My experiments with volcanoesJaggar, Thomas Augustus
Science
My experiments with volcanoes
Jaggar, Thomas Augustus
Geologists -- Biography; Volcanoes
Why thirty-four years? A third of a century? Three times the sunspot
interval? The previous steamblast explosion of Vesuvius before 1906 had
been in 1872. In the case of Mount Pelée and Soufrière the intervals
since past explosions had been fifty-one years and ninety years. But
it should be pointed out that the Carib volcanoes had two years of
terrifying rumblings, odors, and quakes just before 1902. Groundwater
exists in large volume under all three volcanoes. Soufrière, Pelée and
Vesuvius all began the steamblasts with collapsing craters, that is,
with internal lava going down into the bowels of the earth. The lava
usually showed in Vesuvius, whereas at Pelée and Soufrière it merely
made fumaroles, or gas vents. Man, a mere microbe, could make nothing
of hot sulfurous cracks.
On April 25 the electric train slowly pushed us up as far as the
observatory station, beyond which all was destroyed. Outside Naples
the fields were covered with two inches of gray-green dust, and pines
and palms were loaded with a two or three foot drift of sand. Near
the observatory a heavy six-inch mantle of sand and dust buried the
lava fields. The Vesuvian cone was covered with straight sand slides,
whitish gray, which occasionally slipped downward. The landscape was
shrouded in drifts of white ashes revealing obscurely the slaggy
contortions of lava beneath. Pure white steam boiled up from the cavity
in the peak, surrounded by an older rain cloud, like a hat on the
volcano’s crown.
My companions--Dr. Tempest Anderson and Messrs. Yeld and Brigg--were
all from Yorkshire. We started the ascent of the twenty-nine degree
slope in a strong west wind. The steam settled down on the summit, than
alternated with clear spells. We followed the west profile of the cone
straight up, noting how the funicular rails were twisted by landslides.
Everything was covered with pebbles, sand, and dust, with here and
there large fragments up to five feet across. We found solid footing on
the radial elevations of either scoured old lava or packed fragments.
The gullies were filled with deep sand.
Public-domain text, read in full here on John Shaqi.
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