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Although the rocks of the Devils Postpile formed during the ice age, the
Postpile owes its origin to geologic processes initiated earlier. These
rocks are but one manifestation of widespread volcanic activity in this
part of the Sierra Nevada that began more than three million years ago
and has continued to the present. Perhaps born of the same underlying cause
as the volcanism, contemporaneous large-scale fault movements created the
steep eastern front of the Sierra Nevada; volcanic activity was greatest
along or adjacent to the eastern escarpment. Long Valley, from the headwaters
of Owens River to Lake Crowley, is a giant volcanic caldera. Mammoth Mountain-
a massive volcanic dome- has grown on the caldera margin.
Less than 100,000 years ago, basalt lava,
which was to become the Devils Postpile, erupted in the already glaciated
valley
of the Middle Fork of the San Joaquin River. The
age of volcanic rocks can be estimated by study of the radioactive decay
of elements
in the rocks. Previous estimates for the age of
the Postpile basalt, ranging from about 600,000 years to nearly a million
years, are now
thought to be seriously in error. Although an exact
age for the Postpile flow still is not known, we believe that an age
of less than 100,000
years, based on radiometric age determinations
on rocks thought to be correlative, is more reasonable.
The Postpile lava reached the surface in the vicinity
of the Upper Soda Springs Campground at the north
end of Pumice Flat (see map on page 14). Across the
San Joaquin River from the campground,
rust-colored basalt cinders- products of explosive
eruptions- rest upon granite bedrock and are probably
the remains of a volcanic cinder
cone, similar to the Red Cones southeast of the
Monument. Two basalt dikes- tabular bodies of solidified lava- can be
seen cutting
upward
through the cinder pile; when molten, these dikes
may have been feedervents for lava flows. We do not
know how extensive the lava outpourings were,
because most of the basalt has been removed by
combined glacial and stream erosion, but we can piece together some minimum
figures
from
the scattered outcrops that remain. Lava filled
the valley from side to side for a distance of at least three miles,
from
Pumice Flat south
to the Devils Postpile, and in the vicinity of
the Postpile the lava was probably more than 400 feet deep. |