My experiments with volcanoesJaggar, Thomas Augustus
Science
My experiments with volcanoes
Jaggar, Thomas Augustus
Geologists -- Biography; Volcanoes
The result was most remarkable. The yellow liquid lava went into the
salt water without making any column of steam at all; the sea bottom
simply received it with its rush downward, the water boiling superhot,
and the lava taking the water vapor into itself. The phenomenon was not
due to the rising of dry steam, for there was no condensation cloud
above. Scientists explained it by assuming a shell of lava making a
tunnel under the ocean, with the crust ending just at sea level.
Such a submarine arch was definitely not present, for the waves surged
back and forth and, Matsumoto states, there was no sign of a submerged
reef. The motion picture bears this out. What was probably going on
is what happens to slag in a patented process of the steel mills,
where the glow liquid is flowed over a perforated surface emitting
hundreds of water jets, and the melt at 1300° Centigrade absorbs the
water without making visible steam. The slag turns into a myriad of
microscopic glassy spheres, becoming a kind of pumice. A peculiarity
of this substance is that if it is cooled at 700° Centigrade it will
pass a critical point and give up the absorbed water with explosive
effects. It seems likely that Matsumoto’s golden torrent sweeping
into the ocean was so excessively hot that it took up the water and
continued to flow down the sea bottom as a water-charged product. The
snapping and crackling effects, and the submarine earthquakes, making
localized tidal waves such as those noted in 1919 when such a torrent
entered the sea, may be due to the explosive cooling when the slag
gives up its water.
The use of color motion pictures is one of the many improvements
owed to modern science, and the mapping of lava flows by airplane
photography. This gave Macdonald a new weapon for surveying the volume
accumulation at the time of the 1950 outflows, for from air photographs
he got exact outlines of the flows. These, checked against calculated
thicknesses, gave him volumes which could be compared with volumes of
older flows proportionate to areas. These calculations showed that
nothing since 1868 has yielded such large volumes of lava, per days of
outflow.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account