A Visit To Iceland And The Scandinavian North By Madame Ida Pfeiffer































































































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The higher mountains to the left fade gradually more and more from
view; but the river Elvas spreads in such - Page 95
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The Higher Mountains To The Left Fade Gradually More And More From View; But The River Elvas Spreads In Such A Manner, And Divides Into So Many Branches, That One Might Mistake It For A Lake With Many Islands.

It flows into the neighbouring sea, whose expanse becomes visible after surmounting a few more small hills.

The vale of Reikum, which we now entered, is, like that of Reikholt, rich in hot springs, which are congregated partly in the plain, partly on or behind the hills, in a circumference of between two and three miles.

When we had reached the village of Reikum I sent my effects at once to the little church, took a guide, and proceeded to the boiling springs. I found very many, but only two remarkable ones; these, however, belong to the most noteworthy of their kind. The one is called the little Geyser, the other the Bogensprung.

The little Geyser has an inner basin of about three feet diameter. The water boils violently at a depth of from two to three feet, and remains within its bounds till it begins to spout, when it projects a beautiful voluminous steam of from 20 to 30 feet high.

At half-past eight in the evening I had the good fortune to see one of these eruptions, and needed not, as I had done at the great Geyser, to bivouac near it for days and nights. The eruption lasted some time, and was tolerably equable; only sometimes the column of water sank a little, to rise to its former height with renewed force. After forty minutes it fell quite down into the basin again. The stones we threw in, it rejected at once, or in a few seconds, shivered into pieces, to a height of about 12 to 15 feet. Its bulk must have been 1 to 1.5 feet in diameter. My guide assured me that this spring generally plays only twice, rarely thrice, in twenty- four hours, and not, as I have seen it stated, every six minutes. I remained near it till midnight, but saw no other eruption.

This spring very much resembles the Strukker near the great Geyser, the only difference being that the water sinks much lower in the latter.

The second of the two remarkable springs, the arched spring, is situated near the little Geyser, on the declivity of a hill. I had never seen such a curious formation for the bed of a spring as this is. It has no basin, but lies half open at your feet, in a little grotto, which is separated into various cavities and holes, and which is half-surrounded by a wall of rock bending over it slightly at a height of about 2 feet, and then rises 10 to 12 feet higher. This spring never is at rest more than a minute; then it begins to rise and boil quickly, and emits a voluminous column, which, striking against the projecting rock, is flattened by it, and rises thence like an arched fan.

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