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Ch. XIX.] LAKE OF MASAYA. 347

I spent the next day exploring around Masaya, as I was greatly interested with the geological structure of the country. One of the paths down to the lake has been made passable for animals, which have to be taken down to drink. I rode my horse down, but in the steepest part he slipped on to his side, and I was content to lead him the rest of the way. The scene was one which is only possible in a half-civilized tropical land. Women, with the scantiest of clothing, or less, were washing linen, standing up to their waist in the water amongst the rocks, on which they thumped the clothes to be cleansed, laughing and chatting to each other incessantly. Men with mules and horses were bathing themselves and their animals at a small sandy beach, and girls were carrying off great jars of water, which they obtained further down, where the water was less tainted with the ablutions going on. Great rocks, that had fallen from the cliffs above, lined the shore; and amongst these grew many shrubs and plants new to me. The cliffs themselves were, in some parts, green with lovely maiden-hair ferns, belonging to three different species.

On the opposite shore rises the cone of the volcano of Masaya, and the streams of lava that have flowed down to the lake and covered the old precipitous cliffs on that side are plainly visible. The cliff encircles the whole lake, excepting where concealed by the recent lava overflow. At the time of the conquest of Nicaragua, in 1522, the volcano of Masaya was in a state of activity. The credulous Spaniards believed the fiery, molten mass at the bottom of the crater to be liquid gold, and through great danger, amongst the Smoke and fumes, were

lowered down it until, with an iron chain and bucket, they could reach the fiery mass, when the bucket was melted from the chain, and the intrepid explorers, whose hearts avarice had hardened to adamant, were drawn up half dead from amongst the fumes. Since then there have been several eruptions; and so late as 1857 it threw out volumes of smoke, and probably ashes. The whole country is volcanic. For scores of miles every rock is trachytic, and the earth decomposing tufas. The lake itself is like an immense crater with its perpendicular cliffs. I spent some time in making an ac

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curate section of the strata as exposed in the rocky paths leading down to the water. The whole section exposed is 348 feet in height from the surface of the lake to the top of the undulating plain on which Masaya is built. This measurement was kindly given to me by Mr. Simpson, an enterprising American engineer engaged in

Ch. XIX.] LAKE OF MASAYA. 349

erecting a steam pump to raise the water for the supply of the town. At the bottom of this section are seen great cliffs of massive trachyte (No 1. in section). Above this is an ash bed, then a bed of breccia containing fragments of trachyte, then another bed of cinders, which looks like a rough sandstone, but is pisolitic, and contains pebbles of the size of a bean. This bed is surmounted by one that possesses great interest (No. 5 in section). It is composed of fine tufa, in which is imbedded a great number of large angular fragments of trachyte, some of which are more than three feet in diameter. It is the last bed but one, the surface being composed of lightly coherent strata of tufaceous ash, worn into an undulating surface by the action of the elements. I believe there is but one explanation possible of the origin of these strata; namely, that the great bed of trachyte at the base is an ancient lava bed; and that this, perhaps, long after it was consolidated, was covered by beds of ashes and scoriae thrown out by a not far distant volcano, and that at last a great convulsion broke through the trachyte bed and hurled the fragments over the country along with dense volumes of dust and ashes. The angular blocks of trachyte imbedded in the stratum No. 5 in section are exactly the same in composition as the great bed below, and in them. I think we see the fragments of the rocks that once filled the perpendicularsided hollow now occupied by the lake. Looking at the vast force required to hollow out the basin of the lake, by blasting out the whole contents into the air, distributing them over the country, so that they have not been piled up in a volcanic cone round the vent, but lie in comparatively level beds, I cannot expect that this explanation will be readily received; and I should not myself have advanced it if I could in any other way account for the phenomena. Fortunately, within historical times, there have been volcanic outbursts, not of such magnitude, certainly, as was required to excavate the basin of the lake of Masaya, but still of sufficient extent to show that such an origin is not beyond the limits of possibility. & Thus in the same line of volcanic energy, not far from the boundary line of the states of Nicaragua and San Salvador, there was an eruption of the volcano of Cosaguina, on the 20th of January, 1835, when dense volumes of dust and ashes, and fragments of rocks, were hurled up in the air and deposited over the country around. The vast quantity of material thrown out by this explosion may be gathered from the fact that one hundred and twenty miles away, near the volcano of San Miguel, the dust was so thick that it was quite dark from four o'clock in the evening until nearly noon of the next day; and even at that distance there was deposited a layer of fine ashes four inches deep. The noise of the explosion was heard at the city of Guatemala, four hundred miles to the westward, and at Jamaica, eight hundred miles to the north-east. In St. Vincent, in the West Indies, there was a great eruption on April 27th, 1812, which continued for three days, and was heard six hundred and thirty miles away on the llanos of Caraccas. This great eruption has been so graphically narrated by Canon Kingsley that I shall once more quote from his eloquent pages. “That single explosion relieved an interior pressure upon the crust of the earth which had agitated sea and land from the

Ch. XIX.] GREAT EARTHQUAKE. 351

Azores to the West Indian islands, the coasts of Venezuela, the Cordillera of New Granada, and the valleys of the Mississippi and Ohio. For nearly two years the earthquakes had continued, when they culminated in one great tragedy, which should be read at length in the pages of Humboldt. On March 26th, 1812, when the people of Caraccas were assembled in the churches, beneath a still and blazing sky, one minute of earthquake sufficed to bury, amid the ruins of churches and houses, nearly ten thousand souls. The same earthquake wrought terrible destruction along the whole line of the northern Cordilleras, and was felt even at Santa Fé de Bogota and Honda, one hundred and eighty leagues from Caraccas. But the end was not yet. While the wretched survivors of Caraccas were dying of fever and starvation, and wandering inland to escape from ever-renewed earthquake shocks, among villages and farms which, ruined like their own city, could give them no shelter, the almost forgotten volcano of St. Vincent was muttering in suppressed wrath. It had thrown out no lava since 1718, if, at least, the eruption spoken of by Moreau de Jonnés took place in the Souffrière. According to him, with a terrific earthquake, clouds of ashes were driven into the air, with violent detonations from a mountain situated at the eastern end of the island. When the eruption had ceased, it was found that the whole mountain had disappeared. Now there is no eastern end to St. Vincent nor any mountain on the east coast, and the Souffrière is at the northern end. It is impossible, meanwhile, that the wreck of such a mountain should not have left traces visible and notorious to this day. May not the truth be, that the Souffrière had once

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