The Danish History, Books I-IX by Grammaticus Saxo
page 90 of 493 (18%)
page 90 of 493 (18%)
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it and drenched with its reeking fume, nought but the shape surviving.
Here also are said to be other springs, which now are fed with floods of rising water, and, overflowing in full channels, cast a mass of spray upwards; and now again their bubbling flags, and they can scarce be seen below at the bottom, and are swallowed into deep hiding far under ground. Hence, when they are gushing over, they bespatter everything about them with the white spume, but when they are spent the sharpest eye cannot discern them. In this island there is likewise a mountain, whose floods of incessant fire make it look like a glowing rock, and which, by belching out flames, keeps its crest in an everlasting blaze. This thing awakens our wonder as much as those aforesaid; namely, when a land lying close to the extreme of cold can have such abundance of matter to keep up the heat, as to furnish eternal fires with unseen fuel, and supply an endless provocative to feed the burning. To this isle also, at fixed and appointed seasons, there drifts a boundless mass of ice, and when it approaches and begins to dash upon the rugged reefs, then, just as if the cliffs rang reply, there is heard from the deep a roar of voices and a changing din of extraordinary clamour. Whence it is supposed that spirits, doomed to torture for the iniquity of their guilty life, do here pay, by that bitter cold, the penalty of their sins. And so any portion of this mass that is cut off when the aforesaid ice breaks away from the land, soon slips its bonds and bars, though it be made fast with ever so great joins and knots. The mind stands dazed in wonder, that a thing which is covered with bolts past picking, and shut in by manifold and intricate barriers, should so depart after that mass whereof it was a portion, as by its enforced and inevitable flight to baffle the wariest watching. There also, set among the ridges and crags of the mountains, is another kind of ice which is known periodically to change and in a way reverse its position, the upper parts sinking to the bottom, and the lower again returning to the top. |
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