained according to the system of those geologists128 who are of opinion that all chains of mountains, volcanic and not volcanic, have been formed by being raised up, as if through crevices130.]
[* It is asserted that, in the mountains of Aroa, the ground, immediately after the great shocks, was found covered with a very fine and white earth, which appeared to have been projected through crevices.]
Having thus traced the effects of the earthquake to the west of Caracas, as far as the snowy mountains of Santa Martha, and the table-land of Santa Fe de Bogota, we will proceed to consider their action on the country eastward131 of the capital. The commotions were very violent beyond Caurimare, in the valley of Capaya, where they extended as far as the meridian of Cape95 Codera: but it is extremely remarkable that they were very feeble on the coasts of Nueva Barcelona, Cumana, and Paria; though these coasts are the continuation of the shore of La Guayra, and were formerly132 known to have been often agitated by subterranean commotions. Admitting that the destruction of the four towns of Caracas, La Guayra, San Felipe, and Merida, may be attributed to a volcanic focus situated under or near the island of St. Vincent, we may conceive that the motion might have been propagated from north-east to south-west in a line passing through the islands of Los Hermanos, near Blanquilla, without touching133 the coasts of Araya, Cumana, and Nueva Barcelona. This propagation of the shock might even have taken place without any commotion having been felt at the intermediate points on the surface of the globe (the Hermanos Islands for instance). This phenomenon is frequently remarked at Peru and Mexico, in earthquakes which have followed during ages a fixed direction. The inhabitants of the Andes say, speaking of an intermediary tract111 of ground, not affected134 by the general commotion, “that it forms a bridge” (que hace puente): as if they mean to indicate by this expression that the undulations are propagated at an immense depth under an inert136 rock.
At Caracas, fifteen or eighteen hours after the great catastrophe, the earth was tranquil137. The night, as has already been observed, was fine and calm; and the commotions did not recommence till after the 27th. They were then attended by a very loud and long continued subterranean noise (bramido). The inhabitants of the destroyed city wandered into the country; but the villages and farms having suffered as much as the town, they could find no shelter till they were beyond the mountains of los Teques, in the valleys of Aragua, and in the llanos or savannahs. No less than fifteen oscillations were felt in one day. On the 5th of April there was almost as violent an earthquake as that which overthrew the capital. During several hours the ground was in a state of perpetual undulation. Large heaps of earth fell in the mountains; and enormous masses of rock were detached from the Silla of Caracas. It was even asserted, and this opinion prevails still in the country, that the two domes of the Silla sunk fifty or sixty toises; but this statement is not founded on any measurement. I am informed that, in like manner, in the province of Quito, the people, at every period of great commotions, imagine that the volcano of Tunguragua diminishes in height. It has been affirmed, in many published accounts of the destruction of Caracas, that the mountain of the Silla is an extinguished volcano; that a great quantity of volcanic substances are found on the road from La Guayra to Caracas; that the rocks do not present any regular stratification; and that everything bears the stamp of the action of fire. It has even been stated that twelve years prior to the great catastrophe, M. Bonpland and myself had, from our own observations, considered the Silla as a very dangerous neighbour to the city of Caracas, because the mountain contained a great quantity of sulphur, and the commotions must come from the north-east. It is seldom that observers of nature have to justify138 themselves for an accomplished139 prediction; but I think it my duty to oppose ideas which are too easily adopted on the LOCAL CAUSES of earthquakes.
In all places where the soil has been incessantly agitated for whole months, as at Jamaica in 1693, Lisbon in 1755, Cumana in 1766, and Piedmont in 1808, a volcano is expected to open. People forget that we must seek the focus or centre of action, far from the surface of the earth; that, according to undeniable evidence, the undulations are propagated almost at the same instant across seas of immense depth, at the distance of a thousand leagues; and that the greatest commotions take place not at the foot of active volcanoes, but in chains of mountains composed of the most heterogeneous140 rocks. In our geognostical observation of the country round Caracas we found gneiss, and mica-slate containing beds of primitive limestone141. The strata are scarcely more fractured or irregularly inclined than near Freyburg in Saxony, or wherever mountains of primitive formation rise abruptly142 to great heights. I found at Caracas neither basalt nor dorolite, nor even trachytes or trap-porphyries; nor in general any trace of an extinguished volcano, unless we choose to regard the diabases of primitive grunstein, contained in gneiss, as masses of lava143, which have filled up fissures144. These diabases are the same as those of Bohemia, Saxony, and Franconia;* and whatever opinion may be entertained respecting the ancient causes of the oxidation of the globe at its surface, all those primitive mountains, which contain a mixture of hornblende and feldspar, either in veins145 or in balls with concentric layers, will not, I presume, be called volcanic formations. Mont Blanc and Mont d’Or will not be ranged in one and the same class. Even the partisans147 of the Huttonian or volcanic theory make a distinction between the lavas148 melted under the mere pressure of the atmosphere at the surface of the globe, and those layers formed by fire beneath the immense weight of the ocean and superincumbent rocks. They would not confound Auvergne and the granitic149 valley of Caracas in the same denomination150; that of a country of extinct volcanoes.
[* These grunsteins are found in Bohemia, near Pilsen, in granite151; in Saxony, in the mica-slates152 of Scheenberg; in Franconia, between Steeben and Lauenstein, in transition-slates.]
I never could have pronounced the opinion, that the Silla and the Cerro de Avila, mountains of gneiss and mica-slate, were in dangerous proximity to the city of Caracas because they contained a great quantity of pyrites in subordinate beds of primitive limestone. But I remember having said, during my stay at Caracas, that the eastern extremity153 of Terra Firma appeared, since the great earthquake of Quito, in a state of agitation71, which warranted apprehension154 that the province of Venezuela would gradually be exposed to violent commotions. I added, that when a country had been long subject to frequent shocks, new subterranean communications seemed to open with neighbouring countries; and that the volcanoes of the West India Islands, lying in the direction of the Silla, north-east of the city, were perhaps the vents8, at the time of an eruption, for those elastic fluids which cause earthquakes on the coasts of the continent. These considerations, founded on local knowledge of the place, and on simple analogies, are very far from a prediction justified155 by the course of physical events.
On the 30th of April, 1812, whilst violent commotions were felt simultaneously in the valley of the Mississippi, in the island of St. Vincent, and in the province of Venezuela, a subterranean noise resembling frequent discharges of large cannon156 was heard at Caracas, at Calabozo (situated in the midst of the steppes), and on the borders of the Rio Apure, over a superficies of four thousand square leagues. This noise began at two in the morning. It was accompanied by no shock; and it is very remarkable, that it was as loud on the coast as at the distance of eighty leagues inland. It was everywhere believed to be transmitted through the air; and was so far from being thought a subterranean noise, that in several places, preparations were made for defence against an enemy, who seemed to be advancing with heavy artillery157. Senor Palacio, crossing the Rio Apure below the Orivante, near the junction158 of the Rio Nula, was told by the inhabitants, that the firing of cannon had been heard distinctly at the western extremity of the province of Varinas, as well as at the port of La Guayra to the north of the chain of the coast.
