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
52. And now with regard to the melting of ice. On the surface of
a flask containing a freezing mixture we obtain a thick fur of
hoar-frost. Sending the beam through a water-cell, its luminous waves
are concentrated upon the surface of the flask. Not a spicula of the
frost is dissolved. We now remove the water-cell, and in a moment a
patch of the frozen fur as large as half-a-crown is melted. Hence,
inasmuch as the full beam produces this effect, and the luminous part
of the beam does not produce it, we fix upon the dark portion the
melting of the frost.
53. As before, we clench this inference by concentrating the dark
waves alone upon the flask. The frost is dissipated exactly as it was
by the full beam.
54. These effects are rendered strikingly visible by darkening with
ink the freezing mixture within the flask. When the hoar-frost is
removed, the blackness of the surface from which it had been melted
comes out in strong contrast with the adjacent snowy whiteness. When
the flask itself, instead of the freezing mixture, is blackened, the
purely luminous waves being absorbed by the glass, warm it; the glass
reacts upon the frost, and melts it. Hence the wisdom of darkening,
instead of the flask itself, the mixture within the flask.
55. This experiment proves to demonstration the statement in
paragraph (36): that it is the dark waves of the sun that melt the
mountain snow and ice, and originate all the rivers derived from
glaciers.
There are writers who seem to regard science as an aggregate of
facts, and hence doubt its efficacy as an exercise of the reasoning
powers. But all that I have here taught you is the result of reason,
taking its stand, however, upon the sure basis of observation and
experiment. And this is the spirit in which our further studies are
to be pursued.
§ 6. _Oceanic Distillation._
56. The sun, you know, is never exactly overhead in England. But at
the equator, and within certain limits north and south of it, the sun
at certain periods of the year is directly overhead at noon. These
limits are called the Tropics of Cancer and of Capricorn. Upon the
belt comprised between these two circles the sun's rays fall with
their mightiest power; for here they shoot directly downward, and
heat both earth and sea more than when they strike slantingly.
57. When the vertical sunbeams strike the land they heat it, and the
air in contact with the hot soil becomes heated in turn. But when
heated the air expands, and when it expands it becomes lighter. This
lighter air rises, like wood plunged into water, through the heavier
air overhead.
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