The Schafloch does not take its name from the bones contained in it, as is the case with the Kuehloch in Franconia,[58] but from the fact that when a sudden storm comes on, the sheep and goats make their way to the cave for shelter, never, I was told, going so far as the commencement of the ice.  The entrance faces ESE., and is of large size, with a low wall built partly across it to increase the shelter for the sheep:  Dufour calls the entrance 50 feet wide and 25 feet high, but I found the width at the narrowest part, a few yards within the entrance, to be 33 feet.[59] For a short distance the cave passes horizontally into the rock, in a westerly direction, and is quite light; it then turns sharp to the south, the floor beginning to fall, and candles becoming necessary.  Here the height increases considerably, and the way lies over a wild confusion of loose masses of rock, which have apparently fallen from the roof, and make progression very difficult.  We soon reached a point where ice began to appear among the stones; and as we advanced it became more and more prominent, till at length we lost sight of the rock, and stood on solid ice.

On either side of the cave was a grand column of ice forming the portal, as it were, through which we must pass to further beauties.  The ice-floor rose to meet these columns in a graceful swelling curve, perfectly continuous, so that the general effect was that of two columns whose roots expanded and met in the middle of the cave; and, indeed, that may have been really the order of formation.  The right-hand column was larger than its fellow, but, owing to the more gradual expansion of the lower part of its height, and the steepness of the consequent slope, we were unable to measure its girth at any point where it could be fairly called a column.  Christian had been in the cave a few days before, and he assured me that the swelling base of this column had increased very considerably since his last visit, pointing out a solid surface of ice, at one part of our track, where he had before walked on bare rock.  The cave was by no means extremely cold, that is to say, it was rather above than below the freezing point, and the splashing of drops of water was audible on all sides; so that, if Christian spoke the truth,—­it was sad to be so often reminded of Legree’s plaintive soliloquy in the opening pages of ’Uncle Tom’s Cabin,’—­the explanation, I suppose, might be that the drops of water, falling on the top of the column or stalagmite, run down the sides, and carry with them some melted portion from the upper part of the column, and after a course of a few yards become so far refrigerated as to form ice.[60] The pillar on the left was more approachable, but we were unable to determine its dimensions; for on the outer side, where it stood a few feet or yards clear of the side of the cave, the rounded ice at its foot fell off at once into a dark chasm, a sort of smooth enticing Bergschrund, which we did not care to face.  Christian declared that this column was not so high as it was a day or two before, which may go to support the theory expressed above, or at least that part of it which depends upon the supposition of water dropping on to the head of the column, and melting certain portions of it.