The day on which the inhabitants of Terra Firma were alarmed by a subterranean noise was that of the great eruption of the volcano in the island of St. Vincent. That mountain, near five hundred toises high, had not thrown out lava since the year 1718. Scarcely was any smoke perceived to issue from it, when, in the month of May 1811, frequent shocks announced that the volcanic fire was either rekindled159, or directed anew to that part of the West Indies. The first eruption did not take place till the 27th of April, 1812, at noon. It was merely an ejection of ashes, but attended with a tremendous noise. On the 30th, the lava overflowed160 the brink161 of the crater, and, after a course of four hours, reached the sea. The sound of the explosion is described as resembling that of alternate discharges of very large cannon and musketry; and it is worthy162 of remark, that it seemed much louder to persons out at sea, and at a great distance from land, than to those within sight of land, and near the burning volcano.
The distance in a straight line from the volcano of St. Vincent to the Rio Apure, near the mouth of the Nula, is two hundred and ten leagues.* The explosions were consequently heard at a distance equal to that between Vesuvius and Paris. This phenomenon, in conjunction with a great number of facts observed in the Cordilleras of the Andes, shows that the sphere of the subterranean activity of a volcano is much more extensive than we should be disposed to admit, if we judged merely from the small changes effected at the surface of the globe. The detonations163 heard during whole days together in the New World, eighty, one hundred, or even two hundred leagues distant from a crater, do not reach us by the propagation of the sound through the air; they are transmitted by the earth, perhaps in the very place where we happen to be. If the eruptions of the volcano of St. Vincent, Cotopaxi, or Tunguragua, resounded164 from afar, like a cannon of immense magnitude, the noise ought to increase in the inverse165 ratio of the distance: but observations prove, that this augmentation does not take place. I must further observe, that M. Bonpland and I, going from Guayaquil to the coast of Mexico, crossed latitudes in the Pacific, where the crew of our ship were dismayed by a hollow sound coming from the depth of the ocean, and transmitted by the waters. At that time a new eruption of Cotopaxi took place, but we were as far distant from the volcano, as Etna from the city of Naples. The little town of Honda, on the banks of the Magdalena, is not less than one hundred and forty-five leagues* from Cotopaxi; and yet, in the great explosions of this volcano, in 1744, a subterranean noise was heard at Honda, and supposed to be discharges of heavy artillery. The monks167 of San Francisco spread a report that the town of Carthagena was besieged168 and bombarded by the English; and the intelligence was believed throughout the country. Now the volcano of Cotopaxi is a cone169, more than one thousand eight hundred toises above the basin of Honda, and it rises from a table-land, the elevation of which is more than one thousand five hundred toises above the valley of the Magdalena. In all the colossal170 mountains of Quito, of the province of los Pastos, and of Popayan, crevices and valleys without number intervene. It cannot be admitted, under these circumstances, that the noise was transmitted through the air, or over the surface of the globe, and that it came from the point at which the cone and crater of Cotapaxi are situated. It appears probable, that the more elevated part of the kingdom of Quito and the neighbouring Cordilleras, far from being a group of distinct volcanoes, constitute a single swollen171 mass, an enormous volcanic wall, stretching from south to north, and the crest172 of which presents a superficies of more than six hundred square leagues. Cotopaxi, Tunguragua, Antisana, and Pichincha, are on this same raised ground. They have different names, but they are merely separate summits of the same volcanic mass. The fire issues sometimes from one, sometimes from another of these summits. The obstructed173 craters174 appear to be extinguished volcanoes; but we may presume, that, while Cotopaxi or Tunguragua have only one or two eruptions in the course of a century, the fire is not less continually active under the town of Quito, under Pichincha and Imbabura.
[* Where the contrary is not expressly stated, nautical175 leagues of twenty to a degree, or two thousand eight hundred and fifty-five toises, are always to be understood.]
[* This is the distance from Vesuvius to Mont Blanc.]
Advancing northward we find, between the volcano of Cotopaxi and the town of Honda, two other systems of volcanic mountains, those of los Pastos and of Popayan. The connection between these systems was manifested in the Andes by a phenomenon which I have already had occasion to notice, in speaking of the last destruction of Cumana. In the month of November 1796 a thick column of smoke began to issue from the volcano of Pasto, west of the town of that name, and near the valley of Rio Guaytara. The mouths of the volcano are lateral176, and situated on its western declivity177, yet during three successive months the column of smoke rose so much higher than the ridge135 of the mountain that it was constantly visible to the inhabitants of the town of Pasto. They described to us their astonishment178 when, on the 4th of February, 1797, they observed the smoke disappear in an instant, whilst no shock whatever was felt. At that very moment, sixty-five leagues southward, between Chimborazo, Tunguragua, and the Altar (Capac–Urcu), the town of Riobamba was overthrown by the most terrible earthquake on record. Is it possible to doubt, from this coincidence of phenomena, that the vapours issuing from the small apertures180 or ventanillas of the volcano of Pasto had an influence on the pressure of those elastic fluids which convulsed the earth in the kingdom of Quito, and destroyed in a few minutes thirty or forty thousand inhabitants?
To explain these great effects of volcanic reactions, and to prove that the group or system of the volcanoes of the West India Islands may sometimes shake the continent, I have cited the Cordillera of the Andes. Geological reasoning can be supported only by the analogy of facts which are recent, and consequently well authenticated181: and in what other region of the globe could we find greater and more varied182 volcanic phenomena than in that double chain of mountains heaved up by fire? in that land where nature has covered every mountain and every valley with her marvels183? If we consider a burning crater only as an isolated184 phenomenon, if we be satisfied with merely examining the mass of stony substances which it has thrown up, the volcanic action at the surface of the globe will appear neither very powerful nor very extensive. But the image of this action becomes enlarged in the mind when we study the relations which link together volcanoes of the same group; for instance, those of Naples and Sicily, of the Canary Islands,* of the Azores, of the Caribbee islands of Mexico, of Guatimala, and of the table-land of Quito; when we examine either the reactions of these different systems of volcanoes on one another, or the distance at which, by subterranean communication, they simultaneously convulse the earth. (I have already observed (Chapter 1.2) that the whole group of the Canary Islands rises, as we may say, above one and the same submarine volcano. Since the sixteenth century, the fire of this volcano has burst forth185 alternately in Palma, Teneriffe, and Lancerote. Auvergne presents a whole system of volcanoes, the action of which has now ceased; but in the middle of a system of active volcanoes, for instance, in that of Quito, we must not consider as an extinguished volcano a mountain, the crater of which is obstructed, and through which the subterraneous fire has not issued for ages. Etna, the Aeolian Isles186, Vesuvius, and Epomeo; the peak of Teyde, Palma, and Lancerote; St. Michael, La Caldiera of Fayal, and Pico; St. Vincent, St. Lucia, and Guadaloupe; Orizava, Popocatepetl, Jorullo, and La Colima; Bombacho, the volcano of Grenada, Telica, Momotombo, Isalco, and the volcano of Guatimala; Cotopaxi, Tunguragua, Pichincha, Antisana, and Sangai, belong to the same system of burning volcanoes; they are generally ranged in rows, as if they had issued from a crevice129, or vein146 not filled up; and, it is very remarkable, that their position is in some parts in the general direction of the Cordilleras, and in others in a contrary direction.)
