Wonders of the YellowstoneRichardson, James (Geologist)
History
Wonders of the Yellowstone
Richardson, James (Geologist)
Yellowstone National Park
In the northwest corner of the Territory of Wyoming, about half way
between the Mississippi River and the Pacific Ocean, and in the same
latitude as the State of New York, the grand Rocky Mountain system
culminates in a knot of peaks and ranges enclosing the most remarkable
lake basin in the world. From this point radiate the chief mountain
ranges, and three of the longest rivers of the Continent--the Missouri,
the Columbia, and the Colorado.
On the south are the Wind River Mountains, a snow-clad barrier which no
white man has ever crossed. On the east is the Snowy Mountain Range,
and the grand cluster of volcanic peaks between it and Yellowstone
Lake. On the west is the main divide of the Rocky Mountains. On the
north are the bold peaks of the Gallatin Range, and the parallel
ridges which give a northward direction to all the great tributaries of
the Missouri from this region.
Set like a gem in the centre of this snow-rimmed crown of the
continent, is the loveliest body of fresh water on the globe, its
dark-blue surface at an elevation greater than that of the highest
clouds that fleck the azure sky of a summer's day, over the tops of the
loftiest mountains of the East. Its waters teem with trout, and the
primeval forests that cover the surrounding country are crowded with
game. But these are the least of its attractions. It is the wildness
and grandeur of the enclosing mountain scenery, and still more the
curious, beautiful, wonderful and stupendous natural phenomena which
characterize the region, that have raised it to sudden fame, and caused
it to be set apart by our national government as a grand national
play-ground and museum of unparalleled, indeed incomparable, marvels,
free to all men for all time.
Evidences of ancient volcanic action on the grandest scale are so
abundant and striking throughout the lake basin, that it has been
looked upon as the remains of a mammoth crater, forty miles across.
It seems, however, to have been rather the focus of a multitude of
craters. "It is probable," says the United States geologist, Dr.
Hayden, with his usual caution, "that during the Pliocene period the
entire country drained by the sources of the Yellowstone and the
Columbia was the scene of volcanic activity as great as that of any
portion of the globe. It might be called one vast crater, made up of a
thousand smaller volcanic vents and fissures, out of which the fluid
interior of the earth, fragments of rock and volcanic dust, were poured
in unlimited quantities. Hundreds of the nuclei or cones of these
volcanic vents are now remaining, some of them rising to a height of
10,000 to 11,000 feet above the sea. Mounts Doane, Longford, Stevenson,
and more than a hundred other peaks, may be seen from any high point on
either side of the basin, each of which formed a centre of effusion."
Public-domain text, read in full here on John Shaqi.
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