Geology: The Science of the Earth's CrustMiller, William J. (William John)
Philosophy
Geology: The Science of the Earth's Crust
Miller, William J. (William John)
Geology
Some idea of the quantitative geological importance of volcanism may be
conveyed to the reader when we assert that, according to a conservative
estimate, fully one-half of a million cubic miles of molten rocks have
been poured out upon the surface of the earth through volcanic action
in relatively recent geological time! The Cascade Range with its lofty
peaks, including Mount Shasta and Mount Rainier, each rising more than
14,000 feet above the sea, has been built up very largely by volcanic
action during the last era of geologic time. Many other mountain peaks
and various ranges have been similarly developed either wholly or in
part. The great chain of Aleutian Islands extending hundreds of miles
into the sea, is the scene of much volcanic activity where a great
mountain range is now literally being born out of the sea by the
processes of vulcanism.
Before this the reader has more than likely wondered about the source
of the heat, vapors (mainly water), and power involved in volcanic
action. Answers to these questions are closely tied up with the precise
cause (or causes) of volcanic action which remains one of the most
uncertain of the larger problems of geologic science. Before briefly
discussing the causes, a few additional facts should be stated. First,
in regard to the heat, a careful determination of the temperature
of the molten lava of Kilauea in 1911 showed it to be 1,260 degrees
Centigrade, or 2,300 degrees F. This is, however, a relatively low
temperature, because many lavas from other regions show melting points
all the way up to at least 2,000 degrees Centigrade (3,600 degrees
F.). Water in the form of steam is quantitatively one of the greatest
products of volcanoes. A fair idea of the tremendous volumes of water
involved may be gained from the statement that a careful estimate shows
that fully 460,000,000 gallons of water in the form of steam erupted
from a single secondary cone of Mount Etna during a period of 100
days. Among other gases which are given off in greater or less amounts
during volcanic activity are carbonic acid gas, sulphureted hydrogen,
sulphur dioxide, and hydrochloric acid. Some idea of the power back of
volcanoes may be gained not only from the tremendous explosions such
as those above described, but also from the fact that the pressure
necessary to raise the column of lava from sea level to the top of
Mauna Loa (nearly 14,000 feet) is about 1,150 atmospheres, or about
17,000 pounds per square inch. The actual pressure must there be much
greater because the lava is forced up from far below sea level.
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