Chapter IX: Section II: To Hekla, and Up It

The next morning’s work began with a path which introduced us to the mud-bog, as opposed to the turf-bog. This pleasant feature led to lava, whose three main torrents and many secondary streamlets could be seen spilling over the trap wall of Lángahlíð. There were the two normal kinds, the soft and cindery, caverned and friable, which makes good paths: it degrades to the dark red and yellow-red humus which is here, as in the Haurán, the general colour of the ground. This variety is clad with two lichens; the grey with black scutella (_L. calcareus?_), and the pure white (_L. Tartareus?_) which makes the ejections of the Safá near Damascus simulate limestone. The other is intensely hard, ruddy black or brown-grey, and in places solid as if poured out yesterday; the reason generally given is the presence of olivine in this trachytic or silicious form. M. Durocher’s theory is, that being lighter than the doleritic and augitic (basic), it therefore floats separately, and thus he would explain how lava floods of different composition may proceed from the same locality.[93] The plications of this hard lava, looking as if hogs-heads of honey had been poured upon stone, the domes and the drops, not to speak of the sharp-toothed mouths and crevasses, make the traveller suffer for the sufferings of his nag.

At the end of the first great lava-stream was the farm of Herdísarvík; now not a “vik” but a “vatn”--we looked around for sulphur, but in vain. Hard by our right the fierce seas burst and roared upon a coast cruel and harbourless as that of Kafir-land; whilst in the smooth distance a few catspaws suggested shoaly islets. The Hlíðarvatn (lithe or slope water) is not like its neighbour a misnomer, but the supply is brackish, ebbing and flowing with the tide, like wells in the valley of the Thames. The only birds seen were wild geese, crees, gulls, curlews, young snipes, and ravens which especially affect this warm part of the island. During the halt we especially noticed a number of web-less hunting spiders, whose little nests were full of young--the peasants still preserve the old Köngur-váfa (web-weaver) which the citizens hold obsolete, preferring Könguló or Konguló. There are spider-stories, too, like the Gold Coast “Anansesem;” a small red species, for instance, kills when it bites.

From Litlaland, which we reached whilst the sun was still high, we enjoyed a pleasant view. Beyond the rise of Thorlakshöfn lie the “Irish Islands,” tall and picturesque, fronted by the great alluvial plain of south-western Iceland. It has been called Tempe, Arcadia, and Vale of Enna, though utterly unlike the grim defile of Peneus, the stern limestone mounts of the Peloponnesus, and the waterless slopes of Sicily. The “Pastorale in A flat,” as Thomas Hood, sen., would have called it, a raw northern facsimile of the Lagos Lagoon, as it appeared to me, gains dignity by the eastern background of eternal snows, the flat top of Eyjafjall, the long ridge of Tindafjall, and the sharp point of Torfajökull. And it is “classic ground.” From a commanding site we can prospect Ingolfsfjall, where Iceland’s first settler is supposed to be buried, and the Bergthórshvoll farm in the delta of the Markarfljót; behind it lies Hlíðarendi, where the “peerless Gunnar” sleeps in the Tverá Holm.[94]

There is--for Iceland--rare pathos in this description of the hero’s tomb.

“They cast a cairn over Gunnar, and made him sit upright in the
cairn.”

“He sang in the cairn which opened, and he turned himself and
looked at the moon, which was shining clear and bright. And men
thought they saw four lights burning in the cairn, and none of them
cast a shadow. He sang a song, after which the cairn was shut up
again.”

The next morning led us to Reykir. As we rode up the valley of the Ölfusá we could mark the features of the scene. In front the river was a lake, and the green expanse of the water-veined delta was scattered over with south-facing farms, not acknowledged by Gunnlaugsson and Olsen. Eyrarbakki, so called from the host of islets which line the shore, is the only port till Berufjörð on the eastern coast, and it was wholly occupied by two ships. Mr William Hogarth of Aberdeen, who owned the establishment, has not been here, we were told, for years; lately, however, some English visitors had excellent fishing in the river, and were hospitably entertained by Hr Thorgrimsson, agent to M. Lefolii, a Danish merchant. All this greenery was set off by the barrenness of the buttressed Lángahlíð hard on our left. The regular horizon of trap-wall had been succeeded by a sharp slope of Palagonite conglomerate, which evidently underlies the whole block. On the summit is a desert where no man dwells, broken by pyramids which are evidently lava-cones, Skálafell (scald or bald hill?) being the chief feature; upon the lips of the plateau are gushes of modern lava, and on the low levels appears an ancient sea-beach, scattered with rounded blocks like giant rocs’ eggs.

