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
History
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
A rapid commences at the precise point where Fox River issues from
Winnebago Lake. This rapid, down which canoes descend with half loads,
extends a mile and a half, when the river assumes its usual navigable
form, presenting a noble volume. Nine miles below this, a ledge of the
semi-crystalline limestone rock crosses the entire channel, lifting
itself five feet above the bed of the stream. Over this the Fox River
throws itself by an abrupt cascade. Down this shelf of rock, the canoes,
previously lightened of their burden, are lifted by the men. It was
sometime after dark when we reached and encamped on the north shore, at
the foot of this cascade, which bears the name of Konamik. The syllable
_kon_, in this word, appears to me to be the same as _con_ in Wisconsin,
and is, apparently, a derivative from a term for strong water, which
has, in this case, the meaning of cascade or fall. The word _amik_, its
terminal, means a beaver. We thus have the probable original meaning in
beaver-water, or, by implication, beaver cascade. There is a rapid below
this fall. I judged the water must sink its level, in this vicinity,
about fifteen feet. On examining the character of the limestone, I
discovered crystals of calcareous spar occupying small cavities. At
other localities, at lower points, there were found crystals of black
sulphuret of zinc, and yellow sulphuret of iron. The rock appears to be
of the same age as the lead-bearing limestone of the West; it is also
overlaid by the red marly clay, and I should judge it to contain
deposits of sulphuret of lead.
The next morning, we resumed our descent of the Fox River with
difficulty. It was now the 19th of August, and the waters had reached
their lowest summer stage. The entire distance of twelve miles from the
Konamik to the Kákala fall may be deemed to be, at this season, a
continuous rapid. Our barge was abandoned on the rapids. While the men
toiled in these rapids to get down their canoes, it was found rather a
privilege to walk, for it gave a more ample opportunity to examine the
mineral structure and productions of the country.
It was high noon when we reached the rapids of the Kákala. This is a
formidable rapid, at which the river rushes with furious velocity down a
rocky bed, which it seems impossible boats or canoes should ever safely
descend. It demands a portage to be made, under all circumstances, the
water sweeping round a curve or bow, of which the portage path is the
string. This is the apparent meaning of the term, in the Indian tongue;
but it is disguised by early orthography, in which the letter _l_ has
taken the place of _n_, and the syllable _in_ of _au_. The term _kakina_
is the ancient French form of the Indian transitive-adjective _all_,
inclusive, entirely. There is another root for the term in _kakiwa_,
which is the ordinary term for a portage, or walk across a point of
land, which is rendered local by the usual inflection, _o-nong_.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account