The study of volcanoes may be divided into two distinct branches; one, simply mineralogical, is directed to the examination of the stony strata, altered or produced by the action of fire; from the formation of the trachytes or trap-porphyries, of basalts, phonolites, and dolerites, to the most recent lavas: the other branch, less accessible and more neglected, comprehends the physical relations which link volcanoes together, the influence of one volcanic system on another, the connection existing between the action of burning mountains and the commotions which agitate35 the earth at great distances, and during long intervals, in the same direction. This study cannot progress till the various epochs of simultaneous action, the direction, the extent, and the force of the convulsions are carefully noted187; till we have attentively188 observed their progressive advance to regions which they had not previously189 reached; and the coincidence between distant volcanic eruptions and those noises which the inhabitants of the Andes very expressively190 term subterraneous thunders, or roarings.* All these objects are comprehended in the domain191 of the history of nature.
[* Bramidos y truenos subterraneos.]
Though the narrow circle within which all certain traditions are confined, does not present any of those general revolutions which have heaved up the Cordilleras and buried myriads192 of pelagian animals; yet Nature, acting193 under our eyes, nevertheless exhibits violent though partial changes, the study of which may throw light on the most remote epochs. In the interior of the earth those mysterious powers exist, the effects of which are manifested at the surface by the production of vapours, of incandescent194 scoriae, of new volcanic rocks and thermal195 springs, by the appearance of new islands and mountains, by commotions propagated with the rapidity of an electric shock, finally by those subterranean thunders,* heard during whole months, without shaking the earth, in regions far distant from active volcanoes.
[* In the town of Guanaxuato, in Mexico, these thunders lasted from the 9th of January till the 12th of February, 1784. Guanaxuato is situated forty leagues north of the volcano of Jorullo, and sixty leagues north west of the volcano of Popocatepetl. In places nearer these two volcanoes, three leagues distant from Guanaxuato, the subterranean thunders were not heard. The noise was circumscribed within a very narrow space, in the region of a primitive schist, which approaches a transition-schist, containing the richest silver mines of the known world, and on which rest trap-porphyries, slates, and diabasis (grunstein.)]
In proportion as equinoctial America shall increase in culture and population, and the system of volcanoes of the central table-land of Mexico, of the Caribbee Islands, of Popayan, of los Pastos, and Quito, shall be more attentively observed, the connection of eruptions and of earthquakes, which precede and sometimes accompany those eruptions, will be more generally recognized. The volcanoes just mentioned, particularly those of the Andes, which rise above the enormous height of two thousand five hundred toises, present great advantages for observation. The periods of their eruptions are singularly regular. They remain thirty or forty years without emitting scoriae, ashes, or even vapours. I could not perceive the smallest trace of smoke on the summit of Tunguragua or Cotopaxi. A gust196 of vapour issuing from the crater of Mount Vesuvius scarcely attracts the attention of the inhabitants of Naples, accustomed to the movements of that little volcano, which throws out scoriae sometimes during two or three years successively. Thence it becomes difficult to judge whether the emission197 of scoriae may have been more frequent at the time when an earthquake has been felt in the Apennines. On the ridge of the Cordilleras everything assumes a more decided198 character. An eruption of ashes, which lasts only a few minutes, is often followed by a calm of ten years. In such circumstances it is easy to mark the periods, and to observe the coincidence of phenomena.
If, as there appears to be little reason to doubt, that the destruction of Cumana in 1797, and of Caracas in 1812, indicate the influence of the volcanoes of the West India Islands* on the commotions felt on the coasts of Terra Firma, it may be desirable, before we close this chapter, to take a cursory199 view of this Mediterranean200 archipelago.
[* The following is the series of the phenomena:—
27th of September, 1796. Eruption in the West India Islands. (Volcano of Guadaloupe).
November, 1796. The volcano of Pasto began to emit smoke.
14th of December, 1796. Destruction of Cumana.
4th of February, 1797. Destruction of Riobamba.
30th of January, 1811. Appearance of Sabrina Island, in the Azores. The island enlarged very considerably on the 15th of June, 1811.
May, 1811. Commencement of the earthquakes in the island of St. Vincent, which lasted till May 1812.
16th of December, 1811. Commencement of the commotions in the valley of the Mississippi and the Ohio, which lasted till 1813.
December, 1811. Earthquake at Caracas.
26th of March, 1811. Destruction of Caracas. Earthquakes, which continued till 1813.
30th of April, 1811. Eruption of the volcano in St. Vincent; and the same day subterranean noises at Caracas, and on the banks of the Apure.]
The volcanic islands form one-fifth of that great arc extending from the coast of Paria to the peninsula of Florida. Running from south to north, they close the Caribbean Sea on the eastern side, while the greater West India Islands appear like the remains of a group of primitive mountains, the summit of which seems to have been between Cape Abacou, Point Morant, and the Copper Mountains, in that part where the islands of St. Domingo, Cuba, and Jamaica, are nearest to each other. Considering the basin of the Atlantic as an immense valley* which separates the two continents, and where, from 20° south to 30° north, the salient angles (Brazil and Senegambia) correspond to the receding72 angles (the gulf of Guinea and the Caribbean Sea), we are led to think that the latter sea owes its formation to the action of currents, which, like the current of rotation201 now existing, have flowed from east to west; and have given the southern coast of Porto Rico, St. Domingo, and the island of Cuba their uniform configuration202. This supposition of an oceanic irruption has been the source of two other hypotheses on the origin of the smaller West India Islands. Some geologists admit that the uninterrupted chain of islands from Trinidad to Florida exhibits the remains of an ancient chain of mountains. They connect this chain sometimes with the granite of French Guiana, sometimes with the calcareous mountains of Pari. Others, struck with the difference of geological constitution between the primitive mountains of the Greater and the volcanic cones203 of the Lesser204 Antilles, consider the latter as having risen from the bottom of the sea.
[* The valley is narrowest (300 leagues) between Cape St. Roque and Sierra Leone. Proceeding toward the north along the Coasts of the New Continent, from its pyramidal extremity, or the Straits of Magellan, we imagine we recognise the effects of a repulsion directed first toward the north-east, then toward the north-west, and finally again to the north-east.]
If we recollect205 that volcanic upheavings, when they take place through elongated206 crevices, usually take a straight direction, we shall find it difficult to judge from the disposition of the craters alone, whether the volcanoes have belonged to the same chain, or have always been isolated. Supposing an irruption of the ocean to take place either into the eastern part of the island of Java* or into the Cordilleras of Guatimala and Nicaragua, where so many burning mountains form but one chain, that chain would be divided into several islands, and would perfectly207 resemble the Caribbean Archipelago. The union of primitive formations and volcanic rocks in the same range of mountain is not extraordinary; it is very distinctly seen in my geological sections of the Cordillera of the Andes. The trachytes and basalts of Popayan are separated from the system of the volcanoes of Quito by the mica-slates of Almaguer; the volcanoes of Quito from the trachytes of Assuay by the gneiss of Condorasta and Guasunto. There does not exist a real chain of mountains running south-east and north-west from Oyapoc to the mouths of the Orinoco, and of which the smaller West India Islands might be a northern prolongation. The granites208 of Guiana, as well as the hornblende-slates, which I saw near Angostura, on the banks of the Lower Orinoco, belong to the mountains of Pacaraimo and of Parime, stretching from west to east, * (From the cataracts209 of Atures towards the Essequibo River. This chain of Pacaraimo divides the waters of the Carony from those of the Rio Parime, or Rio de Aguas Blancas.) in the interior of the continent, and not in a direction parallel with the coast, between the mouths of the river Amazon and the Orinoco. But though we find no chain of mountains at the north-east extremity of Terra Firma, having the same direction as the archipelago of the smaller West India Islands, it does not therefore follow that the volcanic mountains of the archipelago may not have belonged originally to the continent, and formed a part of the littoral210 chain of Caracas and Cumana.*
[* Raffles211, History of Java, 1817, pages 23–28. The principal line of the volcanoes of Java, on a distance of 160 leagues, runs from west to east, through the mountains of Gagak, Gede, Tankuban–Prahu, Ungarang Merapi, Lawu, Wilis, Arjuna, Dasar, and Tashem.]
