My experiments with volcanoesJaggar, Thomas Augustus
Science
My experiments with volcanoes
Jaggar, Thomas Augustus
Geologists -- Biography; Volcanoes
By 1918 and 1919 the pit was full and overflowing the Kilauea floor.
During the whole of 1919 Halemaumau, as a pit, was obliterated by its
dome of fill. In autumn the south flank of Mauna Loa broke out again,
into a flood of lava that reached the sea in South Kona. Remembering
1916, we predicted that, even though Halemaumau was full to the brim,
the sinking away of Mauna Loa lava would pull down Kilauea lava
suddenly, like a siphon. Exactly this happened on November 28, 1919.
During the night the crags, the clover-leaf lake, and the bulging
dome of the lava fill above Halemaumau’s edge went down as a cylinder
to a depth of 400 feet in two or three hours leaving incandescent
avalanching walls, a gratifying confirmation of theory.
As in 1916, the Halemaumau lava immediately returned to the bottom of
the pit, and lifted itself thirty feet a day for three weeks, so that
in December it was a violently boiling ringshaped puddle, surrounding
a horseshoe of crags with a quiet inner lagoon and resembling a coral
atoll. The Kilauea floor, which is dome-shaped outside of Halemaumau,
split open radially to the south, made floods of lava into the Kilauea
Crater wall valley, and even escaped out into the Kau Desert. This was
extended into a mountain crack, making flank lava flows of Kilauea
Mountain, nine miles away to the southwest, something which had not
happened since 1823 and 1868. Concentric craters like Kilauea caldera
and Halemaumau pit are thus ring-in-ring, or cup-in-cup, structures
by means of slag heapings over a deep fracture in the rock crust, the
circularity determined by occasional central sinking.
This circularity has sometimes reached perfection. In 1894 and 1909
the liquid pool inside Halemaumau, by steady welling up about a
central hole, became perfectly circular within a circumferential
rampart of overflow. This is a rare condition dependent on steadiness
of upwelling, temperature, and viscosity. It is important because it
shows how the perfect circles, and rampart cauldrons, were made on the
moon, where there are also angular calderas of subsidence like Kilauea
Crater. Evidently gas heating and liquidity changed on the moon, just
as it has done in Hawaii. The sources there are over cracks, as in
Hawaii. The analogies are so complete in these and many other ways that
I completely disbelieve in meteor impact for the moon craters. The moon
awaits a complete comparison with active terrestrial basaltic lavas,
by a modern volcanologist.
Public-domain text, read in full here on John Shaqi.
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