§ 12. The only portion of the Matterhorn which approaches such a condition is the shoulder, before alluded to, forming a step of about one twelfth the height of the whole peak, shown by light on its snowy side, or upper surface, in the right-hand figure of [Plate 38]. Allowing 4000 feet for the height of the peak, this step or shoulder will be between 300 and 400 feet in absolute height; and as it is not only perpendicular, but assuredly overhangs, both at this snow-lighted angle and at the other corner of the mountain (seen against the sky in the same figure), I have not the slightest doubt that a plumb-line would swing from the brow of either of these bastions, between 600 and 800 feet, without touching rock. The intermediate portion of the cliff which joins them is, however, not more than vertical. I was therefore anxious chiefly to observe the structure of the two angles, and, to that end, to see the mountain close on that side, from the Zmutt glacier.

§ 13. I am afraid my dislike to the nomenclatures invented by the German philosophers has been unreasonably, though involuntarily, complicated with that which, crossing out of Italy, one necessarily feels for those invented by the German peasantry. As travellers now every day more frequently visit the neighborhood of the Monte Rosa, it would surely be a permissible, because convenient, poetical license, to invent some other name for this noble glacier, whose present title, certainly not euphonious, has the additional disadvantage of being easily confounded with that of the Zermatt glacier, properly so called. I mean myself, henceforward, to call it the Red glacier, because, for two or three miles above its lower extremity, the whole surface of it is covered with blocks of reddish gneiss, or other slaty crystalline rocks,—some fallen from the Cervin, some from the Weisshorn, some brought from the Stockhi and Dent d'Erin, but little rolled or ground down in the transit, and covering the ice, often four or five feet deep, with a species of macadamization on a large scale (each stone being usually some foot or foot and a half in diameter), anything but convenient to a traveller in haste. Higher up, the ice opens into broad white fields and furrows, hard and dry, scarcely fissured at all, except just under the Cervin, and forming a silent and solemn causeway, paved, as it seems, with white marble from side to side; broad enough for the march of an army in line of battle, but quiet as a street of tombs in a buried city, and bordered on each hand by ghostly cliffs of that faint granite purple which seems, in its far-away height, as unsubstantial as the dark blue that bounds it;—the whole scene so changeless and soundless; so removed, not merely from the presence of men, but even from their thoughts; so destitute of all life of tree or herb, and so immeasurable in its lonely brightness of majestic death, that it looks like a world from which not only the human, but the spiritual, presences had perished, and the last of its archangels, building the great mountains for their monuments, had laid themselves down in the sunlight to an eternal rest, each in his white shroud.

§ 14. The first point from which the Matterhorn precipices, which I came to examine, show their structure distinctly, is about half-way up the valley, before reaching the glacier. The most convenient path, and access to the ice, are on the south; but it is best, in order to watch the changes of the Matterhorn, to keep on the north side of the valley; and, at the point just named, the shoulder marked e in [Fig. 33], [p. 181], is seen, in the morning sunlight, to be composed of zigzag beds, apparently of eddied sand.

Fig. 81.

I have no doubt they once were eddied sand; that is to say, sea or torrent drift, hardened by fire into crystalline rock; but whether they ever were or not, the certain fact is, that here we have a precipice, trenchant, overhanging, and 500 feet in height, cut across the thin beds which compose it as smoothly as a piece of fine-grained wood is cut with a chisel.

§ 15. From this point, also, the nature of the corresponding bastion, c d, Fig 33, is also discernible. It is the edge of a great concave precipice, cut out of the mountain, as the smooth hollows are out of the rocks at the foot of a waterfall, and across which the variously colored beds, thrown by perspective into corresponding curvatures, run exactly like the seams of canvas in a Venetian felucca's sail.

