|
Main
- books.jibble.org
My Books
- IRC Hacks
Misc. Articles
- Meaning of Jibble
- M4 Su Doku
- Computer Scrapbooking
- Setting up Java
- Bootable Java
- Cookies in Java
- Dynamic Graphs
- Social Shakespeare
External Links
- Paul Mutton
- Jibble Photo Gallery
- Jibble Forums
- Google Landmarks
- Jibble Shop
- Free Books
- Intershot Ltd
|
books.jibble.org
Previous Page
| Next Page
Page 25
These are the essential facts of geyser display. There are very many
variations of performance in every respect, I have seen over twenty
geysers in almost jocular, and certainly in overwhelmingly magnificent,
activity.
"To him who in the love of nature holds
Communion with her visible forms, she speaks
A various language."
WHAT ARE THE CAUSES?
What is the power that can throw a stream of water two by six feet over
the tops of the highest skyscrapers of Chicago? It is heat manifested
in the expansive power of steam. Scientists have theorized long and
experimented patiently to read the open book of this tremendous
manifestation of uncontrollable energy. At first the form and action
of a teakettle was supposed to be explanatory. Everyone knows that
when steam accumulates under the lid it forces a gentle stream of water
from the higher nozzle. This fact was made the basis of a theory to
account for geysers by Sir George Mackenzie in 1811. But to suppose
that nature has gone into the teakettle manufacturing business to the
extent of thirty such kettles in a space of four square miles was seen
to be preposterous. So the construction theory was given up.
But suppose a tube (how it is made will be explained later), large or
small, regular or irregular, to extend far into the earth, near or
through any great source of heat resulting from condensation,
combustion, chemical action, or central fire. Now suppose this tube to
be filled with water from surface or subterranean sources. Heat
converts water, under the pressure of one atmosphere, or fifteen pounds
to the square inch, into steam at a temperature of two hundred and
twelve degrees. But under greater pressure more heat is required to
make steam. The water never leaps and bubbles in an engine boiler.
The awful pressure compels it to be quiet. A cubic inch of water will
make a cubic foot--one thousand seven hundred and twenty-eight times as
much--of steam under the pressure of one atmosphere. But under the
pressure of a column of water one thousand feet high, giving a pressure
of four hundred and thirty-two pounds to the square inch at the bottom,
water becomes steam, if at all, only by great heat. Every engineer
knows that the pressure exerted by steam increases by great geometrical
ratios as the heat increases by small arithmetical ratios. Steam made
by two hundred and twelve degrees exerts a pressure, as we have said,
of fifteen pounds.
To simply double the two hundred and twelve degrees of heat increases
the steam pressure twenty-three times.
Now suppose the subterranean tube or lake of Old Faithful to be freshly
filled with its million gallons of water. Sufficient heat makes steam
under any pressure. It rises up the tube and is condensed to water
again by the colder water above. Hence no commotion. But the whole
volume of water grows hotter for an hour. When it is too hot to absorb
the steam, and the tube is too narrow to let the amount made bubble up
through the water, it lifts the whole mass with a sudden jerk. The
instant the pressure of the water is taken off in any degree, the water
below, that was kept water by the pressure, breaks into steam most
voluminously, and the measureless power floods the earth and sky with
water and steam.
It is also known that superheated steam suddenly takes on such great
power that no boiler can hold it. Once let the water in a boiler get
very low and no boiler can hold the force of the resultant superheated
steam. The same heat that, applied to water, gives perfect safety,
applied to steam gives utter destruction. Hence the amazing force of
the vast jets of the geyser that follow the first spurts.
As soon as the steam is blown off the subterranean waterworks fill the
tube and the process is repeated.
This modus operandi was first proposed as a theory by Bunsen in 1846,
and later was demonstrated by the artificial geyser of Professor J. H.
J. Muller, of Freiburg.
[Illustration: Pulpit Terrace and Bunsen Peak.]
MOUNDS OF MINERAL DEPOSITS
I have the extremely difficult task of representing emotions by
words--glories of color and form seen by the eye by symbols meant to be
addressed to the ear. Before seeking to describe the diverse colors
made largely by one substance, let us remember that while silica, the
principal part of these water-built mounds, is one of the three parts
of granite, namely, the white crystal quartz, it is also the substance
of the beautifully variegated jasper, the lapis lazuli, the green
malachite, and the opal, with its cloudy milk-whiteness through which
flashes its heart of fire. Silica and alumina combine to make common
clay, but alumina forms itself into the red ruby, the golden-tinted
topaz, the violet oriental amethyst, the red, white, yellow, and violet
sapphire, and the beautiful green emerald. With substances of such
rare capabilities we may expect rich results in color and form.
Previous Page
| Next Page
|
|