Summary Narrative of an Exploratory Expedition to the Sources of the Mississippi River, in 1820: Resumed and Completed, by the Discovery of its Origin in Itasca Lake, in 1832Schoolcraft, Henry Rowe
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Summary Narrative of an Exploratory Expedition to the Sources of the Mississippi River, in 1820: Resumed and Completed, by the Discovery of its Origin in Itasca Lake, in 1832
Schoolcraft, Henry Rowe
Great Lakes (North America); Mississippi River -- Sources; Northwest, Old -- Description and travel
Having spent several hours in the chase, we again embarked, and
proceeded down the river until three o'clock in the afternoon. On the
left bank of the river two prominent elevations of the granitical
series, rising through the prairie soil, attracted my attention.
Immediately below this locality, a high and level prairie stretches on
the west shore, which had a striking appearance from its being crowned
with the poles and fixtures of a large, recently abandoned Sioux
encampment. At this spot the expedition landed and encamped. The quick
glances of Babasikundiba and his party of delegates immediately
discovered a pole, at the site of the chief's lodge, bearing a birch
bark scroll, or letter, inscribed with Indian hieroglyphics, or devices.
It turned out that this spot was the northern terminus of a Sioux peace
embassage, dispatched from St. Peter's shortly previous, under the
direction of Col. H. Leavenworth, U. S. A., the newly-arrived commanding
officer at that post. The message was eagerly received and read by the
Chippewa delegates. By it they were informed that the Sioux also desired
a termination of hostilities. The scroll was executed by tracing lines,
with the point of a knife, or some sharp instrument. The pictographic
devices thus drawn denoted the exact number of the party, their chiefs,
and the authority under which these crude negotiations were commenced.
Of this mode of communicating ideas among the Algonquin tribes, we have
before given details in crossing the boggy plateau of Akik Sepi, between
the St. Louis River and Sandy Lake. The present instance of it is
commented on in an interesting communication of the era, in the
appendix, from the pen of Gov. Cass. It was now no longer doubtful that
the Chippewa mission would be successful, and the satisfaction it
produced was evident in the countenances and expressions of
Babasikundiba and his colleagues.
I took a canoe and crossed the Mississippi, to inspect the geology of
the opposite shore. On reaching the summit of the rock formations
rising through the prairies, which had attracted my notice from the
river, I found them to consist of sienite, which was almost exclusively
made up of a trinary compound of white quartz, hornblende, and
feldspar--the two former species predominating. The feldspar exhibited
its splendent black crystals in fine relief in the massy quartz. This
formation extended a mile or more. What excited marked attention, in
surveying these rocks, was their smoothly rubbed surfaces, which seemed
as if they must have been produced by equally hard and heavy masses of
rock, driven over them from the north. I registered this locality, in my
Geological Journal, as the Peace Rock, in allusion to the purport of the
Indian mission, evidences of which were found at the opposite
encampment.[85]
Public-domain text, read in full here on John Shaqi.
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