nd, too, by this strange irruption:

"One can form some idea of the altitude of this barrier of ice when it
is mentioned that from Hofdabrekka farm, which lies high up on a fjeld,
one could not see Hjorleifshofdi opposite, which is a fell six hundred
and forty feet in height; but in order to do so had to clamber up a
mountain slope east of Hofdabrekka twelve hundred feet high."

These things will help the reader to understand why it is that a man who
keeps company with glaciers comes to feel tolerably insignificant by
and by. The Alps and the glaciers together are able to take every bit of
conceit out of a man and reduce his self-importance to zero if he will
only remain within the influence of their sublime presence long enough
to give it a fair and reasonable chance to do its work.

The Alpine glaciers move--that is granted, now, by everybody. But there
was a time when people scoffed at the idea; they said you might as well
expect leagues of solid rock to crawl along the ground as expect leagues
of ice to do it. But proof after proof was furnished, and the finally
the world had to believe.

The wise men not only said the glacier moved, but they timed its
movement. They ciphered out a glacier's gait, and then said confidently
that it would travel just so far in so many years. There is record of
a striking and curious example of the accuracy which may be attained in
these reckonings.

In 1820 the ascent of Mont Blanc was attempted by a Russian and two
Englishmen, with seven guides. They had reached a prodigious altitude,
and were approaching the summit, when an avalanche swept several of the
party down a sharp slope of two hundred feet and hurled five of them
(all guides) into one of the crevices of a glacier. The life of one
of the five was saved by a long barometer which was strapped to his
back--it bridged the crevice and suspended him until help came. The
alpenstock or baton of another saved its owner in a similar way. Three
men were lost--Pierre Balmat, Pierre Carrier, and Auguste Tairraz. They
had been hurled down into the fathomless great deeps of the crevice.

Dr. Forbes, the English geologist, had made frequent visits to the Mont
Blanc region, and had given much attention to the disputed question of
the movement of glaciers. During one of these visits he completed his
estimates of the rate of movement of the glacier which had swallowed
up the three guides, and uttered the prediction that the glacier would