Glimpses of America: A Pictorial and Descriptive History of Our Country's Scenic MarvelsBuel, James W. (James William)
History
Glimpses of America: A Pictorial and Descriptive History of Our Country's Scenic Marvels
Buel, James W. (James William)
United States -- Pictorial works
FRONT VIEW OF MAMMOTH HOT SPRINGS—CLEOPATRA AND JUPITER TERRACES.—The
chief wonders in Yellowstone National Park are the geysers, and the
limestone formations such as are shown above. These terraces are
formed by exuding water carrying a heavy solution of travertine,
which is deposited in the most remarkable shapes when coming in
contact with the air. This deposit is semi-crystalline, often
resembling snow-banks, and as the process of hardening goes on in
circular rims, basins are left which hold the water, and reflect in
a myriad of hues the sky and surroundings.
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[Illustration: CAÑON OF MISSOURI RIVER, NEAR GREAT FALLS.]
The Montana Central and Great Northern Railroad convey travelers over a
good road eighty miles further, to the Falls of the Missouri, three in
number, which are scattered over a distance of twelve miles, where the
river flows through a cañon with vertical walls 200 to 500 feet high. We
first meet a cascade called Black Eagle Falls, where the entire river
drops over a ledge twenty-six feet high, a precursor of the more
terrible waterfalls that are to come. The next one to appear in view is
Rainbow Falls, where the river, 1,200 feet wide, hurls itself down a
perpendicular descent of fifty feet. Six miles further down are the
Great Falls, that have a leap of ninety feet, and whose terrible roaring
can be heard a dozen miles away. At this point the river has a volume
greater than the Mississippi, but is narrowed to 300 feet by walls 200
feet high. An island divides the rushing waters, the half next to the
right bank dashing down with such tremendous effect that clouds of spray
are sent 200 feet high, which, struck by bright sunbeams, are converted
into rainbows, or at times glow with prismatic hues like giant soap-
bubbles. That part of the stream flowing to the left passes over a
succession of ledges, forming a magnificent cataract of fleecy foam, 200
feet in width and 90 feet in perpendicular elevation. But though these
are the principal falls, there are twelve others within a distance of
ten miles, having a total descent of 400 feet, and these interruptions
in the channel continue, though in a lesser degree, as far down as Fort
Benton, which is the head of navigation.
Public-domain text, read in full here on John Shaqi.
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