[Ice-Caves of France and Switzerland by George Forrest Browne]@TWC D-Link book
Ice-Caves of France and Switzerland

CHAPTER I
13/19

There had been a very large amount of rain, and the surface of the rock in the fissures was evidently wet; so I have no doubt that the filtering through of the warm rain-water had thawed the upper supports of the ice-cascades, and then, owing to their slightly inclined position, the pedestal had not provided sufficient support, and so they had fallen.

One of them, perhaps, had brought down in its fall the free column, which had stood two days before on its own base, without any support from the rock.

Very probably, too--indeed, almost certainly,--the fall of the large mass of rock, which once formed the bottom of the basin on the north side of the road, has affected the old-established fissures, by which rain-water has been accustomed to penetrate in small quantities to the glaciere, so that now a much larger amount is admitted.

On this account, there will probably be a great diminution of the ice in the course of future summers, though the amount formed each winter may be greater than it has hitherto been.

Constant examination of other columns and fissures has convinced me, that, before the end of autumn, the majority of the glacieres will have lost all the columns which depend upon the roof for a part of their support, or spring from fissures in the wall; whereas those which are true stalagmites, and are self-supporting, will have a much better chance of remaining through the warm season, and lasting till the winter, and so increasing in size from year to year.


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