My experiments with volcanoesJaggar, Thomas Augustus
Science
My experiments with volcanoes
Jaggar, Thomas Augustus
Geologists -- Biography; Volcanoes
In 1899 two things happened which affected the rest of my life. First,
Director Walcott asked me to furnish estimates for a Hawaii geologic
survey, a request which eventually led me to Hawaii. Second, the
Yakutat Bay earthquake snapped on an astonished world, though most of
the world didn’t know it.
The Yakutat Bay earthquakes in Alaska, in September 1899, were
accompanied by the pushing up of the bedrock shoreline by forty-seven
feet. Lowered beneath the sea were whole forests, on glacial deposits
pulled down by submarine landslips. It was an uninhabited region at
the foot of Mount St. Elias, along a fjord penetrating far into the
mountains. It came in line with the Aleutian trench, under the Pacific,
4,000 fathoms deep. The earthquakes lasted two weeks.
This colossal movement of blocks of the earth’s crust hundreds of miles
across gave one the impression that we knew little of what was going
on. Remembering that seventy-two percent of the earth’s surface is
covered by oceans and that less than ten percent is really inhabited, I
awoke to how much there was to learn. If whole forests and their roots
could float away into the Pacific currents, with all their plants and
animals and seeds and bacteria, what might not have occurred in past
ages, when such jostling of crust blocks was common.
But before I was to experiment with live volcanoes came a decade of
laboratory experiment.
CHAPTER II
Imitating Ripplemarks
“_The Constitution is an experiment,
as all life is an experiment._”
At the end of the century my experiments with the sclerometer, and with
the class in experimental geology, steered me for years into laboratory
experiment. Europe was headed toward geophysics and geochemistry,
meaning chiefly mathematical and statistical analysis. My vision was
nonmathematical, though I used pressures, temperatures, clocks, and
yardsticks to measure erosion, sediment, warping of strata, and melting.
This took me away from petrography, for the polarizing microscope was
dealing with infinite series of minerals and molecules. I could see
nothing but infinite penetration into the smaller and smaller. Clarence
King and Frank Perret had been on the way to infinite journeying
outward to the bigger and bigger.
The guiding formula was “erosion, sedimentation, deformation, and
eruption.” Measure these on the globe, imitate them with mud pies
in the laboratory. Compare the global examples with the mud pies.
Try to get the mud pies to illuminate the gigantic stream systems,
flood plains, sea bottoms, folded mountains, intrusions, and lavas
of the earth. Then try to measure in the field those processes with
observatories. So, to me, came the transition from collections to
experiments.
Public-domain text, read in full here on John Shaqi.
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