A Book of the United States: Exhibiting its geography, divisions, constitution, and government ... and presenting a view of the republic generally, and of the individual states; together with a condensed history of the land, from its first discovery to the present time. The biography of about two hundred of the leading men: a description of the principal cities and towns; with statistical tables — John Shaqi
A Book of the United States: Exhibiting its geography, divisions, constitution, and government ... and presenting a view of the republic generally, and of the individual states; together with a condensed history of the land, from its first discovery to the present time. The biography of about two hundred of the leading men: a description of the principal cities and towns; with statistical tables
History
A Book of the United States: Exhibiting its geography, divisions, constitution, and government ... and presenting a view of the republic generally, and of the individual states; together with a condensed history of the land, from its first discovery to the present time. The biography of about two hundred of the leading men: a description of the principal cities and towns; with statistical tables
United States -- Biography; United States -- Description and travel; United States -- History
The river, for the distance of about seventeen miles, becomes almost
a continued cataract. In this distance its perpendicular descent is
three hundred and sixty-two feet. The first fall is ninety-eight feet;
the second, nineteen; the third, forty-seven; the fourth, twenty-six.
Next to the Niagara these falls are the grandest in the world. The
river continues rapid for a long distance beyond, but there is not
much variation in its appearance till near the mouth of the Platte.
That powerful river throws out vast quantities of coarse sand, which
contribute to give a new face to the Missouri, which is now much more
impeded by islands. The sand, as it is drifted down, adheres in time
to some of the projecting points from the shore, and forms a barrier
to the mud which at length fills to the same height with the sand-bar
itself. As soon as it has acquired a consistency, the willow grows
there the first year, and by its roots gives solidity to the whole;
with further accumulations the cotton-wood tree next appears, till the
soil is gradually raised to a point above the highest freshets. Thus
stopped in its course, the water seeks a passage elsewhere, and as
the soil on each side is light and yielding, what was only a peninsula
becomes gradually an island, and the river compensates the usurpation
by encroaching on the adjacent shore. In this way the Missouri, like
the Mississippi, is continually cutting off the projections of the
shore, and leaving its ancient channel, which may be traced by the
deposits of mud and a few stagnant ponds.[6]
During the whole length of the Missouri below the Platte, the soil
is generally excellent, and although the timber is scarce, there is
still sufficient for the purpose of settlers. But beyond that river,
although the soil is still rich, yet the almost total absence of
timber, and particularly the want of good water, of which there is
but a small quantity in the creeks, oppose very powerful impediments
to its occupancy. The prairies for many miles on each side of the river
produce abundance of good pasturage.
Public-domain text, read in full here on John Shaqi.
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