CHAPTER IX

Previous

GEYSIR AND THINGVELLIR

We were very near the margin of the desert interior, for within two or three miles we arrived at the farm-house of Bratholt, the first human habitation that we had seen for ten or twelve days. We had traversed the uninhabited country and were then entering upon the final stage of the journey across the island, where we expected to see some of the better class of farms and farmers. Bratholt farm-house seemed to be one of the superior kind—it was certainly the best that we had seen so far. We lunched there, and while the meal was being prepared were shown over the premises by the farmer's wife and daughters. A fine specimen of an old kitchen attracted my attention, and I determined to try to photograph it. The housewife was most anxious to help with the camera. I had a difficulty in setting it up in a suitable position, so she volunteered to hold it wherever I wanted it to stand. I tried to explain that she could not hold it still enough, and that it would have to be kept in one position for nearly ten minutes; she stood in the way looking on till I fetched a guide to explain matters, when she left me to my own devices. It was quite a picture, this kitchen; one of the curiosities it contained was an old quern with a bone (human?) for a handle. The room was as smoky as most of the Icelandic kitchens usually are; in the roof there was a number of skins that had been hung up to dry or placed there for preservation. Some three-legged pots stood in a corner on the floor; a fire was burning in a fireplace built of lumps of basalt, and the smoke that arose from the smouldering peat bricks hung in the air till it gradually escaped through a hole in the roof.

We invaded the work-room and bed-chamber, which is usually called the bathstofa. As its name implies, this chamber was once the bath-room of the house; but bathing has gone much out of fashion with the Icelander, and he no longer considers a tub at short intervals to be desirable. The bathstofa is now used as a living-room; it is fitted up with a series of open bunks ranged along the sides, in which the various members of the family repose at night; but the bunks serve not only for sleeping purposes—they are often the receptacle for all sorts of things, and we could hardly help noticing in one a miscellaneous collection consisting of sugar, stockings, skin shoes, tea, etc. There were several spinning-wheels in the room, and at our request the lady of the house set to work at one of them. The family made cloth, various articles of clothing from it, sheep-skin shoes, and bone spoons with "Gullfoss" carved on them, for the "trippers" who call when on the way to Gullfoss. One of the daughters was an expert in the use of vegetable dyes; she was not at home, but we saw some of her work. We bought a few things: shoes, stockings, gloves, rugs, etc., and the "handy man" cleared out the stock of cloth and called for more, but more was not to be had there. Later in the day, however, we passed another farm where cloth could sometimes be bought; the "handy man" heard of this, and we lost sight of him for more than an hour while he was, ostensibly, making further purchases, though he did not seem to be overburdened with their weight when at last he turned up. In the evening he remarked on the beauty of a girl that he had seen at the farm, which raised grave doubts as to whether the charms of this beauty had not been the real cause of his long stay there. We thought it mean of him not to have informed us when in the neighbourhood, and told him so; he smiled serenely, for we were then a safe distance away—half a day's journey. We expected to camp that night at Geysir; so when the "handy man" appeared with his bundle of cloth, we pushed on for that interesting spot. We had to cross the river Tungufljot on the way; it is a rather deep and swift-flowing river, but we made an excellent crossing at a recently discovered ford where the water did not reach much above the level of our stirrups.

At Geysir there is a region of hot springs, geysers, and blue, boiling cauldrons, where one can stand on the sinter margins, look deep down into the blue waters, and imagine whence they come. There is also a number of holes where liquid mud bubbles and splutters. There are geysers active, and others quiescent and extinct. Among the latter is the celebrated Strokur—a few years ago it was very active, but now it is quite dead; it died during an earthquake that occurred in 1896. Although the earthquake stopped Strokur, it seems to have caused Great Geysir itself to play with increased energy. Strokur had to be coaxed into activity, but it was easily done by feeding it with lumps of turf, which were thrown into its yawning mouth, wide open always and ready for a meal. It never failed to give a display when properly fed. It was when it had had a surfeit, and was likely to be choked with the turf, that it erupted, ejecting the turf violently, and at the same time shooting upward a column of boiling water and steam. But all this is of the past—no quantity of turf will provoke it into activity now; it is dead, and there is no indication that it was once the scene of violent disturbance; nothing remains as a record of former glories but a hole in the ground a few feet in diameter.

