My experiments with volcanoesJaggar, Thomas Augustus
Science
My experiments with volcanoes
Jaggar, Thomas Augustus
Geologists -- Biography; Volcanoes
The recent notion that radioactivity heat is in the outer shell denies
contraction of the inner earth. Furthermore, I do not believe in a
shallow underlayer of lava fifty or less miles down and capable of
flowing horizontally under shifting weight. I do believe in a deep
underlayer of fluid 1,800 miles down, under a block-faulted crust.
This fluid core adjusted itself to the ocean-bottom blocks originally,
making the upright slices moving-down controllers of the Appalachian
basin. There is no proof that sediment weight did it. It is more likely
that igneous, or fire-made, lava, as the thick outer armor plate of
the globe erupted in acts of intrusion, lubricated the vertical slices.
Intrusions are under every sedimentary mountain range on earth. It is
more likely that an agelong up of ridge fault blocks and a down of the
basin fault blocks decided where the central continental basin should
be, all of it well within the permanent side ridges of North America.
For this was a continental mediterranean sea, and the warping of its
highland of Philadelphia and its basin of Cincinnati was a mere episode
in the 2,000 million year history of Atlantic and Pacific borders of
the continent. The sinking of the intracontinental sea, relative to
the staying up of the highlands, was a wave in the history of globe
and core. Erosion and deposition were results, not causes. They were
results of the volcanic history of the ever moving active mosaic of the
globe. The permanent North America remained high, relative to Atlantic
and Pacific deeps.
The folding of the sediments merges into intrusions of magma in the
southern Appalachians. Here arose the granite problem on a tremendous
scale, which is repeated in our Ascutney Mountain in Vermont. What
it was doing under the bottom of those vast fields of limestone from
Ohio to Illinois we have no idea. No more do we know what is doing
under the vast fields of lime and red ooze at the present bottoms of
the deep oceans. But we do know that fire-made rock squirts up under
all sea-laid sediments which anyone has ever studied on islands or
continents. This fire-made rock, solidified, has thickness and a
bottom. We do not know its thickness nor its bottom. We do know that
under it are big cracks 2,000 miles long rupturing it into volcano
systems. The conclusion is that the globe is mantled by a layer of
igneous matter which has spouted up cracks since more than 3,000
million years ago. How did this matter migrate by new intrusions,
to pull, push, heat, and wrinkle through 500 million years the dirt
accumulated in shallow Appalachian trenches from Alabama to Indiana? We
do not know.
Public-domain text, read in full here on John Shaqi.
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