Appletons' Popular Science Monthly, February 1899: Volume LIV, No. 4, February 1899Various
Science
Appletons' Popular Science Monthly, February 1899: Volume LIV, No. 4, February 1899
Various
Science -- Periodicals; Technology -- Periodicals
It was at noon on the 22d of July in the summer of 1897 that we made
camp near the mouth of Cache Creek, about three miles southeast of the
military post and mail station of Soda Butte. In company with Dr.
Francis P. King I at once started up the creek, keeping the left bank,
that we might not miss the gulch, which joins the valley of Cache
Creek from the southern side. We had a toilsome climb through timber
and over steep embankments, cut by the creek in a loose conglomerate,
and after going about a mile and a half we noticed that some of these
banks were stained with whitish and yellow deposits of alum and
sulphur, indicating that we were nearing the old hot-spring district.
Soon a caved-in cone of travertine was seen, with crystalline calcite
and sulphur in the cavities, and the bed of the creek was more or less
completely whitened by these deposits, while here and there could be
seen along the banks oozing "paint-pots" of calcareous mud, in one
case inky black, with deposits of varicolored salts about its rim, and
a steady ebullition of gas bubbles rising from the bottom. In other
cases these pools were crystal clear, and always cold. The vegetation,
which below had been dense close to the creek's bank, here became more
scanty, especially on the southern side, where the bare rock was
exposed and seen to be a volcanic breccia, much decomposed and stained
with solfataric deposits. A mound of coarse _débris_ seen just above
on this side indicated the presence of a lateral ravine, which from
its situation and character we decided was probably the gulch sought
for. A strong odor of sulphureted hydrogen had been perceptible for
some time, and when we entered the gully the fumes became oppressive,
causing a heavy burning sensation in the throat and lungs. The ravine
proved to be as described, a V-shaped trench cut in the volcanic rock,
about fifty feet in depth, with very steep bare whitish slopes,
narrowing to a stony rill bed that ascended steeply back into the
mountain side.
[Illustration: GENERAL VIEW, LOOKING DOWNSTREAM, OF LOWER PART OF
DEATH GULCH.]
Public-domain text, read in full here on John Shaqi.
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