It was late in the evening when we arrived. The weather was not what we should have liked, for it was dull and rainy; there had been much rain at Geysir during the previous few days, and we were informed of the fact by a farmer living in the neighbourhood. It is said that Geysir erupts more frequently during and after a period of much rain, and also when the wind blows from a certain quarter—I forget which quarter, but that is immaterial now, for the all-important thing is that it was then blowing in the favourable direction. Whether there is any real ground for the reports I do not know, but I record the fact that during a stay of about fourteen hours Geysir erupted six times, and that the average is said to be one in twenty-four hours. The first eruption occurred while we were at supper at about 10.15 p.m. There was a dull, deep-seated thud somewhere below, a sort of subterranean rumbling that caused us to inquire of our conductor, who was rather deaf, what it was. We had previously been informed that certain premonitory rumblings always preceded an eruption; but we were doubtful whether what we then heard was the warning. The conductor had not heard it, and he was endeavouring to explain to us the nature of the sound when a guide rushed to the door of the tent to inform us that Geysir was about to play. We hastily left our meal, made an abrupt exit from the tent, and rushed to the spot. Surely enough it was in eruption, for great clouds of steam were rising from the crater and rolling towards us. We got to windward of the steam, and looked towards the crater, and what a sight it was! High into the air, sixty, seventy, eighty feet up, there was shooting stream after stream of boiling water, which fell in showers of spray all around, some descending towards the crater and meeting on its way the outgoing streams. A ring of sinter surrounds the crater; it is raised ten to fifteen feet above the general level of the ground, so the hot water that fell upon it ran off in a ring of little cascades. It was a wonderful sight, this enormous natural fountain; it continued to play for two or three minutes before it gradually subsided and stopped—all was then still, save that the last of the water was streaming over the edges of the sinter ring, whence a little steam was rising. As soon as the eruption came to an end, we climbed upon the ring, which has a diameter of something like a hundred feet; there is a large depression or basin in it that is filled with water before eruption, but it was then empty. In the middle of the basin there is a funnel, said to be about sixty feet deep; at the surface it is about sixteen feet in diameter. We stood on the edge of this funnel or crater, looking down into its depths, the water then standing at a level of something like fifteen feet below that at which we had previously seen it.

THE SINTER RING OF GEYSIR.

We returned to our interrupted meal, congratulating ourselves that we had arrived just in time to witness the fine display, without at all expecting that we should have another opportunity of seeing such a spectacle. But, as I have stated, we were lucky enough to see in all six eruptions, three of which occurred at short intervals during the night. The first occurred at 10.15 p.m.; the others at 1.30, 3.30, 6.30, 8.30, and the last of the series at 10.45 a.m. The finest displays were the first, second, and last. The second, that at 1.30 a.m., occurred just after we had turned in, but the warning rumblings sounded before we had gone to sleep. Each made a dash at some articles of clothing, and hastening into them, made a blind rush through the rain to the side of Geysir, where we presented a curious spectacle: we were a very motley assemblage indeed, and the various costumes it would perhaps be better not to describe accurately. I have not a photographic record of the scene—there had been no time to get out cameras, and the light was very bad.

THE FUNNEL OR CRATER OF GEYSIR.

There is a smaller geyser, known as Little Geysir, distant about a quarter of a mile from its more important neighbour. Now, this happened to be in good working order, for it erupted while we were finishing our evening meal, sending up spray to a height of from ten to twenty feet, and continued more or less active during the rest of the night.

