Letters From High Latitudes By Lord Dufferin















































































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Two days afterwards a stream of lava, issuing from sources
to which no one has ever been able to penetrate - Page 42
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Two Days Afterwards A Stream Of Lava, Issuing From Sources To Which No One Has Ever Been Able To Penetrate,

Came sliding down the bed of the dried-up river, and in a little time, - though the channel was six

Hundred feet deep and two hundred broad, - the glowing deluge overflowed its banks, crossed the low country of Medalland, ripping the turf up before it like a table-cloth, and poured into a great lake whose affrighted waters flew hissing and screaming into the air at the approach of the fiery intruder. Within a few more days the basin of the lake itself was completely filled, and having separated into two streams, the unexhausted torrent again recommenced its march; in one direction overflowing soiree ancient lava fields, - in the other, re-entering the channel of the Skapta, and leaping down the lofty cataract of Stapafoss. But this was not all; while one lava flood had chosen the Skapta for its bed, another, descending in a different direction, was working like ruin within and on either side the banks of the Hverfisfliot, rushing into the plain, by all accounts, with even greater fury and velocity. Whether the two issued from the same crater it is impossible to say, as the sources of both were far away within the heart of the unapproachable desert, and even the extent of the lava flow can only be measured from the spot where it entered the inhabited districts. The stream which flowed down Skapta is calculated to be about fifty miles in length by twelve or fifteen at its greatest breadth; that which rolled down the Hverfisfliot, at forty miles in length by seven in breadth. Where it was imprisoned, between the high banks of Skapta, the lava is five or six hundred feet thick; but as soon as it spread out into the plain its depth never exceeded one hundred feet. The eruption of sand, ashes, pumice, and lava, continued till the end of August, when the Plutonic drama concluded with a violent earthquake.

For a whole year a canopy of cinder-laden cloud hung over the island. Sand and ashes irretrievably overwhelmed thousands of acres of fertile pasturage. The Faroe islands, the Shetlands, and the Orkneys were deluged with volcanic dust, which perceptibly contaminated even the pure skies of England and Holland. Mephitic vapours tainted the atmosphere of the entire island; - even the grass, which no cinder rain had stifled, completely withered up; the fish perished in the poisoned sea. A murrain broke out among the cattle, and a disease resembling scurvy attacked the inhabitants themselves. Stephenson has calculated that 9,000 men, 28,000 horses, 11,000 cattle, 190,000 sheep, died from the effects of this one eruption. The most moderate calculation puts the number of human deaths at upwards of 1,300; and of cattle, etc. at about 156,000.

The whole of this century had proved most fatal to the unfortunate people of Iceland. At its commencement smallpox destroyed more than 16,000 persons; nearly 20,000 more perished by a famine consequent on a succession of inclement seasons; while from time to time the southern coasts were considerably depopulated by the incursions of English and even Algerine pirates.

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