Volcanoes: What They are and What They TeachJudd, John W. (John Wesley)
Science
Volcanoes: What They are and What They Teach
Judd, John W. (John Wesley)
Volcanoes
We have already considered the evidence pointing to the conclusion that
systems of volcanoes, like that of the Lipari Islands, are similarly
ranged along lines of fissures, and there is equally good ground for
believing that the great linear bands of volcanoes, which, as we
have seen, stretch for thousands of miles, have had their positions
determined by great lines of fissure in the earth's crust. While,
however, the smaller fissures, upon which rows of scoria-cones are
thrown up, seem to have been in many cases opened by a single effort
of the volcanic forces, the enormous fissures, which traverse so large
a portion of the surface of the globe, are doubtless the result of
numerous manifestations of energy extending over vast periods of time.
The greatest of these bands along which the volcanic forces are so
powerfully exhibited at the present day, is the one which stretches
from near the Arctic circle at Behring's Straits to the Antarctic
circle at South Victoria. The line followed by this volcanic band,
which, as we have seen, includes more than one half of the active
volcanoes of the globe, is a very sinuous one, and it gives off
numerous offshoots upon either side of it. The great focus of this
intense volcanic action may be regarded as lying in the district
between the islands of Borneo and New Guinea. From this centre there
radiate a number of great lines, along which the volcanic forces are
exhibited in the most powerful manner. The first of these extends
northwards through the Philippine Isles, Japan, the Kurile Islands, and
Kamtschatka, giving off a branch to the east, which passes through the
Aleutian Islands and the peninsula of Alaska. This band, along which
the volcanic forces are very powerfully active, is continued towards
the south-east in the New Britain, the Solomon Islands, Santa Cruz, the
New Hebrides, New Zealand, and South Victoria. East and west from the
great central focus there proceed two principal branches. The former
of these extends through the Navigator Islands and Friendly Islands
as far as Elizabeth Islands. The latter passes through Java, and then
turns north-westward through Sumatra, the Nicobar Islands, the Andaman
Islands up to the coast of Burmah.
The great band which we have been describing exhibits the most
striking examples of volcanic activity to be found upon the globe.
Besides the 150 or more volcanoes which are known to have been in a
state of activity during the historical period, there are several
hundred very perfect volcanic cones, many of which appear to have but
recently become extinct, if indeed, they are not simply in a dormant
condition. For long distances these chains of volcanic cones are almost
continuous, and the only very considerable breaks in the series are
those between New Zealand and the New Hebrides on the one hand, and
between the former islands and South Victoria on the other.
[Sidenote: GREAT VOLCANIC BANDS OF THE GLOBE.]
Public-domain text, read in full here on John Shaqi.
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