“Hjalli,” which we reached about noon, was somewhat peculiar--instead of being a single farm, four establishments clustered round the black chapel. It had its rivulet where the girls comb their yellow hair o’ mornings; the Lavapés (wash-feet) of the Brazilian country town; it had also its Paradís, a poetical name for the grassy combe, where men bask i’ the sun. The males were clad in pastoral attire, the old native dress deemed somewhat too _marqué_ for town and comptoir. The chief items are a shirt, a waistcoat, and a tight, very tight, flannel culotte, braccæ gartered below the knee and ending in stockings and Iceland shoes. The stranger’s first impression is that harlequin, without his spangles, has forgotten his overalls. This primitive toilette of the non-Roman races,[95] which gave birth to our civilised attire, still lingers in parts of Europe, notably in the Cicería of Istria, where the charcoal-burners (Cici) will adopt no other costume. And what can be more ridiculous than the Hungarian footsoldier wearing his drawers, when we know the wide Turkish Shalwar to be his national terminations?

“Reykir!”[96] ejaculated Páll, pointing triumphantly to a little yellow splotch on the far side of the broad valley. As we progressed towards the Reeks, we found the forage improving, and the soil becoming damper; this is commonly the case, because the western frontage enjoys the most sun. Of five springs clustered upon either bank of the little Varmá, the largest lies on the left, where Palagonite breccia forms the base of a ruddy spine, projected by the northern outliers of the Ingolfsfjall _massif_. The usual motley colours of a solfatara are set off by a more brilliant green than usual, and by a silver-tinted moss (_Trichostomum canescens_), which makes the turf-carpet feel soft as velvet.

Reykir is known as the Litlé Geysir, or “the Geysir in Ölfus.” In 1770 Uno Von Troil declared that it used to rise sixty to seventy perpendicular feet, in fact, as high as the Great Geysir of 1872, but that an earthquake, after cutting off a few feet (fifty-four to sixty), made it spout sideways. Nothing can be meaner than the modern display, and my companion compared it disadvantageously with that “furious fountain” of the guidebooks, the Sprudel of Carlsbad. The chief well to the north has built for itself a party-coloured mound like a nest of African termites, and puffs only vapour with the sumph of a donkey-engine. A hundred yards or so to the south is a younger spring with double boilers, in which the water may rise at times a foot and a half high: the “hell broth” slithers through a soft and soppy circle, down a foul channel of burnt pyrites and silica-clothed trap to the bubbling Varmá. This stream shows from a height, three branches draining from the north-west, where are other sulphur springs.

A whole generation of travellers has complained of the farmer of Beykir, who is said to have charged one man $52 per diem. We can only speak of him as we found him; his demand for forage was extremely moderate, and we attributed the fact to having an honest and thrifty guide.

A swampy ride in the afternoon led to the ferry of the Ölfusá or lower Hvitá. The ground was spangled with Fífa or cotton grass (_Eriophorum_), a weed with a bad name. It is more common here than in the southern islands, Scotland, and Germany, and it is supposed to haunt the worst and most dangerous bogs, where water sinks instead of flowing. “Avoid cotton grass ground” is the advice of every traveller: unfortunately you cannot, and you must make the best of it. But why call it the “treacherous cotton grass,” when it at once tells you the worst? On the other hand, buck-bean (Hor-blaka, or _Menyanthes trifoliata_) is praised because it shows the surface to be safe.

After three hours we reached the ferry, a busy scene for Iceland. Caravans charged with imported boards and fish to be exported, lay unloaded on either bank. Amongst the travellers was the Bishop of Iceland with a party of six; he had ridden from Reykjavik to Reykir in nine hours, and as he sat waterproof’d in the sun, he complained sadly of fatigue. A couple of two-oared boats, big and small, with a third high and dry, did not tend to expedite transit--nothing would be easier than to establish a wire rope and a ferry with lee-boards, thus making the current do all the work.

Rain threatened, and we lodged, as Abyssinians might lodge, in the church of Laugadælir, after duly admiring the farmer’s _chef d’œuvre_, a brass chandelier. All was very grotesque; the Psalms were chalked up on the wall, a Mambrino’s helmet acted font, and the altar-piece showed bow-legged Mattheus, with Marcus, Lucus, and Johannes to match. Around the fane lay the churchyard, where the peasant

“lies at peace with all his humble race,
And has no stone to mark his burial-place.”

