We had been told at Reykjavik it was necessary to carry tents, as there was no accommodation for travellers at the Geysers, but on arriving the wind was so strong that there was considerable difficulty in pitching them, and while our guides and gentlemen friends were making the attempt, we ladies tied up some tea in a muslin bag, and put it into a kettle, which we filled at the nearest hot spring. In a very few minutes it was infused, and with thick cream procured from the neighbouring farm, we enjoyed it much after our long dusty ride.

Just as the tent had been, as my brother thought, securely fixed, and while Vaughan and Mr Gordon were inside arranging the rugs and pack-boxes as seats, unfortunately a fresh gust of wind brought the whole affair down, burying them under the ruin. Our guides hastened to the rescue, and, more experienced in the weather forecasts than they were, advised their waiting till the wind had subsided before attempting to put up the tent again. To take our tea sitting on the pack-boxes was all we could do, encouraging each other to patience. We dare not open our boxes of eatables till the stormp. 122 had subsided, or at least until we had some shelter to protect them from a deposit of dust.

After tea we proceeded to make our inspection of the Geysers. Our first need was, however, to wash our hands and faces, so, armed with towels, sponges, and soap, we knelt at the brink of the nearest pool, and stooping down performed our ablutions, with our faces towards the east, our persons being reflected in the clear green water. We could but liken ourselves to Mahommedans, when they turn their faces towards Kibla, at Mecca, or Parsees when they kneel facing the sun, which is considered by them a representative of God.

The immediate neighbourhood of the Geysers is not pretty; hills rise on one side, but otherwise they lie in a plain, which, when we saw it on our first arrival, was so thickly covered with sand from the storm that we could hardly discern any separate object. We hastened to examine the great Geyser. Alas! it did not, and would not play; it had done so two days previously, and we were told it was expected to renew the exploit, but, to our great mortification, it failed to do so during our visit. One of the peculiarities of this natural phenomenon is that sometimes at intervals of only a few hours it will eject columns of boiling water to the height of 100 feet, at others it will remain silent for days together. In 1770 it is recorded that this Geyser spouted eleven times in one day. Disappointed at losing the sight we had come so far to see, we turned our attention to the 'Stroker,' which is situated aboutp. 123 90 feet from its bigger neighbour. This also seemed in a quiescent state, but as the 'Stroker' can always be made to play by filling up the opening with earth sods, until there is no hole for the steam to escape, and it vomits the whole mass with a gigantic spout, we requested our guides to arrange for this artificial display. The emetic was consequently administered. 'Stroker' was evidently sulky, for the process had to be gone through no less than four times, whilst we waited the result in patience for at least two hours; but the display was all the better when it came.

I said we waited in patience, which was hardly true, as we were all on the tiptoe of excitement. Continual false alarms, and we all rushed to the 'Stroker's' side, only to be again disappointed, so we unpacked our goods, and made preparations for our evening meal, examining the Great Geyser and the hot springs meanwhile, grumbled at the smell of sulphur, and nearly despaired of the eruption ever taking place, when a sudden start from our guides, who were standing on the edge of the crater, and a shriek from them, 'He comes!' and a huge column of water ascended straight into the air for about 60 feet, the spray being ejected to a considerable distance. The eruption was accompanied by a rumbling noise and a hissing sound, as the shafts of water ascended.

We stood and watched the effect a few feet distant merely from this boiling column, feeling the rumbling distinctly under our feet and as the wind blew the steam back, it fell like rain,p. 124 quite cold, but with sufficient force to wet us uncomfortably.

This great fountain display continued in full force a quarter of an hour; then the column gradually got smaller, though steam and water issued from its mouth for a full half-hour before it quite subsided. It was a splendid spectacle, and one which left a great impression on our minds; the height of the column was fully 60 feet, and even after it had subsided, we remained some time in contemplation of its cause and effect.

Speaking of Geysers, Professor Geikie says,—

'Eruptive formations of hot water and steam, to which the general name of Geyser (i.e., gusher) is given from the examples in Iceland, which were the first to be seen and described, mark a declining phase of volcanic activity.... It is from irregular tube-like excrescences that the eruptions take place. The term Geyser is restricted to active openings whence columns of hot water and steam are from time to time ejected; the non-eruptive pools are only hot springs. A true Geyser should thus possess an underground pipe or passage, terminating at the surface in an opening built round with deposits of sinter. At more or less regular intervals, rumblings and sharp detonations in the pipe are followed by an agitation of water in the basin, and then the violent expulsion of a column of water and steam to a considerable height in the air.'