Many were the boiling and bubbling springs that we saw along a line of fissure nearly half a mile in extent. The basins of some of them were very beautiful, one especially, where the water was of a bright blue colour and the edges of the sinter basin quite white. The basins and terraces are composed of the silica that was at one time held in solution in the water that flowed over them; it was gradually deposited layer upon layer, slowly lining the vent through which the water was ejected, and building up the terraces and basins.

We were loth to leave the neighbourhood of Geysir and continue on our way; but we could not linger, because time was of importance to some of the members of the party, who had to reach Reykjavik, the capital of the country, in time to catch a certain steamer. Another day could not be spared, so on we had to go. We proceeded at first over a quantity of sinter debris, and then through some hummocky land. After a while we came to a wood—an Icelandic forest, or one of the nearest approaches to a forest that Iceland can boast. It consisted of a quantity of scrubby birch and willow "trees," mere bushes, averaging three to five feet in height, though some, it is true, attained the height of six or even seven feet; interspersed amongst them were some geraniums (G. silvaticum). The river BruarÁ flows through the middle of the wood, and we had to cross it on our way. The crossing was a peculiar one. At the spot there is a rapid in the river, with a waterfall just below. Hard rock stretches from side to side, forming a barrier that is cleft in the middle of the river; the water flows with very picturesque effect over the ledge and into the cleft, which is bridged by a wooden platform; the crossing is effected by the bridge, and by fording the river on each side of it. While I was photographing the spot with some members of the party on the bridge, my pony ran away, and crossed the river, leaving me on the wrong side of it. However, the runaway did not get very far before its career was checked; it was then brought back, and I followed in the track of the others.

Farther on in the wood we halted at a wayside farm-house for lunch, and to rest for a while before continuing on what was likely to be a long journey. Away we went again, though, through the wood, until we overlooked the BruarÁ at a spot where it had worn down the valley to the level of a plain of denudation, of which it is a fine specimen. There, below, was the river meandering in a winding course over the plain; there also were two small lakes, one of which, Laugarvatn, is of historical interest, for it was there that the Icelanders on being converted to Christianity were baptized; they objected to cold water, but a hot spring in this lake causes the water to be warm, so the objection was overcome, and they were baptized in the warm waters of Laugarvatn. We gradually descended to the vicinity of Laugarvatnshellirar, a peculiar volcanic district, where a number of castellated-looking rocks on the hillsides are very suggestive of ancient ruins. To the left of them rises the Kalfstindar range, the peaks of which are the hard plugs of ancient volcanoes that have become exposed by the erosion of the softer material of the original cones. Here we came upon recent lava again, and during the rest of the day's journey we were obliged to travel very slowly, for we had to pick our way over very rough ground.

The ponies stumbled along hour after hour, much to the discomfiture of the "nautical adviser," who was in a helpless state, suffering great pain. Earlier in the day he had been stung on the eye by an insect. At first he did not feel much inconvenience, but as time passed, his eye became inflamed and very troublesome; so intense was the pain at last, that his eyes had to be bandaged. Thus blindfolded he had to ride on, just balancing himself, and allowing his pony to pick its own way through the lava as it followed one or another of us. It was a very dangerous proceeding, because the lava over which he had to pass was of the roughest possible kind; the ponies had to perform all sorts of peculiar antics while dodging from side to side, or in climbing over boulders or outcropping rocks, now going up a steep slope, then descending one at a dangerous-looking angle. When three or four miles from Thingvellir, our destination that night, we came to a great rift in the earth known as Hrafna-gjÁ (Raven's Rift), a crack going deep down into the earth, and extending three or four miles in a line parallel to another even greater rift that will be again referred to. On reaching Hrafna-gjÁ, we had to climb down its steep side, there being a drop of something like a hundred feet to the lava at its foot. The steepness and unevenness of the descent rendered it necessary for us all to dismount and lead our ponies down. The day was dull and the light then becoming bad; but we had to plod on. We were not many miles from our destination, Thingvellir. We presently saw right ahead what looked like a line of high precipitous cliffs with a white patch in it. At first we were very doubtful what the patch could be; but on drawing nearer we heard the splash of falling water, and from the sound, judged that the volume was pretty large. We could see nothing distinctly, though, for it was approaching midnight and the light was failing fast, so we pushed on along a line parallel to the cliff, unable to distinguish anything clearly.

