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
A large portion of the river is in a latitude where it freezes over
every winter. During the ice period it is indeed effectually enchained.
The banks are safe for a season, and the water itself becomes
comparatively clear. But as soon as the breezes of spring soften the
ice the river resumes its customary wanderings, with renewed vigor
after its long rest. By way of celebration of its release from its icy
prison it frequently gives exhibitions of power that far surpass all
its other manifestations. When the ice “breaks” and begins to “run,”
it is liable to strand like a steamboat on the shallow bars. Other ice
following, and finding the way obstructed, piles up on that before it.
Gradually, sometimes, and sometimes rapidly, the accumulation spreads,
cutting off the channel of the river, until, as often happens, it
forms a veritable dam across the entire stream. These ice “gorges”
develop a power that nothing can withstand, and the amount of property
destroyed by them in the history of the river has been very great.
There is almost nothing that can be done to break them. Dynamite
explosions are resorted to, but the ice piles up so rapidly and in
such vast quantities that the most powerful blast seems harmless. In
the face of this appalling danger man is forced to stand a helpless
spectator until the river itself accumulates sufficient force to burst
through the dam. It has more than once happened that, before the dam
has given way, the river has cut an entirely new channel.
[Sidenote: ICE GORGES.]
The moving of the ice, even when not accompanied by serious blockades,
is always an impressive sight. Usually the warm weather loosens it from
the shore before it begins to move, and even disintegrates it, so that
it is unsafe to cross upon. The softer it becomes before it begins to
run the less danger is there of its gorging. After the movement begins
it continues for several days, until the vast quantities of ice stored
in the river above have floated by, or melted away. During the height
of the movement the crushing of innumerable ice cakes upon each other
produces a continuous roar which can be heard for a long distance from
the river.
To the lonely dwellers of the valley in the early times the annual
“break-up” of the ice was the most welcome event of the year, for it
was the knell of the long and tedious winter, and the certain harbinger
of approaching spring.
[Sidenote: ANNUAL FLOODS.]
Public-domain text, read in full here on John Shaqi.
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