———————“grown more holy,
Just like the very Reverend Rowley Powley,
Who shoes the glorious animal with stilts,—
A modern Ancient Pistol, by the hilts!”
We crossed one of those deep chasms or cracks in the lava, so common in volcanic regions. Here a natural bridge of lava was left, apparently on purpose for a road across it. While riding along in this miniature forest, a large flock or brood of ptarmigans flew up before us. This, one of the fine game-birds of the mountainous parts of Scotland, is very common in Iceland. From being long out of the habit of shooting, I believe the murderous propensities bred in my youth—with “dad’s old musket”—have pretty nearly all evaporated. And why should I regret it? A more cheerful or happy sight than flocks of beautiful birds, young and old, cannot be seen. Then see the terrible contrast of “sulphurous smoke and dreadful slaughter,” that follows the “fowler’s murder-aiming eye,” and all for “sport.” The ptarmigan, I believe, is seldom found in America. It is about the size of the partridge of the State of New York, a greyish brown in summer, and turning quite white in winter. The Icelanders call this bird the reaper. Had they game laws here—and thank heaven they don’t require them—it would not be permitted to shoot this bird at this season. The young in this flock, though able to fly short distances, were not over half grown. I have a bit of a confession to make, and I may as well make it now. The day that I was traveling was Sunday! I met several parties of Icelanders, traveling also; the immediate object of our journeying being different: they were going to church, and I was going to see the Geysers. The parties I met were going towards the Thingvalla church, and had on their Sunday’s best. They were all on horseback, the universal way of traveling in this country. Indeed, indeed, it was very queer, the riding of the young Icelandic ladies. These pretty damsels rode just like their brothers. My pen refuses a more elaborate and bifurcated description. The matrons all had a very convenient kind of side-saddle. It was like an arm-chair, the back and arms forming part of a circle, all in one piece. The dame rides exactly sideways, at a right angle with her horse, her feet placed on a sort of wooden step. The saddle must be pretty heavy, but the little animals and their riders seemed to get along very well. There was nothing peculiar about the costume of the females, except the little black caps with long silk tassels, universally worn in Iceland, in doors and out, in place of any other cap or bonnet.
We journeyed towards the south, skirting the shore of the lake some five miles, and then turned to the east, climbing a sharp and steep mountain, but not of great height. From the top we had a fine view of the surrounding country, and to the west, the broad lake, the “Thingvalla vatn.” Across the lake, some ten miles distant—though, from the magical purity of the atmosphere, it seemed but a stone’s throw—was a range of mountains, sloping down to the water’s edge, with patches of snow on their sides. Directly beneath us, at the foot of the mountain, lay the lake with its myriads of trout, and its water a thousand feet deep. Two abrupt islands rise high above the surface. They are mere hills of lava and volcanic matter, without a particle of vegetation. They are called Sandey and Nesey. We traveled some little distance on the broad, flat surface of the mountain, and crossed—by descending into it—one of the deep lava chasms. We did not descend, in going down the mountain to the east, as much as we had ascended; but found it spread itself out into a broad table-land, a number of hundred feet higher than the lake. With long ranges of mountains before us, we traveled several miles over a most desolate volcanic region, completely covered with lava rocks, scoriæ, and volcanic sand. Like all the lava-covered country, it was broken up in huge, irregular masses, and very cavernous, in some places showing caves thirty or forty feet deep. No description or picture will give a good idea of the old lava on the surface of the ground, to a person who has never been in a volcanic country. Not the roughest lime-stone region I have ever seen will bear the slightest comparison with the lava-covered districts—near two-thirds of the surface—of Iceland. In written descriptions of volcanic regions, we often see mention made of “streams of lava.” These streams in other countries are usually down the sides of mountains, but here in Iceland they extend for miles along the surface of the level ground, and we are puzzled to know where it came from, for usually we see no crater or mountain anywhere near. I have seen these “streams” standing up in bold relief, a black, rough, horrid mass, from ten to a hundred feet deep, several hundred yards wide, and one or two miles in length. Brydone, in his observations of Mt. Ætna, pulled all the old theologians about his ears by making a calculation respecting the age of the lava, and proving conclusively—to himself—that some of the lava streams from Ætna were fourteen thousand years old. I believe, however, that philosophers have to own themselves baffled in trying to get at the age of lava. After cooling—which often takes some years—and breaking up by the expansion of the air in it, the lava is usually nearly or quite black. After several hundred years it turns a little more towards a brown, or rather gets grey with age, and is covered with a very slight coating of one of the most inferior of the mosses. Very old lava often gets quite rotten, light, and porous, and in this state is frequently very red. Take a thick piece of zinc and break it with a hammer, and you will have a rough surface that, multiplied ten thousand times, will give some idea of a stream of lava. The word “horrible,” both in the Icelandic and in English descriptions, is often and most appropriately applied to the fields of lava.
