My experiments with volcanoesJaggar, Thomas Augustus
Science
My experiments with volcanoes
Jaggar, Thomas Augustus
Geologists -- Biography; Volcanoes
The process of erosion is supposedly slow, as all geological processes
are slow, if we neglect the possibility of such submarine landslips
or supramarine upheavals as occurred at Yakutat in 1899. But even
New England has floods, hurricanes, landslides, forest fires, and
cloudbursts which are exclamation points on an otherwise sleepy
history. And in the past it has had ice sheets, and subsidences beneath
the sea.
In other words, the making of valleys and stream patterns for the
map is accented occasionally, and the occasions may come in climatal
waves unknown to us. The stream patterns in the Bad Lands, Tennessee,
Pennsylvania, the Grand Canyon, and New England make very different
maps. The rotting of the rock, limestone caverns, rainfall, faults, and
sloping underground strata bearing spring water all influence these
maps. What is erosion and what index is written on the land to say the
Grand Canyon and tributaries are being carved downward faster than the
Mystic River in Boston?
Ralph Stone tackled the Mystic River, and marked ledges and set stakes
opposite the flood plain meanders. The idea was that ledges split by
winter freezes, and that the meanders of a stream build on one side
and cut on the other. Maps were made repeatedly, and the ledge cracks
were measured in millimeters. Some movement was found, but a college
year was not enough time. If we could combine as a motion picture,
photographs from the air taken once a year for many years, doubtless
the film would show that the stream meander pattern is migrating toward
the sea like a wiggling snake.
Stone next made a model three inches thick in a tank of water, by
sedimenting sixty-one very thin layers of marble dust, coal dust,
clay, red lead, and sand. He tipped it up as an island and sprayed it
in periods which lasted one to ninety-two hours, up to a total of 719
hours. A forking stream and its delta were formed in the lagoon of
the tank. The stream cut a canyon with waterfalls, treelike branches,
esplanades, and a flood plain. There were three principal hard white
multiple strata layers in the model, separated by sand. The white
layers made waterfalls and were eaten back to form the canyons.
When the cross section of the delta was sliced with a knife, it showed
three white layers foreset at thirty degrees under the tank pool
and separated by more sandy strata. The bottommost of these was the
sediment of the top thick marble dust layer of the model as first
eroded by the spray, and the top frontal layer of the leaf-shaped delta
was the product of the erosion of the canyon bottom on the lowest of
the white layers. This must happen in nature where one formation in
reverse order is derived by river erosion undermining a stratified
older pile of sediments.
Public-domain text, read in full here on John Shaqi.
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