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
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[Illustration: CUPID’S CAVE, MAMMOTH HOT SPRINGS.]
The most interesting, because always reliable, is Old Faithful Geyser,
which throws up a stream of hot water six feet in diameter 130 feet high
every fifty-seven minutes, and sustains the flow for a period of five
minutes. The amount of water thus discharged every hour is 100,000
gallons, or enough to supply a small river. The Bee-hive, located on the
opposite side of the river, blows up a column of water three feet in
diameter to a height of 250 feet, and plays, generally, for fifteen
minutes, but at intervals of twenty-four hours. The Giantess is, for
several reasons, the most interesting of all the 700 geysers within
National Park. One may approach to the very brink of her crater, which
is twenty feet across, and look down one hundred feet into her hot
throat and hear the fierce gurgling of water, but none is visible until
an eruption is about to occur. Then the sputtering increases, deep
groans are audible, and a burst of steam is followed by a discharge of
water that shoots upward in a succession of jets. The first main column
sent up reaches a height of sixty feet, through which there are
projected small streams a foot in diameter to a height of 250 feet, thus
making a magnificent display for twenty minutes which nothing artificial
can ever rival.
Giant Geyser is less pretentious than the Giantess, having a ragged cone
that is broken on one side, and through a vent eight feet in diameter a
discharge is made at irregular intervals, when a stream of water is
tossed to a height varying from 90 to 200 feet, and the activity
sometimes continues for two or three hours. Other geysers that make fine
displays are the Sawmill, Turban, Grotto, Punch-Bowl, Soda, Grand, Fan,
and Riverside, some of which are never quiet, while others play only
occasionally. It has been found by experiment that foreign substances
thrown into some of these craters create an agitation that frequently
results in eruptions; the introduction of soap or lye is invariably
attended by some manifestation even in the quiet geysers, while the
active ones are by this means made to flow again almost immediately
after an eruption has taken place.
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[Illustration:
Public-domain text, read in full here on John Shaqi.
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