Seen from this spot, it seems impossible that the mountain should long support itself in such a form, but the impression is only caused by the concealment of the vast proportions of the mass behind, whose poise is quite unaffected by this hollowing at one point. Thenceforward, as we ascend the glacier, the Matterhorn every moment expands in apparent width; and having reached the foot of the Stockhi (about a four hours' walk from Zermatt), and getting the Cervin summit to bear S. 11-½° E., I made the drawing of it engraved opposite, which gives a true idea of the relations between it and the masses of its foundation. The bearing stated is that of the apparent summit only, as from this point the true summit is not visible; the rocks which seem to form the greatest part of the mountain being in reality nothing but its foundations, while the little white jagged peak, relieved against the dark hollow just below the seeming summit, is the rock marked g in [Fig. 33]. But the structure of the mass, and the long ranges of horizontal, or nearly horizontal, beds which form its crest, showing in black points like arrow-heads through the snow, where their ridges are left projecting by the avalanche channels, are better seen than at any other point I reached, together with the sweeping and thin zones of sandy gneiss below, bending apparently like a coach-spring; and the notable point about the whole is, that this under-bed, of seemingly the most delicate substance, is that prepared by Nature to build her boldest precipice with, it being this bed which emerges at the two bastions or shoulders before noticed, and which by that projection causes the strange oblique distortion of the whole mountain mass, as it is seen from Zermatt.

J. Ruskin.J. C. Armytage.
39. The Cervin, from the North-West.

§ 16. And our surprise will still be increased as we farther examine the materials of which the whole mountain is composed. In many places its crystalline slates, where their horizontal surfaces are exposed along the projecting beds of their foundations, break into ruin so total that the foot dashes through their loose red flakes as through heaps of autumn leaves; and yet, just where their structure seems most delicate, just where they seem to have been swept before the eddies of the streams that first accumulated them, in the most passive whirls, there the after ages have knit them into the most massive strength, and there have hewn out of them those firm grey bastions of the Cervin,—overhanging, smooth, flawless, unconquerable! For, unlike the Chamouni aiguilles, there is no aspect of destruction about the Matterhorn cliffs. They are not torn remnants of separating spires, yielding flake by flake, and band by band, to the continual process of decay. They are, on the contrary, an unaltered monument, seemingly sculptured long ago, the huge walls retaining yet the forms into which they were first engraven, and standing like an Egyptian temple,—delicate-fronted, softly colored, the suns of uncounted ages rising and falling upon it continually, but still casting the same line of shadows from east to west, still, century after century, touching the same purple stains on the lotus pillars; while the desert sand ebbs and flows about their feet, as those autumn leaves of rock lie heaped and weak about the base of the Cervin.

§ 17. Is not this a strange type, in the very heart and height of these mysterious Alps—these wrinkled hills in their snowy, cold, grey-haired old age, at first so silent, then, as we keep quiet at their feet, muttering and whispering to us garrulously, in broken and dreaming fits, as it were, about their childhood—is it not a strange type of the things which "out of weakness are made strong?" If one of those little flakes of mica-sand, hurried in tremulous spangling along the bottom of the ancient river, too light to sink, too faint to float, almost too small for sight, could have had a mind given to it as it was at last borne down with its kindred dust into the abysses of the stream, and laid, (would it not have thought?) for a hopeless eternity, in the dark ooze, the most despised, forgotten, and feeble of all earth's atoms; incapable of any use or change; not fit, down there in the diluvial darkness, so much as to help an earth-wasp to build its nest, or feed the first fibre of a lichen;—what would it have thought, had it been told that one day, knitted into a strength as of imperishable iron, rustless by the air, infusible by the flame, out of the substance of it, with its fellows, the axe of God should hew that Alpine tower; that against it—poor, helpless, mica flake!—the wild north winds should rage in vain; beneath it—low-fallen mica flake!—the snowy hills should lie bowed like flocks of sheep, and the kingdoms of the earth fade away in unregarded blue; and around it—weak, wave-drifted mica flake!—the great war of the firmament should burst in thunder, and yet stir it not; and the fiery arrows and angry meteors of the night fall blunted back from it into the air; and all the stars in the clear heaven should light, one by one as they rose, new cressets upon the points of snow that fringed its abiding-place on the imperishable spire?