The Strange Adventures of a PebbleHawksworth, Hallam
Science
The Strange Adventures of a Pebble
Hawksworth, Hallam
Geology -- Juvenile literature; Physical geography -- Juvenile literature
When is a volcano dead? You never can tell. A volcano goes off when it
wants to, quite regardless of the fact that it has had the reputation
for a thousand years of being dead. And the worst of it is volcanoes
are like guns--only more so. A gun doesn't shoot any harder because
it wasn't supposed to be loaded; but the volcano, if it breaks out
unexpectedly, is violent in proportion to the length of time it has
been apparently dead. This is the reason. The original vent becomes
plugged up with the cooled lava. This plug being harder than the rest
of the mountain, the next outbreak is forced to take a new course,
and the longer the forces of explosion are held back the greater the
accumulation of energy and the more violent the discharge.
But why do volcanoes go off at all? Why can't they be quiet and
well-behaved like other mountains? Nobody knows for sure. On one thing
all scientific men seem to be now agreed; namely, that while the rocks
inside the earth are hot enough to melt they are hard as steel, owing
to the tremendous pressure of the rocks above them, and one theory
about volcanic eruptions is that they are caused by the release of the
pressure on this rock in one place and a pressing down in another, as
the earth's crust settles and crumples around the centre. Some of this
rock--that on which the pressure is released--melts and rises under the
folds of rising rock, and so makes the granite hearts of the greater
mountains. Some of it wells up through the cracks in the rock and
spreads in lava fields, while some of it gushes up and explodes at the
points where cracks cross and so make volcanoes.
This is one theory, but there are others. The latest is so big that we
will have to take it into the mind in sections.
THE LATEST THEORY OF ERUPTIONS
1. Imagine the interior of the earth divided into three zones. The
central zone, of course, is the hottest. Between this central zone and
the zone reaching down forty miles or so from the surface is a middle
zone. (Think of a doughnut ball inside a doughnut ring, with space
between the ball and ring. That will give you the idea.)
2. From what is known of the laws of heat it is assumed that the flow
of heat from the central to the middle zone is greater than the loss of
heat from the central to the outer zone. Thus the heat income of the
middle zone would constantly exceed its outlay, and so it would get
hotter and hotter.
[Illustration: THE MYSTERIOUS SHAFT OF MOUNT PELÉE
In 1902, after the first explosion, Mount Pelée continued its
eruptions for several months, and in the late stages there slowly
rose, through the crater, this strange shaft of red-hot lava,
like a great iron beam forged by giant hammers in Vulcan's famous
blacksmith-shop. As it rose it crumbled and finally fell to pieces.
It was forced up by the gases beneath and shaped by the crater
through which it came; but can you conceive of anything more weird
and awesome?
]
Public-domain text, read in full here on John Shaqi.
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