Climatic Changes: Their Nature and CausesHuntington, Ellsworth
Science
Climatic Changes: Their Nature and Causes
Huntington, Ellsworth
Climatic changes; Climatology; Paleoclimatology
As to the third possibility, it is perfectly logical to ascribe both
climatic changes and crustal deformation to some outside agency, solar
or otherwise, but hitherto there has been so little evidence on this
point that such an ascription has merely begged the question. If
heavenly bodies should approach the earth closely enough so that their
gravitational stresses caused crustal deformation, all life would
presumably be destroyed. As to the sun, there has hitherto been no
conclusive evidence that it is related to crustal movements, although
various writers have made suggestions along this line. In this chapter
we shall carry these suggestions further and shall see that they are at
least worthy of study.
As a preliminary to this study it may be well to note that the
coincidence between movements of the earth's crust and climatic changes
is not so absolute as is sometimes supposed. For example, the profound
crustal changes at the end of the Mesozoic were not accompanied by
widespread glaciation so far as is yet known, although the temperature
appears to have been lowered. Nor was the violent volcanic and
diastrophic activity in the Miocene associated with extreme climates.
Indeed, there appears to have been little contrast from zone to zone,
for figs, bread fruit trees, tree ferns, and other plants of low
latitudes grew in Greenland. Nevertheless, both at the end of the
Mesozoic and in the Miocene the climate may possibly have been severe
for a time, although the record is lost. On the other hand, Kirk's
recent discovery of glacial till in Alaska between beds carrying an
undoubted Middle Silurian fauna indicates glaciation at a time when
there was little movement of the crust so far as yet appears.[125] Thus
we conclude that while climatic changes and crustal movements usually
occur together, they may occur separately.
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