Dr Samuel Kneeland, in his interesting book on Iceland, says,p. 125—

'There are two kinds of Geysers, one having jets of clear water, the other puffs of scalding vapour, coming up through a soft mud or clay of a reddish colour, probably from iron salts. In the water silica is held in solution by salts of soda, a silicate of soda being the chief ingredient. They are said to have great remediable powers; but, judging from the facility with which objects are encrusted by their silicates, it would seem as if their free use would soon turn a person to stone.... The geyserite, or the solid incrustations, is over 80° of silica, with 3° alumina, and a little magnesia, iron, potash, and soda.'

One thing I looked for in vain at these Geysers, namely, the pretty-coloured mud which is found at the Yellowstone Park of America, and which I had often heard my father and brother describe. In New Zealand the Geyser mud was formerly used by the Maoris as a kind of porridge, which they were very fond of. It is a pity the starving Icelanders cannot do likewise.

I wish our party could have been photographed as it stood round the 'Stroker,' waiting for the display, everybody's face a picture of expectation, which changed to disappointment at the long time we had to wait. As 'little things please little minds,' to pass the time, Miss T. and I were trundled about in the wheelbarrow in which the old men had brought the sods for the Geyser's emetic from the farm; an occasional upset made our ride all the more amusing. It was a ridep. 126 worth noting, as it was performed in one of the very few wheeled conveyances in the Island.

By the time the exhibition of the Geyser was over, the wind had lulled, the sandstorm had ceased, and our tents had been successfully pitched. In the larger tent we dined, and for such an out-of-the-way place, it was so wonderful a meal that I must describe it. We were sitting on the pack-boxes inside the tent, waited on by two guides. First there was ox-tail soup quite hot, the tin having been placed in a neighbouring hot spring—the Blissa—for twenty minutes. We had no soup plates, but tumblers served the occasion, being afterwards washed by the guides, and made ready for further use.

Tinned meat-collops followed, splendidly hot, and to us hungry mortals appeared excellent. The third course was tongue, followed by tinned apricots and thick cream. Alas! we had no spoons, and how to eat our cream and apricots was a puzzle. Our guide, whom we had christened 'Johnny,' to his great delight, helped us out of this difficulty. He produced some horn spoons which he had carved during the long winter evenings, and which he offered to sell to us for a krone a-piece. It was quite high price enough, notwithstanding the carving, but the necessity of the occasion made us glad to close with his offer. Cheese, biscuit, and figs concluded our magnificent repast.

After dinner, another inspection of the greatp. 127 Geyser, to see if it was more inclined to favour us with a display of its power, but a fruitless one; a walk amongst the hot springs, and then, as it was bitterly cold, we decided to turn in for the night. Our tents were pitched exactly half way between the great Geyser and the 'Stroker.' The large tent was to serve for the three gentlemen and the two guides, and the smaller one for Miss T. and myself.

We had secured some bundles of hay for our beds, and our mackintosh sheets were used to cover over them. My brother undertook to make our beds, and arrange our tent for the night, and disappeared inside, carrying with him the rugs, air-pillows, etc., necessary for the purpose.

On his returning and telling us all was ready, Miss T. and myself bid the party good-night. We had not till then realised the height of our bedchamber, and how to enter it was a puzzle. It was not like the big tent, which would hold a dozen people standing erect, but a tiny gipsy tent, the opening so low, we literally had to crawl in on our hands and knees, whilst the whole community stood round watching us, and laughing heartily.

Once inside, our difficulties were not over, for we found the sides of the tent so low that we could only sit up straight in the middle. So we could do no more than partially undress and roll ourselves in our fur cloaks and rugs. With the exception of waking now and then to listen to thep. 128 rumblings we had been told to expect before the eruption of the Great Geyser, we spent a tolerably comfortable night, notwithstanding we were surrounded by boiling, seething waters on every side, and were in hopeful expectation of the big Geyser's eruption. By the morning we had got quite accustomed to the sulphurous odours.

We had several visitors in the early morning, who thrust under our tent such articles as jewellery, saddle-cloths, carved spoons, etc., for sale. We bargained for some of these, and ultimately obtained them. The prices at first asked were absurdly high, but these simple-minded Icelanders have an idea that our nation's liberality is unbounded.

There is really little good old jewellery left in the Island, in consequence of the extreme poverty of the natives, who have sold to travellers the greater portion of that which they possessed.

How to dress in our three feet tent, was a problem which for some time our minds failed to solve, and still more, how and where to wash, until the gentlemen informed us that as they were going to the springs to bathe, their tent was at our disposal for as long as we wished. Here we found that their forethought had provided a large tub from the farm, which they had filled with warm water, so, after all, we had a luxurious bath.