It was the usual reverse of gardenesque or picturesque. Sheep grazed upon the weeds that “had no business there,” and the railings were utilised for drying socks and small-clothes.

The fourth march proved peculiarly unpleasant. When the weather is bad at Reykjavik, here it is detestable. The display of water-works seemed the effort of the old Polynesian giants, who submerged the greater part of earth--Terrible-rain, Long-continued-rain, Fierce-hailstorm, and their progeny, Mist, Heavy-dew, and Light-dew. In plain English it was a “jolly wet day.” The horses very sensibly bolted up stream, and refused to be caught till noon, when the men returned dripping as loons or roaches. The delta of the two great streams is said to be, in fine weather, one of the fairest pastoral scenes the island can show; but we saw it at its worst, sadly deformed, and we gathered practical experience of what a few hours of downfall can do in this semi-saturated region. The paths were “dead,” or rather, they were shown only by lines of puddle; the sloughs and quagmires admitted our ponies to the hocks; the drains overflowed like little hill-races, and the labour of rounding the deeper fens was immense. A few peaks which lay but a little distance to the north seemed immeasurably removed, like

“Far-off mountains turnèd into clouds.”

About mid-afternoon we came upon the Thjórsá, “fluviorum rex Eridanus” of Iceland: even at this upper part it looked like an estuary, split by sandbars, piles of basalt, sandbars and basalt again. We pushed hard over the few good places; and moist, mouldy, and malcontent, we were right glad to find ourselves in the strangers’ room of the ferryman’s house: 20 feet long by 14 broad and 7 high: dated 1848, it was an _omnium gatherum_ of the family goods, and it boasted of one four-paned window, which has never opened, and which never will. The features denoting wealth were huge wooden lockers, like seamen’s chests, of bright colours, painted with flowers and arabesques of still brighter tints: I could not but remember the pea-green and gamboge box which carried to Meccah the drugs of a certain “Haji Abdullah.” The soiree ended with a distressing banality. Fair visions of girls who kiss the stranger on the mouth, who relieve him of his terminal garments, and who place a brandy bottle under his pillow, and a bowl of milk or cream by his side, where are ye? Icelanders have allowed their pleasant primitive fashions to be laughed away by the jeering stranger, who little thought how much the custom told in favour of the hosts. The _naïve_ modesty of antiquity, when Nestor’s youngest daughter laved, anointed, and dressed Telemachus, and when the maids of Penelope had a less pleasant task with the elderly Ulysses, has departed with the public bathings, in angelic attire, of Iceland, of Sind, and of Japan, and the kiss given to the guest by the young wife or the eldest daughter of the Morlacchi house. This _sublime impudeur_ was possible only amongst a pure race: the sneers of a single civilised savage suffice to demolish this “_heureuse absence du ‘schoking.’_”

Next morning, while the horses were grazing, we ascertained that the farm had its therma: a jet of steam issuing from the ground near the river had been turfed over, with room to stand; and thus a Turkish, or rather a Russian, bath was possible on bath-day. We then walked down to the Thjórsá, an especially grisly spectacle. Its breadth, 250 yards, was occupied by white glacier water, with a sulphury tinge, rendered more ghastly by the black sand, rocks, and islets studding the bed above and below the ferry. The right bank showed a wall of conglomerate, and on both sides “cachociras” dashing over the stones gave pleasant reminiscences of San Francisco. The left bank is of Hekla lava, either compact or very porous containing crystals of lime. We found a natural hatchet and quantities of pumice, many-coloured, but mostly yellow: it floats in water, and it is useful for holystoning the skin. The velocity was three knots, and the temperature 52° (F). The ferry creeps up from the stone-head acting pier on the right bank, swings across below the break, and lands you in water on the far side.

The conduct of ponies at the ferry is always amusing. They are driven in by the shouts of lads and lasses, by tossings and wavings of the arms, by sticks and stones, and by the barking and biting of curs. They sidle, jostle, step in daintily, smell the water, and, after trembling on the brink for a time, some plucky little nag takes the lead. He is followed by the ruck, but there are often cowards ready to hark back: these must be forced on with renewal of stick and stone, and by driving those that have crossed up and down the bank. In dangerous narrow beds, it is often necessary to tow over shirkers one by one with a rope. The swimmers gallantly breast the flood, which breaks upon their crests; and they paddle with heads always up stream, dilated eyes and nostrils snorting like young hippopotami; the best always carry the back high. As they reach the far end, they wade slowly to shore, and fall at once to grazing. They took four minutes thirty seconds to cross the Thjórsá, and as usual they were drifted far down.

