June 28.

Steamed out at seven A.M. under Italian skies, and over seas smooth as mirrors, which promised ample enjoyment of this day’s “lion,” Snæfellsjökull, capping the northern land-arm of broad Faxa Fjörð. As we crossed the Hvalfjörð-mouth, the lay of the land suggested a mighty leaf; the water-line being the midrib, with Esja and Akranes representing the up-turned sides. On the south-western slopes of Skarðsheiði, we were shown the streamlet and farm of Leirá, “Rivière de la Vase,” which once owned the printing-press; and beyond the broad Borgarfjörð (burg firth)[59] lay the low alluvial flat Mýra Sýsla. The unromantic name, “mire county,” becomes ridiculous when Mýra-maður (mud-man) is applied to the dweller: the comical wrath which it excites reminded me of Varnhagen’s indignation about the Corcovado or Hunch-back mountain of Rio de Janeiro. Far over the fen-tract, streaked by its three main streams, appeared a suggestive prospect: the long perspective of Jökulls; Ok (the yoke), Geitland’s and the northern Skjaldbreið, not to be confounded with the “Broad Shield” on the road to Hekla: this chaos of ice-deserts and volcanoes was ranged in long dorsa, dish-covers, or antediluvian Twelfth-cakes, flattened at the summit, backed by pearly mists of their own growing, with crests rose-tinged by the sun, and feet streaked with transparent blue shadows. In vain we strained our eyes to catch a sight of Baula, the cow, pronounced somewhat like (the land of) “Beulah;” its pale-grey trachytic columns, though 3000 to 3500 feet high, were hidden by intervening buttresses: even Eld-borg, the “Tower of Fire,” though quite near the coast, refused to show its grand circular crater and flanks too steep for snow. Here begins the northern Skarðsheiði, which, passing through the Hnappadals (button-dale) Sýsla, anastomoses with the broken cones called Katlar (the caldrons), and with the great Snæfellsjökull, the Snebels Hokell of Pontanus, and the “Western Jökull” of our maps. The long thin tongue of land, mostly trachytic, has been mightily exercised by the fire below. Here, upon a naked Tenerife, rises a tall grey cone, fronted by a little extinct volcano, flushing angry red; there a wall of brown lava is built upon a base of ruddy cinders and scoriæ, which have assumed the natural angle. It is a land of chimneys and spiracles rising from cinders and other rejectamenta; of Öl-keldr or “ale” (mineral) “waters;” of cascades, silver fibres dashing into kieves of snow; of jagged sugar-loaves and saddle-backs; of craters either whole or half torn away; and of Klettar or precipices stripped of the snows which encompass them.

Our attention was directed to the Búða-klettar, or cliffs of Buðir, the celebrated centre of eruption which sent forth the Búðarhraun; and at their base, ending the Jökullháls, the long ochraceous slope that falls from the eastern ridge-flank of Snæfell to the settlement of Búðir (the booths), far-famed for chalybeate springs. Huts for invalids have been run up at this well-known “Kur-ort,” but the accommodation is described as rough in the extreme. A little westward again, showing its basaltic pillars, lies “Stapi,” the steeple-formed rock, a local Staffa, suggesting memories of Fin M’Coul.

All eyes now fix themselves upon Snæfellsjökull: as the break of the sea upon the shore told us, it rises within three miles, and the accidents of weather, though apparently determined to conceal the calotte of snow, combine to form an admir-

R. F. B. delt.

SNÆFELLSJÖKULL FROM THE SOUTH.

able setting for the imposing scene. The clearness of the heavens had gradually changed to light mists, which hung mid-way upon the hill-sides: whilst “mackerel’s-back” flecks the upper air, woolpack, growing from the snow wreaths, forms dark-grey columns, perfectly simulating a burning coast, and puffy white cumuli cast a shadow distinct as if drawn by a painter’s hand. About one P.M. the northern breeze becomes a south-easter, bringing with it a decided freshness and a few drops of rain. The brown and dun coloured cirri, before floating high above the wool-pack, now girth its middle, and there is a grand contrast between the here and the there. Around us a few cats’-paws fan the waters, which, under the lee of the land, stretch smooth as oil, and the air is mild and kindly. In the upper regions rages and roars “Satan’s weather;” the cloud chariots rush forward in solid line against the wind, dashing and clashing as they course and career over the battlefield of virgin snow; they are torn to pieces by the artillery of the Storm-Fiend; the troops whirl away in headlong flight, veiling now one cusp of the crater, then another. The westerly peak is connected by a deeply-gashed synclinal slope, a kind of broken saddle-back, with the eastern horn, or rather horns, which appear in the shape of a “Thríhyrningr,” while below them, on the oriental outline, a star of jetty basalt shines radiant in the dazzling white. Below the western peak also the binoculars show a broken quoin, a long, black dyke, and a multitude of dark dots protruding from the névé, as if men were ascending. The apex has never been reached, and we at once see the reason why: it is—