It was at Vallholt, close to the margin of Lake Thingvallavatn, that we halted. There we reached modern civilisation suddenly, for we came to a large galvanised iron structure which we found to be a hotel, so we pulled up and dismounted. On inquiring for our tents, we were informed that they had not been erected, and that we were to take up our quarters at the hotel. We had not expected this, and as we had all become somewhat attached to our canvas quarters, we grumblingly entered the hotel and went in search of our boxes. The arrangement of the interior was peculiar: a large hall occupied the middle of the building, extending the full width, and reaching from floor to roof; at each end of the hall, a passage led through to the end of the building. On each side of one of these passages there was ranged a number of cabin-like rooms, each of which contained two bunks, one above the other, and in a corner there was a wash-hand basin, the whole being fitted up like the interior of a cabin on board ship—this was accounted for by the fact that the arrangement had been designed by a sailor.

Thomas and I had piloted the "nautical adviser" and given his pony a lead during the last part of the journey, so we three were rather late in our arrival; but we were met with the cheering intelligence that supper (it was 11.30 p.m.) would be ready in a few minutes, and that we were to "hurry up" and make whatever change of costume we deemed necessary to celebrate the return to some of the conventionalities of modern civilisation. We were hungry, very hungry, and did not waste time over an elaborate toilet, but soon put in an appearance in the large central hall. Here we were regaled with a most sumptuous and excellent banquet. The soup was all that could be desired, and it was hot—a very comforting thing when one is half frozen. This whetted our appetite for the other good things that were to follow: salmon that was cooked to perfection; then came another excellent dish, and last of all delicious pastry and cream—the Icelanders, as I have already stated, are noted for the quality of their pastry. We had growled on finding that we were to take up quarters in a tourists' hotel, but the quality of the dinner quite reconciled us to the return to civilisation. We had been living for more than a fortnight on tinned foods, so we fully appreciated the good things that "mine host" had provided for us. We were disappointed in one way; but when a hungry man has fed well he is not disposed to quarrel with things in general—especially when they take the form of a fairly comfortable bunk and more room in his cabin than he would have had in his tent.

Thingvellir and the neighbourhood is a most interesting and historic place, for it was there, in the tenth century, that the Althing, or Parliament, used to assemble. The spot whereon it once met, known as the Logberg (Law Rock), is now a verdure-covered hill, lying between two remarkable rifts in the lava. Thingvallavatn is the name of the largest and most picturesque lake in Iceland; the view of it which we had obtained the day before from above Hrafna-gjÁ was very fine, but the atmosphere had not been quite clear; we had seen enough, however, in spite of rain and haze, to enable us to form an idea of the beauty of the scene. We were favoured on this occasion, for the air was clearer and the light brighter, so we were better able, from the elevated site of the Logberg, to enjoy the fine view. The meeting-place of the Althing was removed from the Logberg to one of two islands lying in the lake, but to which of them is questionable, though it is supposed that it used to meet on the long flat island near Thingvellir, close to the shore of the lake.

Not only is this neighbourhood interesting historically, but geologically it claims attention. I have already mentioned the remarkable rift, Hrafna-gjÁ; there is another at Thingvellir—I am not referring to the two rifts at the Logberg, for though noticeable in themselves, they are but minor rifts when compared with that of Hrafna-gjÁ, and still more so when comparison is made with Almanna-gjÁ (All-men's Rift) at Thingvellir. It is a most extraordinary break in the earth, extending for three or four miles across the country in a line parallel to Hrafna-gjÁ, showing a face of lava with a drop of something like a hundred feet. Now what has happened to cause these extraordinary rifts? The whole of the land between Hrafna-gjÁ and Almanna-gjÁ has fallen in, dropped through about a hundred feet, and forms a "rift valley." The lake derives its water chiefly by underground rivers from the ice-field of Lang JÖkull, though one small stream, the OxarÁ, runs into it. This river tumbles over the edge of the cliffs by a fine cascade into the rift of Almanna-gjÁ; but it does not flow very far (less than a mile) before it escapes through a gap in the outer wall of the rift by a second and smaller fall. Above the smaller fall there is a pool known as the Murderesses' Pool, in which it was once the custom to drown women found guilty of infanticide or adultery.