We then pricked fast over the little pampa which lies between the Thjórsá and the Hekla-foot, making, I know not why, for Stóruvellir. Here we were received by Síra Guðmundr Jónsson, a gentlemanly man, who has accompanied several travellers, notably the “Oxonian,” up the volcano; he showed the Iceland peculiarity of “walking the quarter-deck;” and his handsome blue-eyed daughter wore the sternest of looks, apparently engendered by semi-solitude. He indulged in wild archery about the dangers of the climb, which, over biscuits and coffee, sounded truly awful. After leaving the parsonage, we enjoyed our first fair view of Hekla: during the earlier ride it had been buried in clouds, and hidden by the chapel block, Skarðfjall.

The Hekla of our ingenuous childhood, when we believed in the “Seven Wonders of the World,” was a mighty cone, a “pillar of heaven,” upon whose dreadful summit white, black, and sanguine red lay in streaks and patches, with volumes of sooty smoke and lurid flames, and a pitchy sky. The whole was somewhat like the impossible illustrations of Vesuvian eruptions, in body-colours, plus the ice proper to Iceland. The Hekla of reality, No. 5 in the island scale,[97] is a commonplace heap, half the height of Hermon, and a mere pigmy compared with the Andine peaks, rising detached from the plains; about three and a half miles in circumference, backed by the snows of Tindafjall and Torfajökull, and supporting a sky-line that varies greatly with the angle under which it is seen. Travellers usually make it a three-horned Parnassus, with the central knob highest--which is not really the case. From the south-west, it shows now four, then five, distinct points; the north-western lip of the northern crater, which hides the true apex; the south-western lip of the same; the north-eastern lip of the southern crater, which appears the culminating point, and the two eastern edges of the southern bowls. A pair of white patches represents the “eternal snows.” On the right of the picture is the steep, but utterly unimportant, Thríhyrningr, crowned with its bench-mark; to the left, the Skarðsfjall, variegated green and black; and in the centre, the Bjólfell, a western buttress of the main building, which becomes alternately a saddleback, a dorsum, and an elephant’s head, trunk, and shoulders.

We came upon the valley of the Western Rángá[98] at a rough point, a gash in the hard yellow turf-clad clay, dotted with rough lava blocks, and with masses of conglomerate, hollowed, turned, and polished by water: the shape was a succession of S, and the left side was the more tormented. Above the ford a dwarf cascade had been formed by the lava of ’45, which caused the waters to boil, and below the ford jumped a second, where the stream forks. We then entered an Iceland “forest,” at least four feet high; the “chapparal” was composed of red willow (_Salix purpurea_), of Grá-viðir, woolly-leaved willow (_Salix lapponum_),[99] the “tree under which the Devil flayed the goats”--a diabolical difficulty, when the bush is a foot high--and the awful and venerable birch,[100] “la demoiselle des fôrets,” which has so often “blushed with patrician blood.” About mid-afternoon we reached Næfrholt (birch-bark hill),[101] the “fashionable” place for the ascent, and we at once inquired for the guide. Upon the _carpe diem_ principle, he had gone to Reykjavik with the view of drinking his late gains; but we had time to organise another, and even alpenstocks with rings and spikes are to be found at the farm-house. Everything was painfully tourist.

In the evening we scaled the stiff slope of earth and Palagonite which lies behind, or east of, Næfrholt: this crupper of Bjólfell, the Elephant Mountain, gives perhaps harder work than any part of Hekla on the normal line of ascent. From the summit we looked down upon a dwarf basin, with a lakelet of fresh water, which had a slightly (carbonic) acid taste, and which must have contained lime, as we found two kinds of shells, both uncommonly thin and fragile. Three species of weeds floated off the clean sandstrips. Walking northwards to a deserted byre, we found the drain gushing under ground from sand and rock, forming a distinct river-valley, and eventually feeding the Western Rángá. This “Vatn” is not in the map; though far from certain that it is not mentioned by Mackenzie, we named it the “Unknown Lake.” Before night fell we received a message that three English girls and their party proposed to join us. This was a “scare,” but happily the Miss Hopes proved plucky as they were young and pretty, and we rejoiced in offering this pleasant affront of the feminine foot to that grim old _solitaire_, Father Hekla.

