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Mountains and Red Herrings
Peter Molnar
Professor, Geological Sciences
CIRES, University of Colorado
Climate Change, Uplift of Mountain Ranges, and Evolution of Humans:
Which is chicken, which - egg, and which - red herring?
Many of us were taught, in elementary school if not later, that mountain
ranges go through an evolution of "youth," characterized by dramatic
relief and rugged topography, to "maturity," in which mountains and
ridges become gentler, and finally to "old age," where hills rather
than mountains dominate the landscape.
Although this notion makes qualitative sense, its converse - that
rugged mountain ranges must necessarily have formed recently in geologic
time - does not logically follow. Imbued with the association of rugged
topography with youthful mountain belts, geologists throughout the
world have attributed rugged landscapes to geologically recent uplift
(since late Pliocene and Quaternary time or since 3-4 Million years
ago), regardless of whether or not other geologic evidence suggests
recent growth. Said in other words, not only regions of geologically
active mountain building, like the Himalayas, but also tectonically
dead ranges, like the Rocky Mountains of the USA, (and geologically
senile ranges, like the Alps) are treated as young.
I challenge this general view and suggest that the evidence commonly
used to infer recent "uplift" of mountain ranges is better understood
to result from global climate change, with an increase in erosion one
consequence of such a change. To call attention to the absurdity of
the resulting implication that mountain ranges grew simultaneously
on all continents, I first note the correspondence in time of such
alleged "uplift" with the evolution of humans, which could be taken
to suggest that the rise of mountain ranges is responsible for the
evolution of Homo Sapiens. Then I analyze evidence of different kinds
that have been used to infer uplift of mountain ranges, beginning with
misuse of the word "uplift" itself, and I try to show that all such
evidence can be explained by climate change. For instance, paleobotanical
evidence of plants that today live in warm climates but that left fossils
in regions that today are high and cold can be understood as the result
of global cooling, without the need to postulate elevation changes.
Similarly, the cooling increased glacial activity and hence glacial
erosion, which has left an obvious imprint on the modern landscapes
of mountain ranges.
We live in an environment that is very different from that characterizing
most the past 300 million years, and most of the earth's entire 4.5
billion year history. If we had evolved only 3 million years earlier,
before the cooling that led to the Ice Ages, it is quite likely that
there would be no winter Olympics, skiing would not be a sport except
on Greenland and Antarctica, Colorado would be little more than a hilly
Kansas, and Boulder county would be just as conservative politically
as the rest of the state. |