[* Among many such examples which the structure of the globe displays, we shall mention only the inflexion at a right angle formed by the Higher Alps towards the maritime212 Alps, in Europe; and the Belour–Tagh, which joins transversely the Mouz–Tagh and the Himalaya, in Asia. Amid the prejudices which impede213 the progress of mineralogical geography, we may reckon, 1st, the supposition of a perfect uniformity of direction in the chains of mountains; 2nd, the hypothesis of the continuity of all chains; 3rd, the supposition that the highest summits determine the direction of a central chain; 4th, the idea that, in all places where great rivers take rise, we may suppose the existence of great tablelands, or very high mountains.]
In opposing the objections of some celebrated naturalists215, I am far from maintaining the ancient contiguity216 of all the smaller West India Islands. I am rather inclined to consider them as islands heaved up by fire, and ranged in that regular line, of which we find striking examples in so many volcanic hills in Auvergne, in Mexico, and in Peru. The geological constitution of the Archipelago appears, from the little we know respecting it, to be very similar to that of the Azores and the Canary Islands. Primitive formations are nowhere seen above ground; we find only what belongs unquestionably to volcanoes: feldspar-lava, dolerite, basalt, conglomerated scoriae, tufa, and pumice-stone. Among the limestone formations we must distinguish those which are essentially217 subordinate to volcanic tufas* from those which appear to be the work of madrepores and other zoophytes. The latter, according to M. Moreau de Jonnes, seem to lie on shoals of a volcanic nature. Those mountains, which present traces of the action of fire more or less recent, and some of which reach nearly nine hundred toises of elevation, are all situated on the western skirt of the smaller West India Islands.* Each island is not the effect of one single heaving-up: most of them appear to consist of isolated masses which have been progressively united together. The matter has not been emitted from one crater, but from several; so that a single island of small extent contains a whole system of volcanoes, regions purely218 basaltic, and others covered with recent lavas. The volcanoes still burning are those of St. Vincent, St. Lucia, and Guadaloupe. The first threw out lava in 1718 and 1812; in the second there is a continual formation of sulphur by the condensation219 of vapours, which issue from the crevices of an ancient crater. The last eruption of the volcano of Guadaloupe took place in 1797. The Solfatara of St. Christopher’s was still burning in 1692. At Martinique, Vauclin, Montagne Pelee, and the crater surrounded by the five Paps of Carbet, must be considered as three extinguished volcanoes. The effects of thunder have been often confounded in that place with subterranean fire. No good observation has confirmed the supposed eruption of the 22nd of January, 1792. The group of volcanoes in the Caribbee Islands resembles that of the volcanoes of Quito and Los Pastos; craters with which the subterranean fire does not appear to communicate are ranged on the same line with burning craters, and alternate with them.
[* We have noticed some of the above, following Von Buch, at Lancerote, and at Fortaventura, in the system of the Canary Islands. Among the smaller islands of the West Indies, the following islets are entirely calcareous, according to M. Cortes: Mariegalante, La Desirade, the Grande Terre of Guadaloupe, and the Grenadillas. According to the observations of that naturalist214, Curacoa and Buenos Ayres present only calcareous formations. M. Cortes divides the West India Islands into, 1st, those containing at once primitive, secondary, and volcanic formations, like the greater islands; 2nd, those entirely calcareous, (or at least so considered) as Mariegalante and Curacoa; 3rd, those at once volcanic and calcareous, as Antigua, St. Bartholomew, St. Martin, and St. Thomas; 4th, those which have volcanic rocks only, as St. Vincent, St. Lucia, and St. Eustache.]
[* Journal des Mines, tome 3 page 59. In order to exhibit in one point of view the whole system of the volcanoes of the smaller West India Islands, I will here trace the direction of the islands from south to north. — Grenada, an ancient crater, filled with water; boiling springs; basalts between St. George and Goave. — St. Vincent, a burning volcano. — St. Lucia, a very active solfatara, named Oualibou, two or three hundred toises high; jets of hot water, by which small basins are periodically filled. — Martinique, three great extinguished volcanoes; Vauclin, the Paps of Carbet, which are perhaps the most elevated summits of the smaller islands, and Montagne Pelee. (The height of this last mountain is probably 800 toises; according to Leblond it is 670 toises; according to Dupuget, 736 toises. Between Vauclin and the feldspar-lavas of the Paps of Carbet is found, as M. Moreau de Jonnes asserts, in a neck of land, a region of early basalt called La Roche Carree). Thermal waters of Precheur and Lameutin. — Dominica, completely volcanic. — Guadaloupe, an active volcano, the height of which, according to Leboucher, is 799 toises; according to Amie, 850 toises. — Montserrat, a solfatara; fine porphyritic lavas with large crystals of feldspar and hornblende near Galloway, according to Mr. Nugent. — Nevis, a solfatara. — St. Christopher’s, a solfatara at Mount Misery220. — St. Eustache, a crater of an extinguished volcano, surrounded by pumice-stone. (Trinidad, which is traversed by a chain of primitive slate, appears to have anciently formed a part of the littoral chain of Cumana, and not of the system of the mountains of the Caribbee Islands.)]
Notwithstanding the intimate connection manifested in the action of the volcanoes of the smaller West India Islands and the earthquakes of Terra Firma, it often happens that shocks felt in the volcanic archipelago are not propagated to the island of Trinidad, or to the coasts of Caracas and Cumana. This phenomenon is in no way surprising: even in the Caribbees the commotions are often confined to one place. The great eruption of the volcano in St. Vincent’s did not occasion an earthquake at Martinique or Guadaloupe. Loud explosions were heard there as well as at Venezuela, but the ground was not convulsed.
These explosions must not be confounded with the rolling noise which everywhere precedes the slightest commotions; they are often heard on the banks of the Orinoco, and (as we were assured by persons living on the spot) between the Rio Arauca and Cuchivero. Father Morello relates that at the Mission of Cabruta the subterranean noise so much resembles discharges of small cannon (pedreros) that it has seemed as if a battle were being fought at a distance. On the 21st of October, 1766, the day of the terrible earthquake which desolated221 the province of New Andalusia, the ground was simultaneously shaken at Cumana, at Caracas, at Maracaybo, and on the banks of the Casanare, the Meta, the Orinoco, and the Ventuario. Father Gili has described these commotions at the Mission of Encaramada, a country entirely granitic, where they were accompanied by loud explosions. Great fallings-in of the earth took place in the mountain Paurari, and near the rock Aravacoto a small island disappeared in the Orinoco. The undulatory motion continued during a whole hour. This seemed the first signal of those violent commotions which shook the coasts of Cumana and Cariaco for more than ten months. It might be supposed that men living in woods, with no other shelter than huts of reeds and palm-leaves, could have little to dread from earthquakes. But at Erevato and Caura, where these phenomena are of rare occurrence, they terrify the Indians, frighten the beasts of the forests, and impel222 the crocodiles to quit the waters for the shore. Nearer the sea, where shocks are frequent, far from being dreaded by the inhabitants, they are regarded with satisfaction as the prognostics of a wet and fertile year.
