Earth Features and Their Meaning: An Introduction to Geology for the Student and the General ReaderHobbs, William Herbert
Science
Earth Features and Their Meaning: An Introduction to Geology for the Student and the General Reader
Hobbs, William Herbert
Geology; Physical geography
When the writer visited the island some months later, the eruption was
still so vigorous that the crater could not be reached. The ruined
villa, smashed and charred, stood with its walls half buried in ash and
lapilli, among which were partly smashed pumiceous lava projectiles.
The entire _atrio_ about the mountain lay buried in cinder to the depth
of several feet and was strewn with projectiles which varied in size
from a man’s fist to several feet in diameter (Fig. 114). The larger of
these exhibited the peculiar “bread-crust” surface and had generally
been smashed by the force of their fall after the manner of a pumpkin
which has been thrown hard against the ground. One of these projectiles
fully three feet in diameter was found at the distance of a mile and
a half from the crater. Though diminished considerably in intensity,
the rhythmic explosions within the crater still recurred at intervals
varying from four minutes to half an hour, and were accompanied
by a dull roar easily heard at Lipari on a neighboring island six
miles away. Simultaneously, a dark cloud of “smoke”, the peculiar
“cauliflower cloud” or _pino_ mounted for a couple of miles above the
crater (Fig. 115), and the rise was succeeded by a rain of small lava
fragments or _lapilli_ outside the crater rim.
[Illustration:
FIG. 115.—Peculiar “cauliflower cloud” or _pino_ composed of steam and
ash, rising above the cinder cone of Volcano during the waning phases
of the explosive eruption of 1888 (after a photograph by B. Hobson).]
There seems to be no good reason to doubt that Vulcanian cinder
eruptions of this type differ chiefly in magnitude from the rhythmic
explosion within the crater of Stromboli, if we except the elevation of
a considerable quantity of accessory and older tuff which is derived
from the inner walls of the crater and carried upward into the air
together with the pasty cakes of fresh lava derived from the chimney.
It is this accessory material which gives to the _pino_ its dark or
even black appearance.
[Illustration:
FIG. 116.—Double explosive eruption of Taal volcano on the morning of
January 30, 1911.]
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