Origins of Volcanoes

Here, the Guide in the book Etidorhpa describes the origin and nature of at
least some types of volcanoes:

" Know then, that the theories of man concerning volcanic eruptions, in
connection with a molten interior of the Earth, are such as are evolved in
ignorance of even the subsurface of the globe. The earth's interior is to
mankind a sealed chamber, and the wise men who elucidate the curious
theories concerning natural phenomena occurring therein are forced to draw
entirely upon their imagination. Few persons realize the paucity of data at
the command of workers in science. Theories concerning the earth are
formulated from so little real knowledge of that body, that our science may
be said to be all theory, with scarcely a trace of actual evidence to
support it. If a globe ten inches in diameter be covered with a sheet of
paper, such as I hold in my hand, the thickness of that sheet will be
greater in proportion to that of such a globe than the depth lnen have
explored within the earth is compared with the thickness of the crust of the
earth. The outer surface of a pencil line represents the surface of the
earth; the inner surface of the line represents the depth of man's
explorations; the highest mountain would be represented by a comma resting
on the line. The geologist studies the substances that are thrust from the
crater of an active volcano, aiid from this makes conjectures regarding the
strata beneath, and the force that casts the excretions out. The results
must with men, therefore, furnish evidence from which to explain the cause.
It is as though an anatomist would form his idea of the anatomy of the liver
by the secretion thrown out of that organ, or of the lung texture by the
breath and sputum. In fact, volcanoes are of several descriptions, arid
usually are extremely- superficial. This lake, the surface of which is but
one hundred and fifty miles underground, is the mother of an exceptionally
deep one. When the water pours over this ledge it strikes alt element below
us, the metallic base of salt, which lies in great masses in some portions
of the earth's crust. * Then alt immediate chemical reaction ensues, the
water is dissociated, intense heat results, part of the water combines with
the metal, part is vaporized as steam, while part escapes as an inflammable
gas. The sudden liberation of these gases causes an irregular pressure of
vapor on the surface of the lake, the result being a throbbing and
rebounding of the attenuated atmosphere above, which, in gigantic waves,
like swelling tides, dashes great volumes of water over the ledge beside us,
and into the depth below. This water in turn reacts on fresh portions of the
metallic base, and the reflex action increases the vapor discharges, and as
a consequence the chamber we are in becomes a gasholder, containing vapors
of unequal gas pressures, and the resultant agitation of the lake from the
turmoil continues, and the pulsations are repeated until the surface of the
lake is lowered to such a degree as at last to prevent the water from
overflowing the barrier. Finally the lake quiets itself, the gases slowly
disappear by earth absorption, and by escape from the volcanic exit, and for
an unrecorded period of time thereafter the surface of the lake continues to
rise slowly as it is doing now."
" But what has this phenomenon to do with the volcano?"

" It produces the eruption; the water that rushes down into the chasm,
partly as steam, partly as gas, is forced onward and upward through a
crevice that leads to the old crater of the presumed extinct but
periodically active Mount Epomeo. These gases are intensely heated, and they
move with fearful velocity. They tear off great masses of stone, which the
resultant energy disturbances, pressure, gas, and friction, redden with
heat. The mixture of gases from the decomposed water is in large amount, is
burning and exploding, and in this fiery furnace amid such convulsions as
have been described, the adjacent earth substance is fused, and even clay is
melted, and carried on with the fiery blast. Finally the current reaches the
earth's surface through the funnel passage, the apex of which is a
volcano-the blast described a volcanic eruption.""

ยทยทยท

To: Members

From: Dean

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Yes, I love this portion of the book. If you look into the elements that are found in volcanic material one might be surprised that they are quite high in alkaline metals. It seems that this very much verifies these details, yet who seems to care? Certainly not the scientific community. Think on this: NASA is purported to be seriously considering a plan to drill something like a 6 mile hole in order to artificially infuse water into the depths of Yellowstone in order to stop the super volcano from exploding. They believe that it will help to cool it off just like the natural geysers do. Wow, little do they know that this is likely the exact opposite of what they should be doing and will probably blow up the western United States and set the world into a nuclear winter style event.