In this dissertation223 on the earthquakes of Terra Firma and on the volcanoes of the neighbouring archipelago of the West India Islands, I have pursued the plan of first relating a number of particular facts, and then considering them in one general point of view. Everything announces in the interior of the globe the operation of active powers, which, by mutual reaction, balance and modify one another. The greater our ignorance of the causes of these undulatory movements, these evolutions of heat, these formations of elastic fluids, the more it becomes the duty of persons who apply themselves to the study of physical science to examine the relations which these phenomena so uniformly present at great distances apart. It is only by considering these various relations under a general point of view, and tracing them over a great extent of the surface of the globe, through formations of rocks the most different, that we are led to abandon the supposition of trifling224 local causes, strata of pyrites, or of ignited coal.*
[* See “Views of Nature”— On the structure and action of volcanoes in different parts of the world, page 353 (Bohn’s edition); also “Cosmos” pages 199–225 (Bohn’s edition).]
The following is the series of phenomena remarked on the northern coasts of Cumana, Nueva Barcelona, and Caracas; and presumed to be connected with the causes which produce earthquakes and eruptions of lava. We shall begin with the most eastern extremity, the island of Trinidad; which seems rather to belong to the shore of the continent than to the system of the mountains of the West India Islands.
1. The pit which throws up asphaltum in the bay of Mayaro, on the eastern coast of the island of Trinidad, southward of Point Guataro. This is the mine of chapapote or mineral tar67 of the country. I was assured that in the months of March and June the eruptions are often attended with violent explosions, smoke, and flames. Almost on the same parallel, and also in the sea, but westward225 of the island (near Punta de la Brea, and to the south of the port of Naparaimo), we find a similar vent9. On the neighbouring coast, in a clayey ground, appears the celebrated lake of asphaltum (Laguna de la Brea), a marsh226, the waters of which have the same temperature as the atmosphere. The small cones situated at the south-western extremity of the island, between Point Icacos and the Rio Erin, appear to have some analogy with the volcanoes of air and mud which I met with at Turbaco in the kingdom of New Grenada. I mention these situations of asphaltum on account of the remarkable circumstances peculiar to them in these regions; for I am not unaware227 that naphtha, petroleum228, and asphaltum are found equally in volcanic and secondary regions,* and even more frequently in the latter. Petroleum is found floating on the sea thirty leagues north of Trinidad, around the island of Grenada, which contains an extinguished crater and basalts.
[* The inflammable emanations of Pietra Mala, (consisting of hydrogen gas containing naphtha in a state of suspension) issue from the Alpine229 limestone, which may be traced from Covigliano to Raticofa, and which lies on ancient sandstone near Scarica l’Asino. Under this sandstone (old red sandstone) we find black transition limestone and the grauwack (quartzose psammite) of Florence.]
2. Hot Springs of Irapa, at the north-eastern extremity of New Andalusia, between Rio Caribe, Soro, and Yaguarapayo.
3. Air-volcano, or Salce, of Cumacatar, to the south of San Jose and Carupano, near the northern coast of the continent, between La Montana de Paria and the town of Cariaco. Almost constant explosions are felt in a clayey soil, which is affirmed to be impregnated with sulphur. Hot sulphureous waters gush230 out with such violence that the ground is agitated by very sensible shocks. It is said that flames have been frequently seen issuing out since the great earthquake of 1797. These facts are well worthy of being examined.
4. Petroleum-spring of the Buen Pastor82, near Rio Areo. Large masses of sulphur have been found in clayey soils at Guayuta, as in the valley of San Bonifacio, and near the junction of the Rio Pao with the Orinoco.
5. The Hot Waters (Aguas Calientes) south of the Rio Azul, and the Hollow Ground of Cariaco, which, at the time of the great earthquake of Cumana, threw up sulphuretted water and viscous231 petroleum.
6. Hot waters of the gulf of Cariaco.
7. Petroleum-spring in the same gulf, near Maniquarez. It issues from mica-slate.
8. Flames issuing from the earth, near Cumana, on the banks of the Manzanares, and at Mariguitar, on the southern coast of the gulf of Cariaco, at the time of the great earthquake of 1797.
9. Igneous232 phenomena of the mountain of Cuchivano, near Cumanacoa.
10. Petroleum-spring gushing233 from a shoal to the north of the Caracas Islands. The smell of this spring warns ships of the danger of this shoal, on which there is only one fathom45 of water.
11. Thermal springs of the mountain of the Brigantine, near Nueva Barcelona. Temperature 43.2° (centigrade).
12. Thermal springs of Provisor, near San Diego, in the province of New Barcelona.
13. Thermal springs of Onoto, between Turmero and Maracay, in the valleys of Aragua, west of Caracas.
14. Thermal springs of Mariara, in the same valleys. Temperature 58.9°.
15. Thermal springs of Las Trincheras, between Porto Cabello and Valencia, issuing from granite like those of Mariara, and forming a river of warm water (Rio de Aguas Calientes). Temperature 90.4°.
16. Boiling springs of the Sierra Nevada of Merida.
17. Aperture179 of Mena, on the borders of Lake Maracaybo. It throws up asphaltum, and is said to emit gaseous234 emanations, which ignite spontaneously, and are seen at a great distance.
These are the springs of petroleum and of thermal waters, the igneous meteors, and the ejections of muddy substances attended with explosions, of which I acquired a knowledge in the vast provinces of Venezuela, whilst travelling over a space of two hundred leagues from east to west. These various phenomena have occasioned great excitement among the inhabitants since the catastrophes of 1797 and 1812: yet they present nothing which constitutes a volcano, in the sense hitherto attributed to that word. If the apertures, which throw up vapours and water with violent noise, be sometimes called volcancitos, it is only by such of the inhabitants as persuade themselves that volcanoes must necessarily exist in countries so frequently exposed to earthquakes. Advancing from the burning crater of St. Vincent in the directions of south, west and south-west, first by the chain of the Caribbee Islands, then by the littoral chain of Cumana and Venezuela, and finally by the Cordilleras of New Grenada, along a distance of three hundred and eighty leagues, we find no active volcano before we arrive at Purace, near Popayan. The total absence of apertures, through which melted substances can issue, in that part of the continent, which stretches eastward of the Cordillera of the Andes, and eastward of the Rocky Mountains, is a most remarkable geological fact.
In this chapter we have examined the great commotions which from time to time convulse the stony crust of the globe, and scatter235 desolation in regions favoured by the most precious gifts of nature. An uninterrupted calm prevails in the upper atmosphere; but, to use an expression of Franklin, more ingenious than accurate, thunder often rolls in the subterranean atmosphere, amidst that mixture of elastic fluids, the impetuous movements of which are frequently felt at the surface of the earth. The destruction of so many populous236 cities presents a picture of the greatest calamities which afflict237 mankind. A people struggling for independence are suddenly exposed to the want of subsistence, and of all the necessaries of life. Famished238 and without shelter, the inhabitants are dispersed239 through the country, and numbers who have escaped from the ruin of their dwellings240 are swept away by disease. Far from strengthening mutual confidence among the citizens, the feeling of misfortune destroys it; physical calamities augment166 civil discord241; nor does the aspect of a country bathed in tears and blood appease the fury of the victorious242 party.