Before the sleep necessary to prepare for the next day’s work, I will offer a few words concerning the “Etna of the North,” sparing the reader, however, the mortification of a regular history. It was apparently harmless, possibly dormant, till A.D. 1104, when Sæmund, the “Paris clerk,” then forty-eight years old, threw in a casket, and awoke the sleeping lion. Since that time fourteen regular eruptions, without including partial outbreaks, are recorded, giving an average of about two per century. The last was in 1845. The air at Reykjavik was flavoured, it is said, like a gun that wants washing; and the sounds of a distant battle were conducted by the lava and basaltic ground. The ashes extended to Scotland. When some writers tell us that on this occasion Hekla lost 500 feet in height, “so much of the summit having been blown away by the explosions,” they forget or ignore the fact that the new crater opened laterally, and low down.

Like Etna, Vesuvius, and especially Stromboli, Hekla became mythical in Middle-Age Europe, and gained wide repute as one of the gates of “Hel-viti.” Witches’ Sabbaths were held there. The spirits of the wicked, driven by those grotesque demons of Father Pinamonti which would make the fortune of a Zoological Society, were seen trooping into the infernal crater; and such facts as these do not readily slip off the mind of man. The Danes still say, “Begone to Heckenfjæld!” the North Germans, “Go to Hackelberg!” and the Scotch consign you to “John Hacklebirnie’s house.” Even Goldsmith (Animated Nature, i. 48) had heard of the local creed, “The inhabitants of Iceland believe the bellowings of Hecla are nothing else but the cries of the damned, and that its eruptions are contrived to increase their tortures.” Uno Von Troil (Letter I.), who in 1770, together with those “inclyti Brittanici,” _Baron_ Bank and Dr Solander, “gained the pleasure of being the first who ever reached the summit of this celebrated volcano,” attributes the mountain’s virginity to the superstitions of the people. He writes soberly about its marvels; and he explains its high fame by its position, skirting the watery way to and from Greenland and North America. His companions show less modesty of imagination. We may concede that an unknown ascent “required great circumspection;” and that in a high wind ascensionists were obliged to lie down. But how explain the “dread of being blown into the most dreadful precipices,” when the latter do not exist? Moreover, we learn that to “accomplish this undertaking” they had to travel from 300 to 360 miles over uninterrupted bursts of lava, which is more than the maximum length of the island, from north-east to south-west. As will be seen, modern travellers have followed suit passing well.

The next morning (July 13) broke fair and calm, reminding me

“Del bel paese la dove il sì suona.”

The Miss Hopes were punctual to a minute--an excellent thing in travelling womanhood. We rode up half-way somewhat surprised to find so few parasitic craters; the only signs of independent eruption on the western flank were the Rauðhólar (red hills), as the people call their lava hornitos and spiracles, which are little bigger than the bottle-house cones of Leith.

At an impassable divide we left our poor nags to pass the dreary time, without water or forage, and we followed the improvised guide, who caused not a little amusement. His general port was that of a bear that has lost its ragged staff--I took away his alpenstock for one of the girls--and he was plantigrade rather than cremnobatic: he had stripped to his underalls, which were very short, whilst his stockings were very long, and the heraldic gloves converted his hands to paws. The two little snow fonds (“steep glassy slopes of hard snow”) were the easiest of walking. We had nerved ourselves to

“Break neck or limbs, be maimed or boiled alive,”

but we looked in vain for the “concealed abysses,” for the “crevasses to be crossed,” and for places where “a slip would be to roll to destruction.” We did not sight the “lava wall, a capital protection against giddiness.” The snow was anything but slippery; the surface was scattered with dust, and it bristled with a forest of dwarf earth-pillars, where blown volcanic sand preserved the ice. After a slow hour and a half we reached the crater of ’45, which opened at nine A.M. on September 2, and discharged lava till the end of November. It might be passed unobserved by an unexperienced man. The only remnant is the upper lip prolonged to the right; the dimensions may have been 120 by 150 yards, and the cleft shows a projecting ice-ledge ready to fall. The feature is well marked by the new lava-field of which it is the source: the bristly “stone-river” is already degrading to superficial dust. A little beyond this bowl the ground smokes, discharging snow-steam made visible by the cold air. Hence doubtless those sententious old travellers “experienced, at one and the same time, a high degree of heat and cold.”

Fifteen minutes more led us to the First or Southern Crater, whose Ol-bogi (elbow or rim) is one of the horns conspicuous from below. It is a regular formation about 100 yards at the bottom each way, with the right (east) side red and cindery, and the left yellow and sulphury; mosses and a few flowerets grow on the lips; in the sole rise jets of steam, and a rock-rib bisects it diagonally from north-east to south-west. We thought the former the highest point of the volcano, but the aneroid corrected our mistake.

