Wonders of the YellowstoneRichardson, James (Geologist)
History
Wonders of the Yellowstone
Richardson, James (Geologist)
Yellowstone National Park
"The region was filled with boiling springs and craters. Two hills,
each 300 feet high, and from a quarter to half a mile across, had
been formed wholly of the sinter thrown from adjacent springs--lava,
sulphur, and reddish-brown clay. Hot streams of vapor were pouring
from crevices scattered over them. Their surfaces answered in hollow
intonations to every footstep, and in several places yielded to
the weight of our horses. Steaming vapor rushed hissingly from the
fractures, and all around the natural vents large quantities of sulphur
in crystallized form, perfectly pure, had been deposited. This could be
readily gathered with pick and shovel. A great many exhausted craters
dotted the hill-side. One near the summit, still alive, changed its
hues like steel under the process of tempering, to every kiss of the
passing breeze. The hottest vapors were active beneath the incrusted
surface everywhere. A thick leathern glove was no protection to the
hand exposed to them. Around these immense thermal deposits, the
country, for a great distance in all directions, is filled with boiling
springs, all exhibiting separate characteristics.
"The most conspicuous of the cluster is a sulphur spring twelve
by twenty feet in diameter, encircled by a beautifully scolloped
sedimentary border, in which the water is thrown to a height of from
three to seven feet. The regular formation of this border, and the
perfect shading of the scollops forming it, are among the most delicate
and wonderful freaks of nature's handiwork. They look like an elaborate
work of art. This spring is located at the western base of Crater Hill,
above described, and the gentle slope around it for a distance of 300
feet is covered to considerable depth with a mixture of sulphur and
brown lava. The moistened bed of a small channel, leading from the
spring down the slope, indicated that it had recently overflowed.
"A few rods north of this spring, at the base of the hill, is a cavern
whose mouth is about seven feet in diameter, from which a dense jet of
sulphurous vapor explodes with a regular report like a high-pressure
engine. A little farther along we came upon another boiling spring,
seventy feet long by forty wide, the water of which is dark and muddy
and in unceasing agitation.
Public-domain text, read in full here on John Shaqi.
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