After the recital243 of so many calamities, the mind is soothed244 by turning to consolatory245 remembrances. When the great catastrophe of Caracas was known in the United States, the Congress, assembled at Washington, unanimously decreed that five ships laden246 with flour should be sent to the coast of Venezuela; their cargoes247 to be distributed among the most needy248 of the inhabitants. The generous contribution was received with the warmest gratitude249; and this solemn act of a free people, this mark of national interest, of which the advanced civilization of the Old World affords but few examples, seemed to be a valuable pledge of the mutual sympathy which ought for ever to unite the nations of North and South America.
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phenomena
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| n.现象 | |
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volcanic
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| adj.火山的；象火山的；由火山引起的 | |
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eruption
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| n.火山爆发；（战争等）爆发；（疾病等）发作 | |
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eruptions
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| n.喷发，爆发( eruption的名词复数 ) | |
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fissured
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| adj.裂缝的v.裂开( fissure的过去式和过去分词 ) | |
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retracing
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| v.折回( retrace的现在分词 )；回忆；回顾；追溯 | |
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inter
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| v.埋葬 | |
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vents
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| （气体、液体等进出的）孔、口( vent的名词复数 )； （鸟、鱼、爬行动物或小哺乳动物的）肛门； 大衣等的)衩口； 开衩 | |
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vent
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| n.通风口，排放口；开衩；vt.表达，发泄 | |
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commotions
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| n.混乱，喧闹，骚动( commotion的名词复数 ) | |
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commotion
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| n.骚动，动乱 | |
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modifications
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| n.缓和( modification的名词复数 )；限制；更改；改变 | |
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ardent
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| adj.热情的，热烈的，强烈的，烈性的 | |
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14
inveterate
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| adj.积习已深的，根深蒂固的 | |
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15
hatred
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| n.憎恶，憎恨，仇恨 | |
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16
calamities
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| n.灾祸，灾难( calamity的名词复数 )；不幸之事 | |
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17
shun
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| vt.避开，回避，避免 | |
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18
catastrophe
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| n.大灾难，大祸 | |
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19
intercourse
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| n.性交；交流，交往，交际 | |
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20
interrogate
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| vt.讯问，审问，盘问 | |
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21
catastrophes
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| n.灾祸( catastrophe的名词复数 )；灾难；不幸事件；困难 | |
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22
mutual
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| adj.相互的，彼此的；共同的，共有的 | |
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23
fixed
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| adj.固定的，不变的，准备好的；(计算机)固定的 | |
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24
memorable
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| adj.值得回忆的，难忘的，特别的，显著的 | |
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25
hesitation
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| n.犹豫，踌躇 | |
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26
celebrated
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| adj.有名的，声誉卓著的 | |
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27
elucidate
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| v.阐明，说明 | |
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28
dreaded
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| adj.令人畏惧的；害怕的v.害怕，恐惧，担心( dread的过去式和过去分词) | |
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29
dread
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| vt.担忧，忧虑；惧怕，不敢；n.担忧，畏惧 | |
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30
misty
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| adj.雾蒙蒙的，有雾的 | |
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31
temperate
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| adj.温和的，温带的，自我克制的，不过分的 | |
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32
incessantly
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| ad.不停地 | |
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33
inhaled
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| v.吸入( inhale的过去式和过去分词 ) | |
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34
agitated
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| adj.被鼓动的，不安的 | |
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35
agitate
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| vi.(for,against)煽动，鼓动；vt.搅动 | |
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36
overthrow
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| v.推翻，打倒，颠覆；n.推翻，瓦解，颠覆 | |
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37
slate
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| n.板岩，石板，石片，石板色，候选人名单；adj.暗蓝灰色的，含板岩的；vt.用石板覆盖，痛打，提名，预订 | |
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38
primitive
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| adj.原始的；简单的；n.原(始)人，原始事物 | |
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39
interval
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| n.间隔，间距；幕间休息，中场休息 | |
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40
intervals
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|
| n.[军事]间隔( interval的名词复数 )；间隔时间；[数学]区间；（戏剧、电影或音乐会的）幕间休息 | |
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41
situated
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| adj.坐落在...的，处于某种境地的 | |
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42
meridian
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| adj.子午线的；全盛期的 | |
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43
subterranean
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| adj.地下的，地表下的 | |
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44
fathoms
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| 英寻( fathom的名词复数 ) | |
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45
fathom
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| v.领悟，彻底了解 | |
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46
softened
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| （使）变软( soften的过去式和过去分词 )； 缓解打击； 缓和； 安慰 | |
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47
crater
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| n.火山口，弹坑 | |
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48
mere
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| adj.纯粹的；仅仅，只不过 | |
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49
recurrence
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| n.复发，反复，重现 | |
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50
elastic
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| n.橡皮圈，松紧带；adj.有弹性的；灵活的 | |
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51
latitudes
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| 纬度 | |
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52
latitude
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| n.纬度，行动或言论的自由(范围)，(pl.)地区 | |
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53
longitude
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| n.经线，经度 | |
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54
remarkable
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| adj.显著的，异常的，非凡的，值得注意的 | |
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55
elevation
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| n.高度；海拔；高地；上升；提高 | |
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56
circumscribed
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|
| adj.[医]局限的：受限制或限于有限空间的v.在…周围划线( circumscribe的过去式和过去分词 )；划定…范围；限制；限定 | |
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57
insular
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|
| adj.岛屿的，心胸狭窄的 | |
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58
proceeding
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| n.行动，进行，(pl.)会议录，学报 | |
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59
nay
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| adv.不；n.反对票，投反对票者 | |
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60
northward
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| adv.向北；n.北方的地区 | |
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61
precisely
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| adv.恰好，正好，精确地，细致地 | |
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62
serene
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| adj. 安详的，宁静的，平静的 | |
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63
standing
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| n.持续，地位；adj.永久的，不动的，直立的，不流动的 | |
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64
gulf
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| n.海湾；深渊，鸿沟；分歧，隔阂 | |
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65
elevations
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| （水平或数量）提高( elevation的名词复数 )； 高地； 海拔； 提升 | |
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66
simultaneously
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| adv.同时发生地，同时进行地 | |
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67
tar
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| n.柏油，焦油；vt.涂或浇柏油/焦油于 | |
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68
unreasonable
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| adj.不讲道理的，不合情理的，过度的 | |
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69
exempt
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| adj.免除的；v.使免除；n.免税者，被免除义务者 | |
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70
agitations
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| （液体等的）摇动( agitation的名词复数 )； 鼓动； 激烈争论； （情绪等的）纷乱 | |
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71
agitation
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| n.搅动；搅拌；鼓动，煽动 | |
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72
receding
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| v.逐渐远离( recede的现在分词 )；向后倾斜；自原处后退或避开别人的注视；尤指问题 | |
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73
remarkably
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| ad.不同寻常地，相当地 | |
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74
presage
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| n.预感，不祥感；v.预示 | |
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75
sufficiently
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| adv.足够地，充分地 | |
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76
toll
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|
| n.过路(桥)费；损失，伤亡人数；v.敲(钟) | |
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77
perpendicular
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|
| adj.垂直的，直立的；n.垂直线，垂直的位置 | |
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78
entirely
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| ad.全部地，完整地；完全地，彻底地 | |
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79
overthrown
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| adj. 打翻的，推倒的，倾覆的 动词overthrow的过去分词 | |
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80
naves
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| n.教堂正厅( nave的名词复数 )；本堂；中央部；车轮的中心部 | |