From First Crater we walked over the left or western dorsum, over which one could drive a coach, and we congratulated one another upon the exploit. Former travellers, “balancing themselves like rope dancers, succeeded in passing along the ridge of slags which was so narrow that there was scarcely room for their feet,” the breadth being “not more than two feet, having a precipice on each side several hundred feet of depth.” Charity suggests that the feature has altered, but there was no eruption between 1766 and 1845; moreover, the lip would have diminished, not increased. And one of the most modern visitors repeats the “very narrow ridge,” with the classical but incorrect adjuncts of “Scylla here, Charybdis there.” Scylla (say the crater slope) is disposed at an angle of 30°, and Mr Chapman coolly walked down this “vast” little hollow. I descended Charybdis (the outer counterscarp) far enough to make sure that it is equally easy.

Passing the “carriage road” (our own name), we crossed a _névé_ without any necessity for digging foot-holes. It lies where sulphur is notably absent. The hot patches which account for the freedom from snow, even so high above the congelation-line, are scattered about the summit: in other parts the thermometer, placed in an 18-inch hole, made earth colder than air. After a short climb we reached the apex; the ruddy-walled north-eastern lip of the Red Crater (No. 2): its lower or western rim forms two of the five summits seen from the prairie, and hides the highest point. We thus ascertained that Hekla is a linear volcano of two mouths, or three including that of ’45, and that it wants a true apical crater. But how reconcile the accounts of travellers? Pliny Miles found one cone and three craters; Madame Ida Pfeiffer, like Metcalfe, three cones and no crater.

On the summit the guides sang a song of triumph, whilst we drank to the health of our charming companions and, despite the cold wind which eventually drove us down, carefully studied the extensive view. The glorious day was out of character with a scene _niente che montagne_, as the unhappy Venetian described the Morea; rain and sleet and blinding snow would better have suited the picture, but happily they were conspicuous by their absence. Inland, beyond a steep snow-bed unpleasantly crevassed, lay a grim photograph all black and white; Lángjökull looking down upon us with a grand and freezing stare; the Hrafntinnu Valley marked by a dwarf cone, and beyond where streams head, the gloomy regions stretching to the Sprengisandur, dreary wastes of utter sterility, howling deserts of dark ashes, wholly lacking water and vegetable life, and wanting the gleam and the glow which light up the Arabian wild. Skaptár and Öræfa were hidden from sight. Seawards, ranging from west to south, the view, by contrast, was a picture of amenity and civilisation. Beyond castellated Hljóðfell and conical Skjaldbreið appeared the familiar forms of Esja, and the long lava projection of the Gold Breast country, melting into the western main. Nearer stretched the fair lowlands, once a broad deep bay, now traversed by the network of Ölfusá, Thjórsá, and the Markarfljót; while the sixfold bunch of the Westman Islands, mere stone lumps upon a blue ground, seemingly floating far below the raised horizon, lay crowned by summer sea. Eastward we distinctly traced the Fiskivötn.[102] Run the eye along the southern shore, and again the scene shifts. Below the red hornitos of the slope rises the classical Three-horned, not lofty, but remarkable for its trident top; Tindfjall (tooth-fell) with its two horns, or pyramids of ice, casting blue shadows upon the untrodden snow; and the whole mighty mass known as the Eastern Jökull, Eyjafjall (island-fell), so called from the black button of rock which crowns the long white dorsum; Kátlá (Kötlu-gjá), Merkrjökull, and Goðalands, all connected by ridges, and apparently neither lofty nor impracticable.[103] I venture to predict that they will succumb to the first well organised attack.

The descent, in three hours, was as fast as the ascent had been slow. We soon saw the last of our fair companions who, mounted and attended by their train, rode gallantly back to Stóruvellir. Amongst the party was Síra Guðmundr’s son, a sharp youth of eighteen, and if there was not something under his waistcoat buttons which was beating at an accelerated pace, I am much mistaken. We felt demoralised by this unusual dissipation; we cooled our blood with Skyr; we bathed in the Lavapés, and we tried throwing a line, but came back with a hook behind, as the people say.

The reader will probably determine that this account of Hekla is a trifle hypercritical. But after a single day spent upon the volcano, which has so often been ascended, what can man find to explore except the labours of his predecessors? Nor would it be fair to leave unnoticed this excellent specimen of exaggerated writing upon the subject of Thule, which perhaps culminates on Hekla.