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art of his attention either to me or to the horses, preferring to concentrate it upon brandy, an article which can unfortunately be procured throughout the whole country. I had already seen the district between Reikjavik and Havenfiord at my first arrival in Iceland. At the present advanced season of the year it wore a less gloomy aspect: strawberry-plants and violets,--the former, however, without blossoms, and the latter inodorous,--were springing up between the blocks of lava, together with beautiful ferns eight or ten inches high. In spite of the trifling distance, I noticed, as a rule, that vegetation was here more luxuriant than at Reikjavik; for at the latter place I had found no strawberry-plants, and the violets were not yet in blossom. This difference in the vegetation is, I think, to be ascribed to the high walls of lava existing in great abundance round Havenfiord; they protect the tender plants and ferns from the piercing winds. I noticed that both the grass and the plants before mentioned throve capitally in the little hollows formed by masses of lava. A couple of miles beyond Havenfiord I saw the first birch-trees, which, however, did not exceed two or three feet in height, also some bilberry-plants. A number of little butterflies, all of one colour, and, as it seemed to me, of the same species, fluttered among the shrubs and plants. The manifold forms and varied outline of the lava-fields present a remarkable and really a marvellous appearance. Short as this journey is--for ten hours are amply sufficient for the trip to Krisuvik,--it presents innumerable features for contemplation. I could only gaze and wonder. I forgot every thing around me, felt neither cold nor storm, and let my horse pick his way as slowly as he chose, so that I had once almost become separated from my guide. One of the most considerable of the streams of lava lay in a spacious broad valley. The lava-stream itself, about two miles long, and of a considerable breadth, traversing the whole of the plain, seemed to have been called into existence by magic, as there was no mountain to be seen in the neighbourhood from which it could have emerged. It appeared to be the covering of an immense crater, formed, not of separate stones and blocks, but of a single and slightly porous mass of rock ten or twelve feet thick, broken here and there by clefts about a foot in breadth. Another, and a still larger valley, many miles in
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