As we traveled east and approached nearer and nearer the range of mountains, the way became much smoother till we found ourselves on a plain of black, volcanic sand. Near the base of the mountain range before us, the guide took me aside a hundred yards or so to see a curious volcanic crater called the Tin Tron. It stands near twenty feet above the surface of the ground, like a chimney, but on climbing up the side of it and looking down into it, it appears like a well, but the cavity grows much wider below the surface of the ground. On throwing in a stone, after a little period, it quashed in a bed of water, seemingly some fifty feet below where we stood. One side of it was partly broken away, so we did not have to climb clear to the top of it to look down the aperture. I broke off some pieces of lava from the top of the crater with my hands, and found it very soft, light, and porous. This lava was a beautiful purple, and some of it a bright red color. I brought away several samples. We wound round the mountain and descended into a broad and fertile valley called the “Laugardalr,” or vale of warm springs. Broad meadows surrounded us, and we could see the steam rising from numerous hot springs in the distance. This valley appeared like an immense amphitheatre surrounded by mountains. I know not that a painter could make much of it, but the Laugardalr is a fine landscape. It is not like a vale in Derbyshire, or a country scene on the banks of the Connecticut. No forests, no grain fields, orchards, fences, or houses, and yet it is a scene of great interest, and not easily forgotten.
I had plenty of time, as we wound our way slowly down the hillside from the elevated table land, and an opportunity to observe the peculiarities of the country. Certain little green hillocks to my now more practised eye showed themselves to me as habitations. To the left lay a smooth lake, and in bright lines through the green meadow land were several white looking rivers. On every side were high mountains, many of them covered on the tops with snow. Here I got the first view of Hekla, though more than forty miles distant. It was black nearly to the top, where were some small snow banks. This valley, including much that is beyond the Laugardalr, is one of the most extensive and fertile farming districts in Iceland. It extends nearly one hundred miles south to the Atlantic ocean, and is bounded on the east and southeast by Mt. Hekla and the Tindfjalla and Eyjafjalla Jokulls. This tract of country is watered by Iceland’s largest rivers; the Hvitá or White river, the Brúará, the Túngufljot, the Laxá, and the Thjorsá.
We stopped near the first farm-house, and had the saddles taken off, that the ponies could recruit a little on the fine meadow grass, while we went through that very necessary daily ceremony of dining. The farmer sent me out some excellent milk in a Staffordshire bowl, and soon after he and his wife and daughter came out to see me hide it under my jacket. Madame Pfeiffer, in her snarling, ill-tempered journal, complains greatly of the idle curiosity of the people in crowding about and looking at her. From what I heard of her, she was so haughty that the simple and hospitable Icelanders could not approach her near enough to show her any attentions. I exhausted my little stock of Icelandic in talking with the farmer, praised his farm, his cows, the milk, his country, his wife and daughter, called the latter handsome—“fallegh stulkey”—what a lie!—and giving him a piece of silver, which he seemed to like better than all the “fair words”—“butter without parsneps”—and, jumping into our saddles, away we went.
We passed near the small lake, the Laugarvatn, and saw the steam rising from the hot springs near it, but being out of our way we did not visit them. Several hot springs have their source in the bottom of the lake, and only reveal their existence by the steam that rises from the surface of the water. We got into a fine road in a large meadow or bottom land, and I was having a fine gallop across the plain, when the guide called to me to turn aside. I was greatly provoked on his taking me a mile out of the way to show me a cave in the hill side, which he seemed to think was a great curiosity. This wonderful cavern was about twenty feet deep! I “blowed him up” well for a stupid fellow, and told him he need not show a cave like that to an American, for we had caves that extended under ground farther than from there to the Geysers—some ten miles ahead—and cared very little for such a fox burrow as that. He said he showed it to English gentlemen, and they thought it very grand! Well, I told him, he might show it to English gentlemen, but he better not to Yankees, if he consulted his reputation as a guide. Rising a hill we saw to our right another lake, the Apavatn. We crossed the Brúará or Bridge river, the only river in Iceland—with one exception, the Jokulsá, in the east country—that has a bridge over it. This bridge does not span the river by any means, but it merely crosses a chasm or deep place in the middle of the stream. Our horses waded over the rocky bottom and shallow water forty or fifty yards, when we came to a deep chasm, perhaps ten yards across, and over this a slight wooden structure, about six feet wide, was thrown. In this chasm the water is a most furious torrent, roaring some fifty feet below the bridge. Our horses were some frightened, and required considerable urging to get them to cross the frail bridge. The chasm commences but a little way up the river from the bridge, and there the greatest share of the water in the river pours into it, forming a furious and singular cataract. I stopped my horse a few moments on the bridge, and looked at the angry torrent as it rushed beneath me. The water, except where broken into foam, has a deep green appearance. On the road from Thingvalla to the Geysers, nearly all the way, we had mountains on our left, and fine fertile meadows on the right, towards the south. A great deal of the way, a ridge of lava extends along the foot of the mountain, and sometimes, for a long distance, I noticed a strip of fine meadow land between the foot of the mountain and this ridge of lava, the meadow as well as the strip of lava being several hundred yards wide. How this came to be so I could not tell, unless it happened that, after the last eruption of lava, large quantities of ashes were thrown out of the mountain, covering the lava for some distance from its base, and thus forming a coat of soil where now the green meadow is seen. As I have mentioned before, nearly every foot of land in Iceland shows proofs of volcanic origin, and, without doubt, the entire island was formed by volcanic action. At whatever period that took place, if mortal man could have seen it, there would have been a picture of the power of the Almighty most awful to behold. What a scene! A tract of land forty thousand square miles in extent, rising amidst fire and smoke and earthquakes, from the bottom of the ocean. The proofs of subterranean fire shown at the present day, in the occasional action of the volcanoes, and constant spouting of numerous geysers and hot springs of water and boiling mud, exhibit scenes of sublimity and grandeur unequaled on the face of the globe.