“Like a jagged shell’s lips, harsh, untunable;
Blown in upon by devils’ wrangling breath.”
M. Gaimard declares the eastern pinnacle to be “frisée comme des têtes de choux-fleurs:” it appeared to me umbrella-shaped, with under ribbings of frozen snow. M. Jules Verne was not so happy as usual in making “Sneffles” an entrance for Arne “Saknussemm;” nor could we learn anything about “Scortaris.”
The southern front below the névé is a steep incline of contorted lava; and a multitude of “hornitos” and parasitic craters, apparently fallen in or choked up, run down almost to the water’s edge, where they form a wall of contorted and caverned layers. Above the cliff a gentler slope has a faint tinge of rainbow-green; and the steeper acclivities are bare, red and yellow, brown and black. As we hugged the shore, I carefully looked for the snow-drainage, and saw none: had there been any, the sea-scaur must have shown it. Henderson rightly reports the general belief that the water set free by the sun passes by underground tunnels to the sea; and, all along this peninsula, the people hold to subterranean connections. But the explanation somewhat savours of the Congo Yellala (rapids), where the mighty mass of the upper stream, “above the ghauts,” is supposed to pass through an invisible channel. Herðubreið afterwards taught me that Palagonite allows no surface drainage in the dry season; and this I hold to be the true explanation of a remarkable phenomenon often seen in Iceland.
So striking a feature as Snæfell, whose shadow may be traced in the air, could not fail to engender a variety of tales and legends. Some declare, with the old Sagas, that it is within sight of Hvítserk in Eastern Greenland. Certes its height (4577 Danish feet) is very far from affording a vision ranging over 200 direct geographical miles; but here we are little more than a degree from the Arctic circle, and it is hard to limit the magic powers of refraction.[60] When the bishop declared that it was unassailable by reason of “Dominus Bardus Snæfellsás, cujus sine auspiciis mons Snæfell vix, ac ne vix quidem, superari potest,” he alluded to a superstition still preserved. In Hitárdalr,[61] farther east, is shown a huge feminine face carved in stone, and said to represent Hít, the Ás or guardian goddess of the dale: a “Plutonic affection” exists between her and Bárð or Snæfell’s Ás, whom Mackenzie calls a tutelar saint, and whom Charles Forbes uncivilly converts from Dominus to demon. He represents right well the Spirit of the Glacier. Curious to say, the same tale concerning the “Loves of the Mountains” is told in far New Zealand, where Messrs Tongariro and Taranaki (Mount Egmont) are jealous as they are amorous of Mrs or Miss Taupo.
The earliest climbers seem to have attempted the ascent from the east and south-east, where the snow-line extends much lower. Such were Eggert Ólafsson (1755); Mr, afterwards Sir, John Stanley (1789); and the three Britishers who “wrote their mistresses’ names in the snow—the emblem of their purity.” Sir George Mackenzie (1810) remained below, and Drs Bright and Holland went stoutly up: the latter tells us (p. 55, Recollections of a Fast Life) that a snow bridge gave way during the descent, and one leg sank through the arch: he was saved by the poles of the two Iceland guides, but ever after he sought to shun the remembrance. They were followed by Henderson (1814), by Gaimard (1835), and by Forbes (1859).
Of course, none reached the very summit. The Frenchman sensibly attempted it from the north, and found the slope easy: we shall presently see his line of march. Remains only to try the west where the snow lies much higher up, and where the angle does not apparently exceed 25°: here also the distance to the cusps or peaks is notably shorter. The Beruvík farm appears to be a good starting-place. But Alpines who love “climbing for climb” must remember that without ropes and ladders, perhaps kites also, and very likely with them, it will be impossible to do more than has been done by their predecessors.
The accidents of the shore-line preserve their interest: the lone rock Göltr (the deer)[62] and the twin Lón-drángar (sea-inlet drongs), donjons of lava 240 feet tall, the north-western appearing as if standing inland, where a red rock acts castle. Beyond it, amongst the conical and degraded craters, we remark the Tröllakyrkja, Kirk of the Trolls, or Giants, who here have a diocesan as well as a governor. They have been busy on and off this coast, as shown by the Trölla-botn, Giant Bay, the Polar Sea between Norway and Greenland; the Trölla-börn (chimneys), or volcanic “hornitos;” the Trölla-hlað, the Giant’s Causeway, or colonnade of basalt; and the Trölla-dyngjur, or Giantesses’ bowers, the mamelons near Reykjanes, which erupted in A.D. 1000. And that the dwarfs have not been idle we see by the Dverga Kamarr, their hollowed chambers in the basalt. We run by Dritvík (guano bay), along the caverned cliff, built in various layers, here frosted like silver, there dotted with white points, which prove to be birds. At Öndverðarnes (fronting naze), after an hour of thorough enjoyment, thanks to Dominus Barðr, we turn the corner, the north-westernmost projection of Snæfellsjökull, which the pilot calls Svarta-lot, from the steps protruded by the swart sea-wall; we open the Breiði Fjörð, and again we find waters smooth as a silver plate.
Not that Broad Firth is always so well behaved: at times he rages with frantic violence, mixing sea and sky till the general view is like a well-shaken basin of soup, and confusing all the elements in a chaotic matter, which justifies the much-maligned Pytheas. Many have been drowned when crossing the dangerous sea, amongst them Ólafsson, the Icelandic traveller, in 1767; shortly after he had “addicted himself to the study of revealed religion.” During the winter of 1873-74, it was completely invested by the Greenland ice; congelation extended as far as the eye could reach from the highest hill-tops; and drifted bears were slaughtered by the peasantry. There are traditions of skating across the broad bay, of seals being killed, and of ships’ anchors being blown away by the furious wind. At least, so says Mr Clausen, who has now taken us in charge. The grandson of a Danish merchant mentioned by Henderson, he has married a wife from Bonnie Dundee, and he has spent some four years at Melbourne, which have opened his eyes to auriferous quartz-reefs, to large deposits of iron, and to other minerals in his native island.
We delay for a while at the mouth of the big bay to swing the ship and prove her compasses, a precaution never to be neglected. The “Jón” then runs at a respectful distance along the northern shore of the Snæfellsjökull tongue, which is not less interesting than its southern coast. Our cicerone points out Enni or Ennisfjall, “forehead mountain,” la montagne de front,[63] where those who would avoid a long detour inland must pass over an Úfæra or “don’t travel” path—sands liable to frequent bombardments from the red bluff 2500 feet high. Henderson tells the exaggerated tale of its horrors, quaintly wondering how they were not felt by the young girls who rode with him. Mr Clausen then introduces to us Ólafsvík, his ancestral home, two slate-roofed houses, with surrounding huts, nestling in a sheltered bay; and, by way of urging his hospitality, he nobly makes us “free of the cellar.”