The history of Bannock County, IdahoSaunders, A. C. (Arthur Charles)
History
The history of Bannock County, Idaho
Saunders, A. C. (Arthur Charles)
Bannock County (Idaho) -- History
During pioneer days, Fort Hall was one of the most important posts
along the Oregon trail. It was the first point west of Fort Laramie,
where travelers could rest securely under the protection of the flag,
and where there was a garrison of soldiers to relieve them of all fear
of sudden attack from the Indians. Here the weary and travel-stained
pioneers, pushing on for the far-famed Oregon territory, found respite
from their toils and dangers, and enjoyed once more the companionship
of their own kind. Here, too, preparatory for the last, long march
of their transcontinental journey, they repaired their wagons, and
discarded such baggage as it had seemed wise to bring when starting,
but which later experience proved to be only an encumbrance. An area of
several acres around Fort Hall is said to have been covered with this
debris, which was ransacked by the Indians and shorn of such parts as
the red men wanted. Prof. W. R. Siders, superintendent of the Pocatello
public schools, who has been interested for several years in the effort
to locate the site of the original fort, and to whom the writer is
indebted for very generous and valuable information, maintains that
it ought to be possible to identify the Hudson Bay company’s fort by
the rummage in its vicinity. He has examined the banks of the Snake
river for several miles and been unable to unearth any such remains.
This failure adds probability to the statement of old “Doc” Yandell,
a trapper in early days, who still resides in these parts. Mr. Yandell
says that some years ago he and Pete Weaver lived on the site of old
Fort Hall, which was then on the banks of the Snake river, and three
quarters of a mile distant from a spring. In later years Mr. Yandell
maintained that he could walk directly to the site of his former camp,
but when he attempted to do so, he found that the Snake was flowing
within three hundred yards of the spring that used to be three-quarters
of a mile from its bank. It is probable that since his departure some
spring flood had washed out a new channel for the river, thereby
changing its course, and placing the old fort site under water. This
might account for Prof. Siders’ failure to find the debris of which he
was in search.
Public-domain text, read in full here on John Shaqi.
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