Four Theories of Earth Expansion and
the Eocene Event
Karl W. Luckert
A Video Script prepared
for the 32nd IGC Post-Workshop PWO 09 -- “New Concepts in
Global Tectonics” -- Urbino, Italy,
August
29-31, 2004.
Commentary, added
during the 2016 Revision of the “Triplehood” Website:
About the precise
manner of East-Pacific rifting – and of Antarctica “moving” southward relative
to the present sphere – I have already noted the fact, that in my videos I was
displaying the continental separations all too loosely. My explanations of
Antarctica’s relationship to the tip of South America, influenced to some
extent by my video animations in my bilingual Theuern
video, and in the Urbino edition, were definitely inadequate.
Explaining
Antarctica’s twisting away, to the west of the Americas, my Urbino video was
even farther off the mark. In my recent book, Spread and Growth Tectonics… (2016), I explained continental
contacts along the South American cape much tighter. I am publishing these
dated videos on Youtube, now anyhow, because they also contain
illustrations of other processes—such as the general expansion of oceans as
illustrated by isochrones. The videos will at least demonstrate, roughly, how I
do envision the overall expansion and how my thinking has evolved over time. However,
everything here should be viewed as leading up to my 2016 book, titled “Spread
and Growth Tectonics….” In comparison with differences presently championed by
other Earth-Expansionists, changes within my own visualization of the expansion
process, overall, appear to be minor issues. I am getting too old to acquire
better technology to remake my videos. Nevertheless, serious students equipped
with better technology should be able to visualize—or even synthesize—my explanations
easily enough from what I have made available over time, shown at this website
and in the book.
The initial
ocean-spreading in the north-eastern Pacific began with rifting between
Antarctica and North America, gradually, since the Cretaceous. Expansion in the
northeastern Pacific was the natural result of the round Pacific cavity,
carving out the round Antarctica while the ocean itself was getting enlarged by
way of creating new ocean floor. The earliest ocean floor in the northeastern
Pacific resulted from the general enlargement of the ocean. It became part of
the triangular ocean floor plate that grew along the round of Antarctica and
which now points into the southwestern Indian Ocean. Along the southern flank
of the Atlantic, since Africa’s departure from there—and Australia’s departure
in the opposite direction during the Eocene—the ocean floor was pre-torn down
into the Upper Mantle and soft enough to be intruded upon. All the while, the
Pacific has insisted on its own round enlargement—thereby tearing and twisting
the round Antarctica west- and southward. The Pacific’s growth itself has pushed
Antarctica, shearing past the Cape of South America, nearly all the way east
across the width of the southern Atlantic edge of the time.
In any case, I am back
again, closer to my Theuern video of seeing the
Antarctic Plate do most of its turning later, in fresh southern
ocean space, after having poked eastward as far as the Islas Orcadas Rise. With this observation, I cannot see anymore
the possibility of a small continental collision having occurred there, which
for I while I had granted as a possibility. Not here at the toe of South
America, nor anywhere else in the topography of the planet, is there evidence
of a continental collision. There is no need to postulate that coastal mountain
ranges were pushed up by continental collisions. What we see at the toe of
South America was a slight displacement caused by tearing, close shearing, and
a nudge between the toe just mentioned and the portion of Antarctica that has
become its tail.
I regret now having
ever used the metaphor of a “dance” to refer to the southward “turn” of the
Antarctic Plate during the Eocene. Apparently, I have been lecturing too many
years, trying to challenge students with analogies and exaggerations. In any
case, by using this metaphor I lost at least the sympathy of the late Klaus
Vogel. Because he could not understand my meaning relative to the isochrones,
he has reproached me to the effect that continents do not jump (“sie hüpfen nicht”). The Langenscheidt Dictionary, was too timid
to help him recognize the difference between turning a dance-step and “hüpfen.” I should
have limited myself to the weaker metaphors of “twisting” and “turning.” But then, our friendly disagreements went
deeper than the metaphors we preferred.
