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
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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
The first explanation given of those veins by Professor Forbes was, that
they were small fissures formed in the ice by its motion; that these
were filled with the water of the melted ice in summer, which froze in
winter so as to form the blue veins. This is the explanation given in
his 'Travels,' page 377; and in a letter published in the 'Edinburgh New
Philosophical Journal,' October, 1844, it is re-affirmed in these
words:--"With the abundance of blue bands before us in the direction in
which the differential motion must take place (in this case sensibly
parallel to the sides of the glacier), it is impossible to doubt that
these infiltrated crevices (for such they undoubtedly are) have this
origin." This theory was examined by Mr. Huxley and myself in our joint
paper; but it has been since alleged that ours was unnecessary labour,
Prof. Forbes himself having in his Thirteenth Letter renounced the
theory, and substituted another in its place. The latter theory differs,
so far as I can understand it, from the former in this particular, that
the _freezing of the water_ in the fissures is discarded, their sides
being now supposed to be united "by the simple effects of time and
cohesion."[B] For a statement of the change which his opinions have
undergone, I would refer to the Prefatory Note which precedes the volume
of 'Occasional Papers' recently published by Prof. Forbes; but it would
have diminished my difficulty had the author given, in connexion with
his new volume, a more distinct statement of his present views regarding
the veined structure. With many of his observations and remarks I should
agree; with many others I cannot say whether I agree or not; and there
are others still with which I do not think I should agree: but in hardly
any case am I certain of his precise views, excepting, indeed, the
cardinal one, wherein he and others agree in ascribing to the structure
a different origin from stratification. Thus circumstanced, my proper
course, I think, will be to state what I believe to be the cause of the
structure, and leave it to the reader to decide how far our views
harmonize; or to what extent either of them is a true interpretation of
nature.
[Sidenote: USUAL ASPECT OF BLUE VEINS.]
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