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
We have here supposed the water of the lake to be at rest, and the
liquid vein or the solid rod to move through it; but precisely the same
effect is produced if we suppose the rod at rest and the liquid in
motion. Let a post, for example, be fixed in the middle of a flowing
river; diverging from that post right and left we shall have lines of
ripples exactly as if the liquid were at rest and the post moved through
it with the velocity of the river. If the same post be placed close to
the bank, so that _one_ of its edges only shall act upon the water,
diverging from that edge we shall have a _single_ line of ripples which
will cross the river obliquely towards its centre. It is manifest that
any other obstacle will produce the same effect as our hypothetical
post. In the words of Professor Forbes, "the slightest prominence of any
kind in the wall of such a conduit, a bit of wood or a tuft of grass, is
sufficient to produce a well-marked ripple-streak from the side towards
the centre."
[Sidenote: MEASURE OF DIVERGENCE OF RIPPLES.]
The foregoing considerations show that the divergence of the two lines
of ripples from the central post, and of the single line in the case of
the lateral post, have their mechanical element, if I may use the term,
in the experiment of the Messrs. Weber. In the case of a swimming duck
the connexion between the diverging lines of ripples and the propagation
of rings round a disturbed point is often very prettily shown. When the
creature swims with vigour the little foot with which it strikes the
water often comes sufficiently near to the surface to produce an
elevation,--sometimes indeed emerging from the water altogether. Round
the point thus disturbed rings are immediately propagated, and the
widening of those rings is _the exact measure of the divergence of the
ripple lines_. The rings never cross the lines;--the lines never retreat
from the rings.
[Sidenote: RIPPLES AND VEINS DUE TO DIFFERENT CAUSES.]
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