For Klaus Vogel, and for his globe constructions, the continents have
remained genuine Wegenerian wanderers. He was not interested in contemplating
isochrones, which I happen to recognize as primary data. For me the “Wandern” of
continents has all along been an overdrawn metaphor—much more so than a full
turn (Umdrehung)
in a dance. Of course, in both the German and the English language can it be
said that, superficially, continents “do wander.” They wander after the fashion
in which, for common folk and scientists alike, the Sun continues “to rise” in
the East and “to go down” in the West. Antarctica was turned horizontally by a
process of getting transported sideways, by irregularly expanding ocean floors
and sitting on a tough mantle substratum, being invited into regional mafic areas
where ocean floors were still young and soft.
Abstract
Reflecting on numerous
presentations of Expansion Tectonics theory, the conclusion has emerged, that
most misunder-standings regarding Earth Expansion, in
the past, can be traced to defective visualizations. I have been doing video
animations of the Earth expansion process since 1996, and by now my method has
evolved to a level at which it can be used as a preliminary scientific testing
procedure for a variety of tectonic processes. Common wisdom has it that video
animation -- known in some languages as “trick photography” -- does exist for
the sole purpose of deceiving the viewer. This need not be the goal. Animations
that are based on serious globe models or thumbnail images can help illustrate
a proposed expansion process dynamically, reflecting exactly how the author of
a particular expansion theory does envision it. Animation can give to a viewer
a preliminary impression of whether a proposed expansion process falls within
the range of tectonic probability -- provided the viewer is alert to material
and tectonic processes in general, within three-dimensional space and time.
Animation can ruthlessly expose certain tectonic improbabilities which static
globe models and thumbnail sketches might fail to reveal.
The models and thumbnails of Earth
expansionists, whose theories I have chosen to animate -- Hilgenberg, Vogel, Maxlow, and my own -- can better be visualized, studied,
and judged after they have been viewed comparatively, in video animation.
Contextual animation does solve many global tectonic problems in stride -- as
the present video succeeds in illuminating the uniform formation of East
Asia’s marginal seas and island chains. As a matter of principle, I have
expanded equal and sometimes even greater efforts in producing correct animated
sequences for the theories of my competitors than I have for my own.
The comparative aim of my video
presentation is new to the field, and it is intended to stimulate a continued
desire for clarification. At various steps of preparation have I been able to effect some improvements regarding details of my own theory.
Moreover, in addition to the usual isochrone maps and globes I have, in this
edition, utilized numerous NASA satellite images. I consider this 33-minute
video lecture, in DVD format, to be a fitting addendum to my last year’s DVD-lecture
at the Theuern Conference, in Germany 2003. It was
undertaken as a follow-up and as an improvement on its precedent.
The VideoScript:
Hello, I am Karl Luckert, speaking near Mount Hood, in the Cascade
Mountain Range, along our planet’s beautiful Ring of Fire.
The Theuern
Conference of 2003, in Germany, was an event at which three presenters,
Klaus Vogel, James Maxlow (in absentia), and I,
offered in tandem our theories of Earth expansion, focusing primarily on ocean
spreading. Ideally such a meeting should have facilitated an opportunity for
making critical comparisons. But, because all three of us used different media
-- globe models, PowerPoint, and video -- direct comparisons have proven to be
rather difficult. To better compare the three expansion models that were
presented, I shall attempt to translate all three onto the common denominator
of my video medium. I will include again animations of Wegener’s Pangaea and
add some illustrations pertaining to Ott Christoph Hilgenberg’s (and Klaus
Vogel’s) pioneering work.
Alfred
Wegener
The habit of Alfred Wegener, of
having a world ocean “Panthalassa” as a foil for the expanding Pangaea-crust,
at the opposite side of the globe, has persisted in earth science circles. For
instance, I was able to find the thumbnail images for this Wegener animation at
the website of the Geological Society of America. Today many subscribers to
Plate Tectonics theory still appreciate the convenience of subducting
excess ocean floors in Wegener’s Panthalassa -- in the mysterious Pacific -- somewhere
along the “backside” of our planet. When Alfred Wegener lopped off the
subcontinent of India, and permitted it to float freely among the
wandering continental scabs of Pangaea, he created an appetite for similar
geological marvels. Not only people who later subscribed to the Plate
Tectonics theory, but also Earth expansionists have indulged in the
“terrestrial surgery” that Wegener’s world of wandering continents has made
possible.
