History of Early Steamboat Navigation on the Missouri River, Volume 1 (of 2): Life and Adventures of Joseph La BargeChittenden, Hiram Martin
History
History of Early Steamboat Navigation on the Missouri River, Volume 1 (of 2): Life and Adventures of Joseph La Barge
Chittenden, Hiram Martin
La Barge, Joseph, 1815-1899; Missouri River -- History; Steam-navigation -- Missouri River
Of the many tributaries of the Missouri the most important is the
Yellowstone, which rivals in size the main stream and joins it nearly
eight hundred miles below the Three Forks. Like the Missouri it finds
its source in and around that now famous region, where Nature has
lavished without stint her most marvelous handiwork, and which the
government of the United States has set apart for the common enjoyment
of the people. Both the Missouri and the Yellowstone rivers, in the
upper portions of their course, flow over immense cascades and rapids
which have become well known among the cataracts of the globe. The
Great Falls of the Missouri are located near the modern city of the
same name. They comprise several cataracts and rapids, the highest
perpendicular distance being 87 feet, and the total fall over 500 feet.
The falls of the Yellowstone are within the National Park, the highest
perpendicular distance being 310 feet, and the total descent from
Yellowstone Lake to below the first cañon near Livingston, Mont., being
about 3200 feet.
[Sidenote: ALLUVIAL CHARACTER.]
Upon emerging from the foothills of the mountains, both streams
begin to assume that peculiar character which distinguishes them
throughout the rest of their course to the sea. They flow through
alluvial bottoms, built up of the detritus from the highlands and
mountains, until the present bed of the river is in most places fifty
to a hundred feet above the original bed in the solid rock. The
usual characteristics of an alluvial river are here found in their
highest development--a muddy current, freshly formed islands, sandbars
innumerable, an unstable channel, and a shifting bed which is never in
the same place for two years in succession.
Among the most striking phenomena of a river like the Missouri is the
constant change that is going on in the location of its channel. This
seems to be in some places a periodical matter. The forces of the river
get to working on particular lines and push their devastations for
many years in one general direction. Being finally arrested by some
insurmountable obstacle, or turned, it may be, by trifling causes,
they work in another direction, and invade lands which have enjoyed
long immunity, and upon which the cottonwood, walnut, and cedar have
attained mature growth.
[Illustration: A NEW “CUT OFF”
Old course of river toward background
Old course of river from background]
[Sidenote: A WINDING WATERWAY.]
Public-domain text, read in full here on John Shaqi.
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