Canada -- Description and travel; United States -- Description and travel
coming out alternately with the water jets. It generally acts in
unison with the Grand Geyser, a quarter of a mile northward, which
goes off about once a day. The Grand Geyser in action is most
powerful, causing the earth to tremble, while there are fearful
thumping noises beneath. The water in the crater suddenly recedes, and
then quickly spurts upward in a solid column for two hundred feet,
with steam rising in puffs above. The column seems to be composed of
numerous separate jets, falling back with a thundering sound into the
funnel. The outburst continues a few minutes, stops as suddenly as it
starts, and is repeated six or eight times, each growing less
powerful. Along the river bank nearby are the Wash Tubs, small basins
ten feet in diameter, each with an orifice in the bottom. If the
clothes are put in, the washing progresses finely until suddenly out
goes the water, and with it all the garments, sucked down the hole.
After awhile the basin fills again, and back come the clothes, though
sometimes they are very dilatory in returning. The Devil's Well, about
fifty feet away, is usually accused of complicity in this movement. It
is a broad and placid basin of hot water, with a beautiful blue
tinge, in which tourists sometimes boil their eggs and potatoes. It is
sentinelled by the Comet Geyser, exploding several times daily, but
through an orifice so large that it does not throw a very high column.
The great geyser of this Upper Basin is the Giant. It has a broken
cone set upon an almost level surface, with the enclosing formation
fallen away on one side, the interior being lined with brilliant
colors like a tessellated pavement. It is somewhat uncertain in
movement, but usually goes off every fourth day. It gives ample
notice, certain "Little Devils" adjoining, and a vent in the side of
the crater, boiling some time before it sends up the enormous column
which plays ninety minutes. The outburst, when it starts, comes like a
tornado, and the stream from it runs into and more than doubles the
current of the river. The column is eight feet in diameter, rises two
hundred and fifty feet at first, and is afterwards maintained at two
hundred feet. There is a deafening noise, and the steam clouds seem to
cover half the valley. The column goes up perfectly straight, and
falls back around the cone with a deluge of hot water. The Catfish, a
small geyser, is nearby, and to the northward a short distance is the
Grotto. This is an odd formation, its crater perforated with orifices
around a low, elongated mound, which point in different directions;
and when it goes off at six-hour intervals, the eruption is by streams
at an angle, giving a curious sort of churning motion to the water
column, which rises forty feet, continuing twenty minutes. The
Riverside has a little crater on a terraced mound just at the river's
edge, and is a small, irregular but vigorous spouter, throwing a
stream sixty feet. The Fan has five spreading tubes, arranged so that
Public-domain text, read in full here on John Shaqi.
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