The Geologic Story of Yellowstone National ParkKeefer, William R.
Science
The Geologic Story of Yellowstone National Park
Keefer, William R.
Geology -- Yellowstone National Park
The pronounced rise in elevation of the general ground surface and the
chopping of the region into many mountainous fault blocks caused a
profound increase in the rate of erosion. Once-sluggish streams turned
into vigorous, fast-moving rivers that began to cut deeply into the
Absaroka volcanic plateau. Huge quantities of rock debris were stripped
off and carried out of the area, and at the end of the Pliocene, the
Yellowstone region must have been very highly dissected mountains and
table- and canyon-lands. Much of the landscape may have resembled the
rugged terrain now seen in the Absaroka Range along the east side of the
Park. These mountains (fig. 27), and the Washburn Range in the interior
of the Park (fig. 4), today represent but small remnants of the vast
pile of Absaroka volcanic rocks that once covered all of Yellowstone and
the surrounding regions.
[Illustration: Moose]
Formation of the Yellowstone Caldera
We have now approached that point in geologic time—the beginning of the
Quaternary Period between 2 million and 3 million years ago—when the
stage was set for the triggering of those all-important events that
culminated in the development of the 1,000-square-mile Yellowstone
caldera and ultimately gave rise to the world-renowned hot-water and
steam phenomena. Involved were some of the earth’s biggest explosions,
which have had no apparent counterpart in recorded human history. A few
extremely explosive eruptions have occurred historically, however, such
as the one that took place on the uninhabited island of Krakatoa,
between Java and Sumatra in the East Indies, during the latter part of
August 1883. For several days this island had been shaken by a series of
violent explosions. Then, on August 27, it was ripped by an explosion
that was heard as far away as Australia, a distance of about 3,000
miles. Fifty-mile-high dust clouds became windborne around the globe,
producing colorful sunrises and sunsets in all parts of the world for
several years. When the air around Krakatoa finally cleared, it was
found that two-thirds of the island, some 12 square miles, had collapsed
and vanished into the sea. Though the Krakatoa eruption resulted in a
caldera that is only a small fraction of the size of the one in
Yellowstone, it provides a mental picture to help us understand what has
been discovered about the great volcanic holocaust in Yellowstone
National Park that was described briefly in an early part of this
report.
Public-domain text, read in full here on John Shaqi.
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