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81
vestiges
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| 残余部分( vestige的名词复数 )； 遗迹； 痕迹； 毫不 | |
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82
pastor
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| n.牧师，牧人 | |
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83
regiment
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| n.团，多数，管理；v.组织，编成团，统制 | |
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84
buttresses
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| n.扶壁，扶垛( buttress的名词复数 )v.用扶壁支撑，加固( buttress的第三人称单数 ) | |
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85
remains
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| n.剩余物，残留物；遗体，遗迹 | |
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86
computed
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| adj.[医]计算的，使用计算机的v.计算，估算( compute的过去式和过去分词 ) | |
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87
distress
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| n.苦恼，痛苦，不舒适；不幸；vt.使悲痛 | |
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88
domes
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| n.圆屋顶( dome的名词复数 )；像圆屋顶一样的东西；圆顶体育场 | |
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89
desolate
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|
| adj.荒凉的，荒芜的；孤独的，凄凉的；v.使荒芜，使孤寂 | |
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90
imploring
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| 恳求的，哀求的 | |
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91
miserable
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|
| adj.悲惨的，痛苦的；可怜的，糟糕的 | |
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92
groans
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| n.呻吟，叹息( groan的名词复数 )；呻吟般的声音v.呻吟( groan的第三人称单数 )；发牢骚；抱怨；受苦 | |
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93
implements
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| n.工具( implement的名词复数 )；家具；手段；[法律]履行（契约等）v.实现( implement的第三人称单数 )；执行；贯彻；使生效 | |
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94
invalids
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| 病人，残疾者( invalid的名词复数 ) | |
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95
cape
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| n.海角，岬；披肩，短披风 | |
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96
foliage
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| n.叶子，树叶，簇叶 | |
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97
linen
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| n.亚麻布，亚麻线，亚麻制品；adj.亚麻布制的，亚麻的 | |
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98
procure
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|
| vt.获得，取得，促成；vi.拉皮条 | |
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99
considerably
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| adv.极大地；相当大地；在很大程度上 | |
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100
swelled
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| 增强( swell的过去式和过去分词 )； 肿胀； （使）凸出； 充满（激情） | |
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101
vessels
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| n.血管( vessel的名词复数 )；船；容器；（具有特殊品质或接受特殊品质的）人 | |
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102
enjoined
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| v.命令( enjoin的过去式和过去分词 ) | |
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103
piety
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| n.虔诚，虔敬 | |
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104
commissioners
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| n.专员( commissioner的名词复数 )；长官；委员；政府部门的长官 | |
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105
ERECTED
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| adj. 直立的，竖立的，笔直的 vt. 使 ... 直立，建立 | |
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106
devoted
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| adj.忠诚的，忠实的，热心的，献身于...的 | |
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107
appease
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| v.安抚，缓和，平息，满足 | |
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108
wrath
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| n.愤怒，愤慨，暴怒 | |
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109
hymns
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| n.赞美诗，圣歌，颂歌( hymn的名词复数 ) | |
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110
distraction
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| n.精神涣散，精神不集中，消遣，娱乐 | |
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111
tract
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| n.传单，小册子，大片(土地或森林) | |
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112
confessions
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| n.承认( confession的名词复数 )；自首；声明；（向神父的）忏悔 | |
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113
benediction
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| n.祝福；恩赐 | |
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114
drawn
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| v.拖，拉，拔出；adj.憔悴的，紧张的 | |
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115
calamity
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| n.灾害，祸患，不幸事件 | |
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116
rendering
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| n.表现，描写 | |
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117
inhuman
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| adj.残忍的，不人道的，无人性的 | |
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118
benevolence
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| n.慈悲，捐助 | |
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119
disposition
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| n.性情，性格；意向，倾向；排列，部署 | |
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120
overthrew
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| overthrow的过去式 | |
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121
copper
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| n.铜；铜币；铜器；adj.铜(制)的；(紫)铜色的 | |
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122
proximity
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| n.接近，邻近 | |
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123
torrent
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| n.激流，洪流；爆发，(话语等的)连发 | |
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124
peculiar
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| adj.古怪的，异常的；特殊的，特有的 | |
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125
stony
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| adj.石头的，多石头的，冷酷的，无情的 | |
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126
strata
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| n.地层（复数）；社会阶层 | |
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127
villa
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| n.别墅，城郊小屋 | |
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128
geologists
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| 地质学家，地质学者( geologist的名词复数 ) | |
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129
crevice
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| n.(岩石、墙等)裂缝；缺口 | |
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130
crevices
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| n.（尤指岩石的）裂缝，缺口( crevice的名词复数 ) | |
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131
eastward
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| adv.向东；adj.向东的；n.东方，东部 | |
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132
formerly
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| adv.从前，以前 | |
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133
touching
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| adj.动人的，使人感伤的 | |
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134
affected
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| adj.不自然的，假装的 | |
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135
ridge
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| n.山脊；鼻梁；分水岭 | |
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136
inert
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| adj.无活动能力的，惰性的；迟钝的 | |
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137
tranquil
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| adj. 安静的, 宁静的, 稳定的, 不变的 | |
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138
justify
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| vt.证明…正当(或有理)，为…辩护 | |
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139
accomplished
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|
| adj.有才艺的；有造诣的；达到了的 | |
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140
heterogeneous
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| adj.庞杂的；异类的 | |
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141
limestone
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| n.石灰石 | |
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142
abruptly
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| adv.突然地，出其不意地 | |
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143
lava
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| n.熔岩，火山岩 | |
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144
fissures
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| n.狭长裂缝或裂隙( fissure的名词复数 )；裂伤；分歧；分裂v.裂开( fissure的第三人称单数 ) | |
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145
veins
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| n.纹理；矿脉( vein的名词复数 )；静脉；叶脉；纹理 | |
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146
vein
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| n.血管，静脉；叶脉，纹理；情绪；vt.使成脉络 | |
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147
partisans
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| 游击队员( partisan的名词复数 )； 党人； 党羽； 帮伙 | |
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148
lavas
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| n.（火山喷发的）熔岩( lava的名词复数 )；（熔岩冷凝后的）火山岩 | |
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149
granitic
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| 花岗石的，由花岗岩形成的 | |
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150
denomination
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| n.命名，取名，(度量衡、货币等的)单位 | |
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151
granite
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| adj.花岗岩，花岗石 | |
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152
slates
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| （旧时学生用以写字的）石板( slate的名词复数 )； 板岩； 石板瓦； 石板色 | |
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153
extremity
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| n.末端，尽头；尽力；终极；极度 | |
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154
apprehension
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| n.理解，领悟；逮捕，拘捕；忧虑 | |
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155
justified
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| a.正当的，有理的 | |
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156
cannon
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| n.大炮，火炮；飞机上的机关炮 | |
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157
artillery
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| n.(军)火炮，大炮；炮兵(部队) | |
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158
junction
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| n.连接，接合；交叉点，接合处，枢纽站 | |
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159
rekindled
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| v.使再燃( rekindle的过去式和过去分词 ) | |
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160
overflowed
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| 溢出的 | |
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161
brink
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| n.(悬崖、河流等的)边缘，边沿 | |
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162
worthy
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| adj.(of)值得的，配得上的；有价值的 | |
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163
detonations
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| n.爆炸 （声）( detonation的名词复数 ) | |
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164
resounded
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| v.（指声音等）回荡于某处( resound的过去式和过去分词 )；产生回响；（指某处）回荡着声音 | |
