The Forms of Water in Clouds and Rivers, Ice and Glaciers — John Shaqi
The Forms of Water in Clouds and Rivers, Ice and GlaciersTyndall, John
Science
The Forms of Water in Clouds and Rivers, Ice and Glaciers
Tyndall, John
Clouds; Glaciers; Ice; Rivers; Water
130. We also see another glacier, or a portion of it, to the left,
falling apparently in broken fragments through a narrow gorge
(Cascade du Talèfre on the sketch) and joining the Léchaud, and from
their point of junction also a stripe of débris (_d_) runs downwards
along the Mer de Glace. Beyond this again we notice another stripe
(_e_), which seems to begin at the bottom of the ice-fall, rising
as it were from the body of the glacier. Beyond all of these we can
notice the lateral moraine of the Mer de Glace.
131. These stripes are the _medial moraines_ of the Mer de Glace. We
shall learn more about them immediately.
132. And now, having informed our minds by these observations, let
our eyes wander over the whole glorious scene, the splintered peaks
and the hacked and jagged crests, the far-stretching snow-fields, the
smaller glaciers which nestle on the heights, the deep blue heaven
and the sailing clouds. Is it not worth some labour to gain command
of such a scene? But the delight it imparts is heightened by the
fact that we did not come expressly to see it; we came to instruct
ourselves about the glacier, and this high enjoyment is an incident
of our labour. You will find it thus through life; without honest
labour there can be no deep joy.
§ 17. _The Talèfre and the Jardin. Work among the Crevasses._
133. And now let us descend to the Mer de Glace, for I want to take
you across the glacier to that broken ice-fall the origin of which we
have not yet seen. We aim at the farther side of the glacier, and to
reach it we must cross those dark stripes of débris which we observed
from the heights. Looked at from above, these moraines seemed flat,
but now we find them to be ridges of stones and rubbish, from twenty
to thirty feet high.
134. We quit the ice at a place called the Couvercle, and wind round
this promontory, ascending all the time. We squeeze ourselves through
the _Égralets_, a kind of natural staircase in the rock, and soon
afterwards obtain a full view of the ice-fall, the origin of which we
wish to find. The ice upon the fall is much broken; we have pinnacles
and towers, some erect, some leaning, and some, if we are fortunate,
falling like those upon the Glacier des Bois; and we have chasms from
which issues a delicate blue light. With the ice-fall to our right
we continue to ascend, until at length we command a view of a huge
glacier basin, almost level, and on the middle of which stands a
solitary island, entirely surrounded by ice. We stand at the edge of
the _Glacier du Talèfre_, and connect it with the ice-fall we have
passed. The glacier is bounded by rocky ridges, hacked and torn at
the top into teeth and edges, and buttressed by snow fluted by the
descending stones.
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