From an Easy ChairLankester, E. Ray (Edwin Ray), Sir
History
From an Easy Chair
Lankester, E. Ray (Edwin Ray), Sir
Natural history; Science
The pressing of the high-lying snow, so as to form solid ice or
“glacier,” is concerned with the same property of snow as that
which enables us to make snow “bind” into a snowball. You cannot
make snowballs during very hard frost--the snow must be in air of a
thawing temperature at the moment it is squeezed by the hand. The hand
itself will not be warm enough to produce that temperature when the
thermometer is below freezing-point. The snow commences to melt in
the hand when one squeezes it, and then when the squeezing is stopped
the water formed quickly freezes again and cements the snow particles
together to form ice, enclosing innumerable minute bubbles. The heat
of the sun and the pressure of the weight of the snow itself take the
place in the mountains of the warmth and pressure of the human hand.
The minute air bubbles make the newest glacier-ice white and opaque,
especially when seen in a great mass; but gradually they get squeezed
together, and the glacier ice becomes first “fibrous” in appearance,
and then, after long years of pressure by its own weight, fairly clear.
Ice in great masses has the properties of a viscous body, like pitch
or soft sealing-wax, owing to the fact that wherever the solid mass
breaks its particles melt a very little and then freeze again. Under
increased pressure ice melts at a lower temperature than when it is not
subjected to pressure. When the pressure is removed the water freezes
again. Thus crushed ice or snow can be put into a “squeeze-mould” and
pressed, so as to form a solid mass of ice of any shape you may choose.
Four or five slabs of ice, placed one over the other, very soon become,
owing to this property, one continuous solid mass. White glacier ice
is so full of air bubbles as to be comparable in structure to sponge,
or, more closely, to cork. A cube of such ice exposes, owing to its
rough air-hole pitted surface, a much larger surface of contact to the
atmosphere than does a cube of perfectly smooth clear ice. Consequently
in a warm room or chamber the white ice melts much more quickly than
does the clear, and hence you should choose clear ice rather than
white ice if you wish for a block which will last.
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