Italian Alps. Freshfield Douglas William

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СКАЧАТЬ ambition, however, had never soared to such a conquest, and we were content to discuss a matter nearer at hand, the upper ice-fall which separated us from the supposed pass. Opinions differed; François prophesied difficulties and five hours' work to the top; a sanguine spirit set it down as half an hour's walk. The rope was soon put on, and we prepared to face the unknown.

      I presume everyone who cares to take up these sketches has already felt sufficient interest in the Alps to endeavour to realise, even if he has not seen, the nature of an ice-fall. If he has not, he had better go and look at Mons. Loppé's pictures. No word-painting can give an idea of anything so unlike the usual phenomena of our temperate zone. A cream-cheese at once squeezed and drawn out, so that the surface split and isolated blocks stood up, might, if viewed through a magnifying glass, slightly resemble in form, though not in colour, the contorted ice. But the imagination would have to look on from the point of view of the smallest mite.

      The lower ice-falls differ considerably from the highest. In one case the material is hard ice; in the other, closely compacted snow. In the ice the rifts are longer, narrower and more frequent, and fewer towers rise above the general level; the snow or névé opens in wider but less continuous chasms, sinks in great holes like disused chalk-pits, and throws up huge blocks and towers, which the sun slowly melts into the most fantastic shapes. The higher fall is generally both the most imposing and formidable to look at, and the easiest to get through. The maze here is less intricate, and the very size of its features makes it easier to choose a path. But it is unsafe to shout before you are well out of the wood. At the very top, where the strain caused by the steepening slope first cracks the glacier, one huge rent often stretches across from edge to edge, and unless Providence throws a light causeway or a slender arch across the gulf, there will be work for the ice-axe before you stand on the upper edge. Some crack in the pit's wall must be dug into steps, the huge disorderly blocks which make a floor must be got through, and then escape must be found in the same way that entrance was made, by a ladder of your own contriving. Such a passage may often cost an hour's hard work.

      The Bondasca Glacier above where we struck it was riven by a network of small crevasses. Some could be jumped, and the larger clefts were generally bridged, and thanks to a sharp night's frost the arches were in good bearing order. With occasional step-cutting and frequent zigzags we got clear of the thickest labyrinth and stood victorious on the upper snow-fields. They rose before us in a succession of frozen banks to a well-defined gap flanked by two snow hummocks. The western was connected by a long curtain of rock with the Punta Trubinesca. After skirting the highest snow-bowl, we crossed the deep moat which marks the point where the true mountain-form rises out of the folds of its snowy vestment, and in a moment more stood on the crest of a curling wave, fringed with icicles for spray.

      Where we had expected to see only the rock-surrounded basin of the Val dei Bagni, we looked down on a deep, long valley, running southwards towards the Val Tellina.

      At the second glance our eyes were caught by an enormous object lying in the centre of a grassy meadow. We were at once assured as to the identity of the valley. The block could be nothing else than the 'natural curiosity' of Val Masino, the biggest boulder in the Alps. Its dimensions are given by Mr. Ball as – 'Length, 250 feet; breadth, 120 feet; height, 140 feet;' or as tall as an average church tower, and large enough to fill up many a London square. Legend has nothing to tell about this monstrous block, and we are left to determine as we like, whether it fell from some neighbouring mountain going to ruin in the course of nature, or was dropped by the devil, on one of those errands of mischief which are always so fortunately interrupted by the opportune appearance of the pious peasant.

      We had only been two hours from our last resting-place, and the day was still young, so that we could well afford a halt. As there are some tourists whose chief object is to get to the end of their tours, so there are climbers who throughout the day seem to long only to arrive in as few hours as possible at the end of it. But peaks and passes and not inns were our goal, and we had no desire to hurry on. We chose a warm corner in the sun-facing rocks, whence by lifting our heads we looked over intervening ridges to the Alps of Glarus, and raked the Punta Trubinesca and its neighbours, now viewed end on, as weird a pile of granite as I have seen in many a long day's wanderings.

      From the snow-dome on our right a lofty and extraordinarily jagged ridge stretched out at right angles to the main chain, the barrier, probably, between the two branches of Val Masino.16 I wanted to climb the dome and reconnoitre, but clouds had partially covered the blue sky, and were whisking, now one way now the other, as the gust took them, as if playing a wild game of hide-and-seek amongst the granite towers. A storm seemed probable, and François thought it foolish to waste time.

      We were clearly not on the legendary Passo di Bondo,17 but on another 'Col' of our own contriving, leading somewhere into the Val di Mello, the eastern branch of Val Masino. The descent looked practicable. Why not attempt it and complete the pass? The distance to be retraced along the valley to our sleeping quarters, the 'Bagni,' could scarcely be worth considering. So after erecting a solid stoneman, and trusting him with the usual card-filled bottle, we set out.

      The last man had not set foot on the ice when François disappeared to his shoulders beneath the surface. Looking through the hole he had made we could appreciate the use of the rope. A dark green chasm, some thirty feet wide, yawned beneath us, its depths scarcely visible in the light thus suddenly let in upon them. The glacier we were descending fell away steeply, and became so broken and troublesome that we tried the rocks on the left. The change was for the worse, and we soon came back and cut our way through the difficulties.

      As soon as the rocks ceased to be precipitous we took to them again. But they were not pleasant footing. We found ourselves committed to a slope of boulders so shockingly loose that the slightest provocation sent half-a-dozen rolling from under our feet, and piled at so high an angle that when once started they bounded away at a pace which promised to take them straight to the valley. In such places an impetuous companion always insists on stopping to take off his gaiters and then following at a run. You have scarcely missed him before his return is announced by a whole volley of grape rattling about your ears, while a playful shout warns you to make way for a 100-pounder boulder which is ricochetting down on your heels with the force of a cannon-ball. Then your friend comes up with a pleased air, as much as to say, 'Didn't I come down that well?' and it is hard not to remonstrate with him in language the use of which should be restricted to divines.

      Halting beside some water which filtered out at the foot of the boulders, we enjoyed a beautiful view of the Disgrazia and the wild range behind us. On our right was a long comb, whose teeth had been tortured by time and weather into all sorts of quaint shapes; one rock bent over like a crooked finger, in another place a window was pierced through the crest. At a hasty glance one might have compared the fantastic shapes to those assumed so frequently by dolomitic limestone, but closer observation showed the tendency to curving outlines and to sharpness of edge peculiar to crystalline rock. In the dolomite districts the separate crags, cut up as they may be by flaws at right angles to the lie of the strata, have not, except from considerable distances, the same flamelike outlines. In any near view the layers of which they are built up become conspicuous, and often, as in the Brenta chain, have all the appearance of courses of masonry.

      Bearing to the left from the first huts on the Alpe di Ferro, we crossed a stream just below a tempting pool, in which five minutes later we were all plunging. At the next step in the descent our path re-crossed the water, and zigzagged steeply down the hillside, which was covered with broom and Scotch heather. Passing a succession of pretty cascades, we entered the Val di Mello, near a group of châlets, whence a stony mule-road led us in half an hour to San Martino, the village situated at the fork of the valley. It is a cluster of untidy stone houses, with nothing to delay the passer-by except a douanier's bureau and a tobacco store.

      We now met a car-road running up the Val dei Bagni – the western fork of the valley. The floor of the glen soon rises СКАЧАТЬ