Curiosities of Olden TimesBaring-Gould, S. (Sabine)
History
Curiosities of Olden Times
Baring-Gould, S. (Sabine)
Curiosities and wonders
from north to south, and as they were bearing to the east they had to
cross every one of them. Most were filled with water which overflowed the
glacier, and disappeared in the snowdrift, and in some places they rode
through the water on the ice. None of these rifts were too broad to be
crossed in one place or another, either higher up the glacier towards the
south, or at its lower and north end. If they had met with a rift which
they could not pass, they intended to have made a snow-bridge over it,
rather than return. In this way they crossed the ice of the glacier. Next
came another bed of snow, over which they rode for some while; but it was
very heavy, as the day was exceedingly warm and mild.
“When they were within a short distance of what seemed to them to be the
highest point of the glacier on the east, a mist set in on both sides from
the north and south, leaving a clear space towards the east, so that they
could see the bright sky exactly opposite their faces; and the reason of
this was that the mountains rose on either side, leaving a sort of
depression between them, along which they were going as they held on due
east. This was not discouraging, as it showed that the mountain peaks
caught the mist, and left the lower ground clear. At the same time, they
heard the rush of water beneath their feet without being able to see the
stream. The noise indicated a volume much larger than that which they had
seen pouring through the ravine, and they conjectured that the sub-glacial
river divided into several streams before discharging itself.
“They now passed from the snow to a gravelly soil, devoid of grass. It was
a smooth ridge of sandstone, like the bank of a mountain torrent. The
glaciers now sloped towards the north-east, whilst some tended towards the
east; but right across the glaciers there lay a hollow trough, and in many
places along the edge black rocks shot out of the snow. On the north side
were lofty and craggy fells, connected by snowdrifts and strips of shale;
and the glacier range rose considerably on the north side.
Public-domain text, read in full here on John Shaqi.
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