The Glaciers of the Alps: Being a narrative of excursions and ascents, an account of the origin and phenomena of glaciers and an exposition of the physical principles to which they are relatedTyndall, John
Science
The Glaciers of the Alps: Being a narrative of excursions and ascents, an account of the origin and phenomena of glaciers and an exposition of the physical principles to which they are related
Tyndall, John
Alps -- Description and travel; Glaciers -- Alps
Were the statements of some writers upon this subject well founded, or
were the dirt-bands as drawn upon the map of Professor Forbes correctly
shown, this explanation could not stand a moment. It has been urged that
the dirt-bands cannot thus belong to a single tributary of the Mer de
Glace; for if they did, they would be confined to that tributary upon
the trunk-glacier; whereas the fact is that they extend quite across the
trunk, and intersect the moraines which divide the Glacier du Geant from
its fellow-tributaries. From my first acquaintance with the Mer de Glace
I had reason to believe that this statement was incorrect; but last year
I climbed a third time to the Cleft-station for the purpose of once more
inspecting the bands from this fine position. I was accompanied by Dr.
Frankland and Auguste Balmat, and I drew the attention of both
particularly to this point. Neither of them could discern, nor could I,
the slightest trace of a dirt-band crossing any one of the moraines.
Upon the trunk-stream they were just as much confined to the Glacier du
Geant as ever. If the bands even existed east of the moraines, they
could not be seen, the dirt on this part of the glacier being sufficient
to mask them.
The following interesting fact may perhaps have contributed to the
production of the error referred to. Opposite to Trelaporte the eastern
arms of the dirt-bands run so obliquely into the moraine of La Noire
that the latter appears to be a tangent to them. But this moraine runs
along the Mer de Glace, not far from its centre, and consequently the
point of contact of each dirt-band with the moraine moves more quickly
than the point of contact of the western arm of the same band with the
side of the valley. Hence there is a tendency to _straighten_ the bands;
and at some distance down the glacier the effect of this is seen in the
bands abutting against the moraine of La Noire at a larger angle than
before. The branches thus abutting have, I believe, been ideally
prolonged across the moraines.
[Illustration: Fig. 38. Plan of Dirt-bands taken from Johnson's
'Physical Atlas.']
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