When our only looking-glass was passed round, we each in turn exclaimed, 'How fearfully burnt Ip. 129 am!' and so indeed we were. Our yachting caps and deerstalkers had been shade enough on board ship, but not for a four days' ride across country in wind and a dust storm.

We had arrived at our journey's end, had seen the 'Stroker' at any rate play, and now if we wished to catch our steamer at Reykjavik, we had no time to lose in preparing for our return journey, so after breakfast, while our guides collected our steeds, packed the tents, etc., we started for a final look at the Geysers and the hot springs, which so abound in this neighbourhood. There are, I believe, no less than fifty within the circuit of half a mile. These springs lie at the base of a mountain of no great height, the tract in which these thermal waters is found being about 700 yards in length and 300 in width.

The Great Geyser lies to the north of this plain, its basin, 60 feet in diameter, is at the summit of a mound 20 feet in height, composed of silica, a mineral that the Geyser water holds in solution, and which from the constant overflowing of the water, deposits layers of beautiful enamel, which at the top is too hard to detach, although round the base soft and crumbly. The basin is nearly circular, and is generally, except after an eruption, full to the brim, and always steaming, the water at the bottom being about 228° Fahr.

The tube in the centre, from which the water spouts is about 10 feet across, and I read somewhere that on measuring down about 70 feet,p. 130 the tube took a sudden turn which prevented further soundings. The water is ejected at a heat of 180° or 190° Fahr., and rises over 100 feet into the air.

These Geysers are nearly 400 feet above sea level.

The formation of the 'Stroker' differs from that of the Great Geyser in not having any basin round its well, the latter being in shape like a rough test-tube, about 8 feet in diameter and 36 feet deep, with two pipe-mouths. After the eruption witnessed by 'Burton,' he noticed that 'the level of the water in the tube was at a depth of 25 feet, where might be seen, partly submerged, the mouths of two pipes entering at different angles, close together on the side nearest the Great Geyser. From these pipes steam belched forth at intervals with considerable force, churning the water in the well round rapidly.'

It is strange that the eruptions of the 'Stroker' do not affect the water in the well of the Great Geyser, though it is not 100 yards off, while on the other hand, when the Geyser is in eruption, the water of the 'Stroker' subsides.

It really was very tantalising to have come so far, and be within a few hours' distance of Hecla, and yet have to return without having visited it. Besides, from what we gathered, we could well have exhausted another week in expeditions in the neighbourhood, but snow-capped Hecla, the ice-clad heights of the JÖklar, and thep. 131 Red Crater, with innumerable other interesting excursions of Icelandic note, had to be left for a future visit, if ever we should make it, to the Island.

The name of Hecla means a mantle: its last eruption occurred in 1845. Where is Hecla? Who has not been asked that question at school? and little did I think, when learning geography, that I should ever see it, even at a distance. Alas! time would not allow us a nearer acquaintance. Visiting it meant either seventeen days round the Island in a Danish boat, or waiting six weeks for the Camoens, circumstances over which we had no control made both impossible, and we had reluctantly to give up the excursion. While these volcanoes and their adjuncts must ever remain, from their uncertain eruptions, a cause of terror to the inhabitants—boiling and bubbling for years, and then suddenly bursting forth, to the entire destruction of all around—they have, we know also, a beneficial effect in the world's domestic economy. What, for instance, would happen to Britain were it not for the Gulf Stream? It would be as cold as Labrador. The streams in the Gulf of Mexico are fed from equatorial currents and boiling springs, and rush on to the North Atlantic 25° or 30° warmer than the sea through which it passes, warming the air of Western Europe.

Again, hot springs (caused by subterranean fires), which, from their curative celebrity, attractp. 132 visitors and invalids, mean business, and business means money to the inhabitants of the locality.

Taking our last farewell of these seething pools, which bubbled and boiled around us, I could not help wondering what kind of commotion could be going on beneath the earth's surface. A power that could thus eject 100 feet of boiling water into the air, and not burst asunder the surrounding ground, was indeed a marvellous phenomenon. The Iceland Geysers, which were the first discovered, as well as those of New Zealand (so soon to be destroyed), and those of the Yellowstone Park, must ever be of enormous interest to the traveller and geologist, and with regret we turned our backs upon them, having reached the turning-point of our journey and the limit of our time. Time waits on no man, so we tore ourselves away, feeling, however, we had seen in the Iceland Geysers one of the greatest marvels of Nature.

Various explanations of Geysers have been attempted by scientific men, and as some of my readers may take sufficient interest in these wonderful phenomena to wish to know something regarding the causes which originate them, I have got my father to write a short chapter on what he saw and thought of the great Geysers in the volcanic district of the Yellowstone Park, which I have appended at the end of my narrative.

p. 133