ALMANNA-GJÁ—IN THE RIFT NEAR THE WATERFALL.

There are several legends connected with Thingvellir. One of them refers to a remarkable jump supposed to have been performed by one Flossi, an outlaw, who, on being closely pursued, escaped by jumping across one of the lava rifts of the Logberg hill—an impossible feat with the rift at its present width, but it is supposed to have widened considerably. In these rifts of the Logberg there is, deep down, some beautifully clear water standing at about the same level as the lake. Over one of the rifts there is a small wooden bridge with a hole in the middle of it; beside the hole we saw a bucket with a long rope attached. As the clear water of one of the pools was immediately below, it was not difficult to infer that this was the source of the water-supply of the hotel which was in the immediate neighbourhood.

After we had seen all that was of special interest at Thingvellir, we started on the last stage of our journey across the island; but before doing so we took leave of two of the guides, Josef and Sigurthur, who were returning to our starting-point, Akureyri, with about a dozen of the ponies; for we had no further use for the full pack, seeing that we expected to reach Reykjavik, the capital, in the course of a few hours. From this place to Reykjavik a road has been constructed—a rough one at best, but still a road; the only one of any length in all Iceland, for it is thirty-six miles long. It commences just below the lower fall of the OxarÁ; after a short ascent, a bridge crosses the river between the waterfall and the Murderesses' Pool, whence it rises by a steep ascent to the level of the country above the rift. This part of the road has been cut in the side of the fissure of Almanna-gjÁ. From above we obtained a fine view overlooking Lake Thingvallavatn, but after losing sight of the lake we saw no more of the picturesque until nearing Reykjavik. An exceedingly fine specimen of a glaciated lava surface attracted Thomas and myself. My photograph shows it excellently: in it there can be seen the undulating surfaces of lava, the roches moutonnÉes, just as they were smoothed by the passing ice, and there on the surfaces are several "perched blocks" which helped in the smoothing and scratching process. There was evidence all along the road not only of the work of frost and ice, but also of that of fire and heat, for we saw in all directions tuff and lava cones and volcanic necks.

GLACIATED LAVA SURFACE NEAR THINGVELLIR.

On nearing Reykjavik we met a number of pack-trains conveying goods of all descriptions to the farms. It was just the end of the season when the farmers make their annual journey to the capital. They take in their wool, dispose of it, and then return with whatever goods they have purchased. Some of the farmer's women-folk accompany him as a rule. The women ride their ponies on a saddle peculiar to Iceland. They balance themselves on their ponies seated sideways, with feet resting on a little platform that hangs suspended from the saddle by two straps; they ride by balance alone, for there is no horn by which they can grip the saddle. All goods have to be transported on the backs of ponies, for as there are no roads (with the exception of that from Reykjavik to Thingvellir) so there are no carts or waggons in general use—I did see three carts in Iceland, one of them in Reykjavik, but they were used only for hauling goods from the wharves into the towns. Timber and galvanised iron are carried balanced on the backs of ponies, the galvanised iron having to be doubled up. A pony sometimes looks very peculiar as he plods along with an unwieldy load swinging from side to side. He has an awkward time of it whenever there is a heavy or gusty wind blowing, and that in Iceland is very frequently. Heavy goods that cannot possibly be carried on the backs of ponies are transported when the winter snows cover the ground; rough sleighs are then used for the purpose.


                                                                                                                                                                                                                                                                                                           

Clyx.com


Top of Page
Top of Page