The chief officer, Dr. Ferdinand V. Hayden, was an unusually capable
geologist. In addition, he possessed an inspiring personality and
statesmanlike views. There were nineteen scientists directly under his
command. The personnel included James Stevenson, managing director;
Henry W. Elliott and Thomas Moran, artists; Professor Cyrus Thomas,
agricultural statistician and entomologist; Anton Schonborn, chief
topographer; William H. Jackson, photographer; George B. Dixon,
assistant photographer; J. W. Beaman, meteorologist; Professor G. N.
Allen, botanist; Robert Adams, Jr., assistant botanist; Dr. A. C. Peale,
mineralogist; Dr. C. S. Trunbull, physician; Campbell Carrington, in
charge of zoological collections; William B. Logan, secretary; F. J.
Huse; Chester M. Dawes, son of Representative Henry L. Dawes of
Massachusetts; C. De V. Hegley and J. W. Duncan, assistants. Barlow’s
army detail also had a competent and well-balanced personnel.[145]
A military escort, including Lieutenant Doane, rounded out these
expeditions and provided all that could have been desired in point of
training and ability. Each detachment had a retinue of helpers. Two
technical studies and scientific reports, which not only substantiated
but actually enhanced the findings of the previous civilian
explorations, resulted from these two expeditions.
Hayden’s party left Fort Ellis, near Bozeman, on July 15, 1871. Upon
reaching the junction of the Yellowstone and Gardner rivers they elected
to ascend the latter. It was a good choice because within the hour they
beheld a white mountain which resembled a vast cascade of frozen snow.
The Mammoth Hot Springs Terraces “alone surpassed all the descriptions
which had been given by former travelers.”[146]
As this expedition progressed, the geological record was interpreted.
Thereafter, rocks were identified as travertine, gneiss, rhyolite,
dacite, basalt, breccia, geyserite, sinter, and obsidian. Trees and
plants were likewise classified, and in addition to geysers, springs and
pools there were fumaroles and _solfataras_. Geological speculations
were formulated relative to petrified forests, Grand Canyon, the lake’s
former Snake River outlet, and the relationship of heat, water, and
“plumbing” essential for geyser action.
[Illustration: _The Hayden expedition in camp_]
Public-domain text, read in full here on John Shaqi.
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