Some Salient Points in the Science of the EarthDawson, John William, Sir
Science
Some Salient Points in the Science of the Earth
Dawson, John William, Sir
Geology; Paleontology
The Arve, which drains the glaciers of the north side of Mont Blanc,
carries its burden of mud into the Rhone, which sweeps it, with the
similar material of many other Alpine streams, into the Mediterranean,
to aid in filling up the bottom of that sea, whose blue waters
it discolours for miles from the shore, and to increase its own
ever-enlarging delta, which encroaches on the sea at the rate of about
half a mile per century. The upper waters of the Rhone, laden with
similar material, are filling up the Lake of Geneva; and the great
deposit of "loess" in the alluvial plain of the Rhine, about which Gaul
and German have contended since the dawn of European history, is of
similar origin. The mass of material which has thus been carried off
from the Alps, would suffice to build up a great mountain chain. Thus,
by the action of ice and water--
"The mountain falling cometh to naught,
And the rock is removed out of its place."
Many observers who have commented on these facts have taken it for
granted that the mud thus sent off from glaciers, and which is so
much greater in amount than the matter remaining in their moraines,
must be ground from the bottom of the glacier valleys, and hence have
attributed to these glaciers great power of cutting out and deepening
their valleys. But this is evidently an error, just as it would be
an error to suppose the flour of a grist mill ground out of the mill
stones. Glaciers, it is true, groove and striate and polish the rocks
over which they move, and especially those of projecting points and
slight elevations in their beds; but the material which they grind up
is principally derived from the exposed frost-bitten rocks above them,
and the rocky floor under the glacier is merely the nether mill stone
against which those loose stones are crushed. The glaciers, in short,
can scarcely be regarded as cutting agents at all, in so far as the
sides and bottoms of their beds are concerned, and in the valleys which
the old glaciers have abandoned, it is evident that the torrents which
have succeeded them have far greater cutting power.
Public-domain text, read in full here on John Shaqi.
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