Ott
Christoph Hilgenberg
Hilgenberg
derived Antarctica from the Pacific -- while Australia was
clinging to the round of Antarctica down south. I take here the
liberty of completing his three-globe sequence by way of morphing toward a NASA
satellite image. Hilgenberg has sliced North America into three
segments. He severed Alaska to have it slide home along the
continent’s western coast. The remainder of North America he cut
diagonally. He postulated a mega-shear that severed the mountainous West from
the Great Plains.
Unfortunately for Hilgenberg’s
theory, this gigantic hypothetical rift has left no revealing topographical
scar and, had there been such a rift, uplift of the Rocky
Mountains would surely have been prevented. It took magma pressure from
underneath the settling Plains to raise the continent’s peripheral wrinkles.
And it took Earth expansion to flatten and to lower the Plains.
Klaus
Vogel
To the lasting credit of Klaus Vogel it must be said, that he has avoided Hilgenberg’s
continental gash.
He has reversed Hilgenberg’s
starting positions for Antarctica and Australia by way of
placing Australia to the north of Antarctica. Hilgenberg’s rift,
that was supposed to have split Alaska, Klaus Vogel has re-routed to
bypass most of that problem. But even in Vogel’s reduced problem area, across
his amputated Alaskan Peninsula, his hypothetical shear lacks the evidence of a
topographical scar -- as did the two mega-shears of Hilgenberg, earlier.
The Aleutian Islands, today,
are curved evenly between Asia and North America. To obtain such
an even bow, both ends of the “stick” needed to be held fast. It seems
impossible to have had one end of the Aleutian strip slide all the way
from California to Alaska, and still achieve, in the end, an even
curve that is welded seamlessly onto Alaska. Matters could still be well
with Klaus Vogel’s hypothesis if, following the Second World War, the ocean
floors of the planet had not been explored as thoroughly as they were.
Even without the problem of the
Aleutian bow, projecting a Jurassic rift into the eastern Pacific
and Arctic Ocean is problematic by itself. Vogel’s crescent-shaped
sliver of an Ur-Ozean would have had
to exist in an area that now features the youngest sea-floors -- with none
being older than the Eocene.
James
Maxlow
From among the current Earth
Expansion theories I am taking the tectonics of James Maxlow
most seriously. The methodologies of both Maxlow and Luckert are based on isochrones-data found on maps of the
ocean floors which pioneers of the Plate Tectonics Revolution have produced.
James Maxlow
has avoided the gash that Klaus Vogel has projected across the Arctic. He
pays attention to magnetic striping and ocean floor chronology in the northern
Pacific and he begins his Pacific Ocean, as he should, with a Jurassic
triangular gap.
Maxlow extends his Jurassic Pacific
eastward -- as he opens up a crescent-shaped sliver there, similar in shape to
the Ur-Ozean of
Vogel. One wonders about the ease with which a blue extension of
Jurassic ocean is painted Cretaceous green, in the next thumbnail image. It is
impossible to animate this change. I can only try to be helpful and fade
Jurassic blue to dark Cretaceous green. But fading one color into another does
not solve a tectonic problem. It only conceals.
From eastern Asia, Maxlow pulls away Australia with Austral-Asia in
its tow. One wonders whether all the continental scabs and shelves, which now
stretch between Japan and Australia, could have been pulled from the small
Jurassic continental patch which Maxlow has allowed.
If his movement of Australia were correct, should not the smooth
curve that now runs along Sumatra/Java have been bent along the northeastern
edge of Austral-Asia instead? Somewhat like this?
The Indic Ocean
For the confirmation of my doubts
I must turn to the Indic Ocean. Maxlow’s
overall tearing pattern of the Indic Ocean, especially of the
northeastern portion, presents a serious problem for me.
According to James Maxlow’s isochrones-drawings -- from which I have removed
the fluctuating equator -- the Indic Ocean has unfolded in this
manner. The isochrones do delineate a distinct triangular patch of Eocene ocean
floor, west of the Andaman Islands and Sumatra. His projection,
back into pre-Eocene times, does obscure the Eocene triangle with a bulge of
continental shelf. While in this instance it is possible to animate between his
thumbnails, we are nevertheless left with the tectonic puzzle of how a rounded
bulge could have vacated a sharply defined triangular patch of Eocene floor -- and
have done so while, concurrently, the whole of Austral-Asia was swirling
north?
