Frontier and pioneer life -- West (U.S.); West (U.S.) -- Social life and customs
after two more days of travel, we were told that even then Fremont Peak
was nearly one hundred miles beyond us. Fred accordingly declared that
we should never reach it unless we turned back in the other direction,
because the longer we traveled toward it, the further it was away.
[Illustration: THE ROCKIES]
The day after we obtained our first view of Fremont Peak, we knew that
we were near a certain strange freak of nature known as Ice Springs. Its
location is carefully noted on the old charts, and it is described in
the reports of numerous explorers and travelers. In every description of
the springs that I had read or heard, it was stated that at any time of
the year, even in the late summer, a solid mass of ice could be found
within a foot of the surface. We determined to see this remarkable
phenomenon. The springs lie near the foothill on the edge of a somewhat
extensive area of swampy ground from which no water issues on the
surface. Digging down a spade's depth we reached the white crystal and
found it to be cold enough to answer all requirements, but it was so
hard and the superimposed mud was so deep, that it seemed hardly worth
the effort to obtain a block under such difficulties. We reported to our
friends as had been done to us by former travelers that solid ice was
there, and endeavored to explain to each other by what processes ice
could be formed on an open plain during hot summer days, but never
arrived at a satisfactory solution of the problem. Professor W. H. Reed,
of the University of Wyoming, has finally come to my assistance and
exploded the "ice" theory _in toto_. Having learned of the generally
accepted belief that natural ice is formed in those springs, he made
the matter the subject of personal investigation and informs me that
"the springs show what appears to be ice, but what in reality is soda
and gypsum. The so-called ice springs yield a bitter water; this is
because of the dissolving of the gypsum, one of the lime deposits." The
springs like many frauds in other lands are very interesting to the
deluded seeker of curiosities and marvels, but it causes a shock to
learn that this midsummer ice is a fiction. The gypsum resembles soda
and also salt and ice. And thus is our popular delusion dispelled!
Public-domain text, read in full here on John Shaqi.
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