My experiments with volcanoesJaggar, Thomas Augustus
Science
My experiments with volcanoes
Jaggar, Thomas Augustus
Geologists -- Biography; Volcanoes
The liquid phase took an unusual fountain form, resembling that of
Mauna Loa in Hawaii, and nine spells of bright incandescent explosive
fountaining occurred. The collapse began on March 13; the fountaining
occurred during March 20 to 22, with jets of bright liquid lava and
flames, 1,000 to 3,000 feet high; and the crater became a lava lake.
The flames were occasioned by hydrogen within the lava itself, and
perhaps some carbon gases. This liquid fountaining phase was the
culmination of explosions, making pumice, with water vapor the gaseous
product. Ash fell four feet deep three miles away, and some fell on the
Adriatic coast. Both white steam clouds and black ash clouds arose with
the fountains, white and black side by side.
The net effect was to leave a bowl 1,500 feet in diameter and 800 feet
deep, floored with avalanche gravel. This reconstructed the funnel
of 1906, and as in 1906, the height of the rim was 4,100 feet after
eruption. In other words, the thirty-eight years had filled the vast
crater, only to have 1944 engulf and eject the contents, and strew them
down the slopes, adding an immense weight to the outer shell of the
cone.
A hundred million cubic yards of lava was poured out, and 50 million
cubic yards of ash now lie on the volcano. Three times as much was
carried far away, and the volume of gases was ten times as great.
The rock fragments, probably 200 times as great, were engulfed by
avalanches.
The big achievement of an eruption is to wedge open a mountain, let
the internal lava effervesce and go down, admit ground water, and make
spectacular fireworks of burning gas and meltings. Release of pressure
by splitting open the crust permits a great show of fiery foaming,
but no geologist sees the profound accomplishment of lava sinking
and flowing away by underground channels. It may flow out along the
Mediterranean Sea bottom. At Vesuvius, it may slip through deep cracks
in the direction of Sicily.
Certainly a periodic adjustment of the big system
(Vesuvius-Stromboli-Etna) has taken place deep down in the earth, and
the thirty-eight years of accumulation mean a stress by weighting down.
The pressure of 100 million tons of stored lava inside a weak cone
mountain and ready to effervesce with heat and give up its hydrogen is
what science too often forgets.
Public-domain text, read in full here on John Shaqi.
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