
Origins 12(1):41-45 (1985).
LITERATURE REVIEW
THE EXPANDING EARTH. 1976. S. Warren Carey. Elsevier Scientific Publishing Company, Amsterdam, The Netherlands. 488 pp.
This book is the tenth volume in a series on Developments in
Geotectonics.
S. Warren Carey is an internationally known geologist at the University
of Tasmania in Australia. His publications on tectonics go back to his Doctor of Science
thesis entitled Tectonic Evolution of New Guinea and Melanesia done in 1938 at
the University of Sydney. He has regularly published in this area since that time, being a
proponent of Wegener's continental drift theory when it was generally being ridiculed. In
1953 Carey sent a paper to the American Geophysical Union proposing "the transport of
continental blocks on the back of convection cells" with subduction of the crust at
"the downgoing limb of the convection cell." The paper was rejected at the time
"on the grounds that it was naive" (p. 9). In 1971 Carey resubmitted this paper
with an attached letter that included the following paragraph:
Although I worked with subduction models for more years than any of the new generation of subducers has yet done, I have since moved on to what I think are more probable models (p. 10).
And that is what this book is about, a "more probable
model" which proposes "that the earth is expanding and that the separation of
the continents by growth of new oceans is not extensively compensated by the swallowing of
old crust elsewhere" (p. 14). "That the diameter of the earth has increased with
time at an increasing rate, is the theme of this book" (p. 118). In fact Carey
suggests that there is evidence that the surface area of the earth has doubled since the
Paleozoic era (pp. 20, 47, 51).
The evidence that Carey cites necessitating an expanding earth are:
Carey also discusses the double-equator paradox during the Triassic
period (p. 209) and the paradox of paleopole overshoot for the Tertiary period (p. 215) as
evidence for an expanding earth.
Carey reserves some of his most scathing comments about standard plate
tectonics for the subduction trenches. He states, "Subduction exists only in the
minds of its creators" (p. 16) and "the Pacific subduction zones like all other
subduction zones are myths" (p. 50). This is the crucial difference between standard
plate tectonic theory and Carey's expansion model, for both schools of thought agree on
sea-floor spreading but differ on the interpretation of the trenches (p. 54). Arguments
that he uses to support these contentions are:
Carey cites studies which claim that seismic (p. 74) and
paleomagnetic data (p. 195) have been screened and selectively interpreted to be
consistent with assumed subductions.
In response to the question, "What causes the expansion of the
earth?" Carey's first response is that he does not know. Suggested possibilities are:
The scenario that Carey proposes starts with a dense earth with an
Archean crust broken by tensional rifts over a slowly expanding interior. Heat and gas
escaped from the interior via the cracks with rocks changing to less dense phases along
these boundaries causing these polygonal boundaries to arch upward to form basins for
shallow seas. Due to "the inherent feedback instability of the outgassing process,
some undations [formation of mountains by huge waves in the crust of the earth] inevitably
developed more than others" (p. 126). This process eventually led to the formation of
the Pacific basin and Pangea. During the Carboniferous period asymmetric expansion
developed a "mantle tumour" under the southern part of Pangea which led to the
break-up and dispersion of Gondwanaland (Australia, Antarctica, Africa and South America)
(pp. 134, 135). This large megatumor also resulted in a rotational asymmetry of the earth
causing an axial wobble which the gravitational torques of the sun and moon turned into an
axial tilt which led to the Permian glaciation. Viscous drag dissipated this tilt by the
Jurassic period (p. 135).
Carey argues that the obliquity of the rotation axis of the earth is
the most important variable for geologic history (p. 131). These changes affect the
intensity of the magnetic field because changes in the paleomagnetic poles govern climate
changes and affect the motion of the plates. These cycles are related to the inability of
heat interior to the earth to escape by conduction and stable convection, and cause
instabilities to develop with the formation of megatumors which cause wobble and tilt.
Also, excess heat is expelled by magma floods, crustal disruption and explosions (p. 138).
Presumably another bulge during the Eocene epoch caused the present
23½° tilt of the earth and cause further dispersion of the continents (p. 136).
Greater expansion in the southern hemisphere tended to move the
continents northward which increased the moment of inertia of the northern hemisphere
tending to slow down the rotation of the north which created the "Tethyan shear"
(pp. 271, 272). The fact that North America is west of South America is an evidence of
this shear.
Carey suggests that two tests already demonstrate the validity of his
model (p. 443):
He proposes three more tests (p. 443):
Carey feels that these tests conducted over several years would be able to test his
model.
Carey critiques the concept of uniformitarianism (p. 114). He
distinguishes methodological or immanent uniformitarianism (uniform application of natural
law) and substantive or configurational uniformitarianism (uniformity in the environment).
He feels that the principle of uniformitarianism is much too rigorously applied (p. 114)
and that we must allow for changes in even fundamental physical constants. He states,
"We have no right to assume that unique events have not occurred, but must be alert
to recognise them if they are recorded. Unfortunately we see only what we know, so the
probability is, that if faced with the evidence of a unique event in the geological
record, we would fail to observe it. As Claude Bernard said, 'It is what we think we know
that prevents us from learning'" (p. 118).
Much of the middle part of this book discusses technical details of
paleomagnetism, rotational dynamics of the earth and solar system, and regional data.
Little reference exists in the literature about Carey's proposal of an
expanding earth. There are a few geologists, in addition to Carey, who maintain an
expanding earth hypothesis, including Krassilov, Owen, Shields and Stewart (Shields 1979).
Among those who have criticized Carey's ideas, Cox claims that "paleomagnetic studies
have now pretty well ruled out expansion large enough to account for the formation of all
the ocean basins" (Cox 1973). Hess admits that an expanding earth removes some of the
difficulties in dealing with the evolution of ocean basins, but he finds it
philosophically unsatisfying. He does point out the difficulty of adding "an enormous
amount of water to the sea in just the right amount...." Le Pichon notes that it
would be necessary for the great circle of the equator and the great circles of longitude
to expand at the same rate in order to maintain an approximately spherical earth. But
"spreading rates" from axes of ridges would suggest that the equatorial circle
is expanding more than twice as fast as the longitudinal circles on an expanding earth
model (Le Pichon 1968). And with respect to the "subduction trenches" it is
still not clear even with the conventional plate tectonic model whether the plates are
being "pushed" or "pulled" down (Wyllie 1976). If the latter is the
main mechanism, then these trenches would show tensional features even though subduction
was occurring.
In conclusion, it does seem that Carey has raised some questions about
plate tectonics and that his model does resolve some problems in the current theory. The
three tests which he proposes are "do-able" and would provide essential evidence
about the validity of the expanding earth hypothesis.
REFERENCES
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