Wonders of the YellowstoneRichardson, James (Geologist)
History
Wonders of the Yellowstone
Richardson, James (Geologist)
Yellowstone National Park
"From any point of view the Upper Falls are extremely picturesque and
striking. The entire volume of water seems to be, as it were, hurled
off of the precipice with the force which it has accumulated in the
rapids above, so that the mass is detached into the most beautiful
snow-white, bead-like drops, and as it strikes the rocky basin below,
it shoots through the water with a sort of ricochet for the distance of
200 feet. The whole presents in the distance the appearance of a mass
of snow-white foam. On the sides of the basalt walls there is a thick
growth of vegetation, nourished by the spray above, which extends up as
far as the moisture can reach.... After the waters roll over the upper
descent, they flow with great rapidity over the apparently flat rocky
bottom, which spreads out to nearly double its width above the falls,
and continues thus until near the Lower Falls, when the channel again
contracts, and the waters seem, as it were, to gather themselves into
one compact mass and plunge over the descent of 350 feet in detached
drops of foam as white as snow; some of the large globules of water
shoot down like the contents of an exploded rocket.... The entire mass
of the water falls into a circular basin, which has been worn into the
hard rock, so that the rebound is one of the magnificent features of
the scene.... It is a sight far more beautiful, though not so grand or
impressive as that of Niagara Falls. A heavy mist always rises from
the water at the foot of the falls, so dense that one cannot approach
within 200 or 300 feet, and even then the clothes will be drenched in
a few moments. Upon the yellow, nearly vertical wall of the west side,
the mist mostly falls, and for 300 feet from the bottom the wall is
covered with a thick matting of mosses, sedges, grasses, and other
vegetation of the most vivid green, which have sent their small roots
into the softened rocks, and are nourished by the ever-ascending spray.
At the base and quite high up on the sides of the cañon, are great
quantities of talus, and through the fragments of rocks and decomposed
spring deposits may be seen the horizontal strata of breccia."
Public-domain text, read in full here on John Shaqi.
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