The bottom line is that mainstream science doesn't consider all of the details that could possibly bring further light to the sciences.

ยทยทยท

On Fri, Sep 1, 2017 at 9:50 PM, [email protected] [ALLPLANETS-HOLLOW] [email protected] wrote:

To: Members

From: Dean

Here, the Guide in the book Etidorhpa describes the origin and nature of at
least some types of volcanoes:

" Know then, that the theories of man concerning volcanic eruptions, in
connection with a molten interior of the Earth, are such as are evolved in
ignorance of even the subsurface of the globe. The earth's interior is to
mankind a sealed chamber, and the wise men who elucidate the curious
theories concerning natural phenomena occurring therein are forced to draw
entirely upon their imagination. Few persons realize the paucity of data at
the command of workers in science. Theories concerning the earth are
formulated from so little real knowledge of that body, that our science may
be said to be all theory, with scarcely a trace of actual evidence to
support it. If a globe ten inches in diameter be covered with a sheet of
paper, such as I hold in my hand, the thickness of that sheet will be
greater in proportion to that of such a globe than the depth lnen have
explored within the earth is compared with the thickness of the crust of the
earth. The outer surface of a pencil line represents the surface of the
earth; the inner surface of the line represents the depth of man's
explorations; the highest mountain would be represented by a comma resting
on the line. The geologist studies the substances that are thrust from the
crater of an active volcano, aiid from this makes conjectures regarding the
strata beneath, and the force that casts the excretions out. The results
must with men, therefore, furnish evidence from which to explain the cause.
It is as though an anatomist would form his idea of the anatomy of the liver
by the secretion thrown out of that organ, or of the lung texture by the
breath and sputum. In fact, volcanoes are of several descriptions, arid
usually are extremely- superficial. This lake, the surface of which is but
one hundred and fifty miles underground, is the mother of an exceptionally
deep one. When the water pours over this ledge it strikes alt element below
us, the metallic base of salt, which lies in great masses in some portions
of the earth's crust. * Then alt immediate chemical reaction ensues, the
water is dissociated, intense heat results, part of the water combines with
the metal, part is vaporized as steam, while part escapes as an inflammable
gas. The sudden liberation of these gases causes an irregular pressure of
vapor on the surface of the lake, the result being a throbbing and
rebounding of the attenuated atmosphere above, which, in gigantic waves,
like swelling tides, dashes great volumes of water over the ledge beside us,
and into the depth below. This water in turn reacts on fresh portions of the
metallic base, and the reflex action increases the vapor discharges, and as
a consequence the chamber we are in becomes a gasholder, containing vapors
of unequal gas pressures, and the resultant agitation of the lake from the
turmoil continues, and the pulsations are repeated until the surface of the
lake is lowered to such a degree as at last to prevent the water from
overflowing the barrier. Finally the lake quiets itself, the gases slowly
disappear by earth absorption, and by escape from the volcanic exit, and for
an unrecorded period of time thereafter the surface of the lake continues to
rise slowly as it is doing now."
" But what has this phenomenon to do with the volcano?"

" It produces the eruption; the water that rushes down into the chasm,
partly as steam, partly as gas, is forced onward and upward through a
crevice that leads to the old crater of the presumed extinct but
periodically active Mount Epomeo. These gases are intensely heated, and they
move with fearful velocity. They tear off great masses of stone, which the
resultant energy disturbances, pressure, gas, and friction, redden with
heat. The mixture of gases from the decomposed water is in large amount, is
burning and exploding, and in this fiery furnace amid such convulsions as
have been described, the adjacent earth substance is fused, and even clay is
melted, and carried on with the fiery blast. Finally the current reaches the
earth's surface through the funnel passage, the apex of which is a
volcano-the blast described a volcanic eruption.""

1 Like