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165
inverse
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| adj.相反的，倒转的，反转的；n.相反之物；v.倒转 | |
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166
augment
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| vt.(使)增大，增加，增长，扩张 | |
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167
monks
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| n.修道士，僧侣( monk的名词复数 ) | |
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168
besieged
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| 包围，围困，围攻( besiege的过去式和过去分词 ) | |
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169
cone
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| n.圆锥体，圆锥形东西，球果 | |
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170
colossal
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| adj.异常的，庞大的 | |
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171
swollen
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| adj.肿大的，水涨的；v.使变大，肿胀 | |
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172
crest
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| n.顶点；饰章；羽冠；vt.达到顶点；vi.形成浪尖 | |
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173
obstructed
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| 阻塞( obstruct的过去式和过去分词 )； 堵塞； 阻碍； 阻止 | |
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174
craters
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| n.火山口( crater的名词复数 )；弹坑等 | |
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175
nautical
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| adj.海上的，航海的，船员的 | |
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176
lateral
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| adj.侧面的，旁边的 | |
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177
declivity
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| n.下坡，倾斜面 | |
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178
astonishment
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| n.惊奇，惊异 | |
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179
aperture
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| n.孔，隙，窄的缺口 | |
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180
apertures
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| n.孔( aperture的名词复数 )；隙缝；（照相机的）光圈；孔径 | |
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181
authenticated
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| v.证明是真实的、可靠的或有效的( authenticate的过去式和过去分词 )；鉴定，使生效 | |
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182
varied
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| adj.多样的，多变化的 | |
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183
marvels
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| n.奇迹( marvel的名词复数 )；令人惊奇的事物（或事例）；不平凡的成果；成就v.惊奇，对…感到惊奇( marvel的第三人称单数 ) | |
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184
isolated
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| adj.与世隔绝的 | |
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185
forth
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| adv.向前；向外，往外 | |
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186
isles
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| 岛( isle的名词复数 ) | |
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187
noted
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| adj.著名的，知名的 | |
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188
attentively
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| adv.聚精会神地；周到地；谛；凝神 | |
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189
previously
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| adv.以前，先前（地） | |
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190
expressively
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| ad.表示(某事物)地；表达地 | |
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191
domain
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| n.(活动等)领域，范围；领地，势力范围 | |
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192
myriads
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| n.无数，极大数量( myriad的名词复数 ) | |
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193
acting
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| n.演戏，行为，假装；adj.代理的，临时的，演出用的 | |
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194
incandescent
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| adj.遇热发光的， 白炽的，感情强烈的 | |
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195
thermal
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| adj.热的，由热造成的；保暖的 | |
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196
gust
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| n.阵风，突然一阵（雨、烟等），（感情的）迸发 | |
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197
emission
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| n.发出物，散发物；发出，散发 | |
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198
decided
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| adj.决定了的，坚决的；明显的，明确的 | |
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199
cursory
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| adj.粗略的；草率的；匆促的 | |
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200
Mediterranean
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| adj.地中海的；地中海沿岸的 | |
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201
rotation
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| n.旋转；循环，轮流 | |
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202
configuration
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| n.结构，布局，形态，(计算机)配置 | |
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203
cones
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| n.（人眼）圆锥细胞；圆锥体( cone的名词复数 )；球果；圆锥形东西；（盛冰淇淋的）锥形蛋卷筒 | |
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204
lesser
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| adj.次要的，较小的；adv.较小地，较少地 | |
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205
recollect
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| v.回忆，想起，记起，忆起，记得 | |
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206
elongated
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| v.延长，加长( elongate的过去式和过去分词 ) | |
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207
perfectly
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| adv.完美地，无可非议地，彻底地 | |
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208
granites
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| 花岗岩，花岗石( granite的名词复数 ) | |
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209
cataracts
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| n.大瀑布( cataract的名词复数 )；白内障 | |
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210
littoral
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| adj.海岸的；湖岸的；n.沿（海）岸地区 | |
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211
raffles
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| n.抽彩售物( raffle的名词复数 )v.以抽彩方式售（物）( raffle的第三人称单数 ) | |
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212
maritime
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| adj.海的，海事的，航海的，近海的，沿海的 | |
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213
impede
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| v.妨碍，阻碍，阻止 | |
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214
naturalist
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| n.博物学家(尤指直接观察动植物者) | |
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215
naturalists
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| n.博物学家( naturalist的名词复数 )；（文学艺术的）自然主义者 | |
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216
contiguity
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| n.邻近，接壤 | |
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217
essentially
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| adv.本质上，实质上，基本上 | |
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218
purely
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| adv.纯粹地，完全地 | |
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219
condensation
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| n.压缩，浓缩；凝结的水珠 | |
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220
misery
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| n.痛苦，苦恼，苦难；悲惨的境遇，贫苦 | |
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221
desolated
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| adj.荒凉的，荒废的 | |
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222
impel
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| v.推动；激励，迫使 | |
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223
dissertation
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| n.（博士学位）论文，学术演讲，专题论文 | |
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224
trifling
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| adj.微不足道的；没什么价值的 | |
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225
westward
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| n.西方，西部；adj.西方的，向西的；adv.向西 | |
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226
marsh
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| n.沼泽，湿地 | |
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227
unaware
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| a.不知道的，未意识到的 | |
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228
petroleum
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| n.原油，石油 | |
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229
alpine
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| adj.高山的；n.高山植物 | |
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230
gush
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| v.喷，涌；滔滔不绝(说话)；n.喷，涌流；迸发 | |
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231
viscous
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| adj.粘滞的，粘性的 | |
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232
igneous
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| adj.火的，火绒的 | |
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233
gushing
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| adj.迸出的；涌出的；喷出的；过分热情的v.喷，涌( gush的现在分词 )；滔滔不绝地说话 | |
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234
gaseous
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| adj.气体的，气态的 | |
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235
scatter
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| vt.撒，驱散，散开；散布/播；vi.分散，消散 | |
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236
populous
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| adj.人口稠密的，人口众多的 | |
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237
afflict
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| vt.使身体或精神受痛苦，折磨 | |
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238
famished
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| adj.饥饿的 | |
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239
dispersed
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| adj. 被驱散的, 被分散的, 散布的 | |
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240
dwellings
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| n.住处，处所( dwelling的名词复数 ) | |
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241
discord
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| n.不和，意见不合，争论，（音乐）不和谐 | |
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242
victorious
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| adj.胜利的，得胜的 | |
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243
recital
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| n.朗诵，独奏会，独唱会 | |
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244
soothed
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| v.安慰( soothe的过去式和过去分词 )；抚慰；使舒服；减轻痛苦 | |
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245
consolatory
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| adj.慰问的，可藉慰的 | |
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246
laden
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| adj.装满了的；充满了的；负了重担的；苦恼的 | |
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247
cargoes
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| n.（船或飞机装载的）货物( cargo的名词复数 )；大量，重负 | |
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248
needy
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| adj.贫穷的，贫困的，生活艰苦的 | |
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249
gratitude
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| adj.感激，感谢 | |
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