In response to James Maxlow I would have to say that to me
the Indic Ocean does appear differently. I believe, that the
Ninety-East Ridge was the western edge of Austral-Asia, and that it was
stretched southward by general Earth expansion. What is at stake here is much
more than the formation of an Eocene triangle. An entirely different expansion
pattern for Austral-Asia, and of movement for Antarctica, is implied.
East
Asia’s Island Chains and Marginal Seas
If 58 million years ago our
ancestors had not been so busy running away from dinosaurs, and instead had put
a satellite into orbit, they could have seen Austral-Asia stretched southward,
somewhat like this. By the end of the Eocene, Austral-Asia was elongated
southeastward, and ever since then it has been ricocheting northwestward.
The Eocene triangle in the Indic
Ocean was torn open when the western edge of Austral-Asia, along the Andaman
Islands, Sumatra and Java, was bent eastward in an even curve, away from the
Ninety-east Ridge-line.
When a little while ago I played
my animation of the NASA satellite photo, your eyes probably have followed the
wanderings of Australia. But in this instance Australia is a
diversion.
Let me focus on East
Asia specifically. I take the isochrones-map and roll it back unto a
contemporary globe. We reduce the globe by way of subtracting from the ocean
floor all the recent stripes, down to the Paleocene. And then we can play the
Eocene Event forward, up to the present.
We can apply the same procedure to
a satellite image that, surprisingly, lets us look deep into the Pacific. It
reveals the outlines of the oldest patch of ocean floor on our planet. We
reduce this hemisphere down to the Paleocene by removing all the recent
stripes, and now we are ready to observe the surprisingly smooth unfolding of
the eastern Asian marginal seas -- the Philippine Sea, the East China Sea, the
Sea of Japan, the Sea of Okhotsk, as well as the Bering Sea. This is
how East Asia obtained its marginal seas and its island chains. Down
south, Australia pushed against Celebes and thereby
squeezed open the South China Sea and the Philippine Sea.
It goes without saying that with
the shrinking of eastern Asia, during the Eocene, spectacular mountain
ranges were created on the mainland.
Nine-Figure-shaped
Ocean and Continent
In a slightly larger context, I am
postulating that the rounded Nine-shape of Antarctica came
from the rounded space of the Nine-shaped Pacific
Ocean which, for present-day emphasis, still happens to be encircled by
the rounded Nine-shaped Ring of Fire. Of course, the cavity
that was left by Antarctica has, over time, been expanded several
times its original size.
Like Hilgenberg, Vogel, and others
before him, James Maxlow remains faithful to the
tradition that was begun by Wegener, of trying to fit some round contour
of Antarctica into the Bight of Australia. I personally think that
this solution has, all along, been a mistake. While the “roundness” in each
does tempt the human mind to make an association, wherever two continental
crusts are supposed to match, size also is a significant factor. The round
of Antarctica is everywhere too large to fit into the Bight of Australia,
and upon an expanding sphere there is no way to explain why the Bight of
Australia should have been shrinking. But, inasmuch as “roundness” is being
judged by most people as being more interesting than “size,” I am willing to
quarantine this crucial datum -- for the moment.
The
Central Spreading Rift
For me there looms a still more
fundamental question. Spreading happens nowadays in the Atlantic, the
Indic, Arctic, and in the younger eastern Pacific, all along the
interconnected worldwide oceanic rift. Is it thinkable -- as the Maxlow-animations suggest -- that since Jurassic times and
throughout the Paleocene, the Pacific Ocean was spreading without the
presence of a central rift? I should think not.
I suspect that the older Pacific
was created by the same process that we can observe today in all the oceans.
For this reason I pay attention to the fact that the
northeastern flank of the Pacific patch of Jurassic floor does show offsets
which suggest ancient transverse faulting. Transverse faults could have been
developing alongside the flank of a central spreading rift.
I postulate that the Jurassic
remnants that now can be found along Antarctica do match the
northeastern edge of the Pacific Jurassic floor. This observation is
corroborated by the tear-drop shape of the Paleocene Antarctic plate which
nicely fits into what has become the eastern Pacific.
Once this possibility is
acknowledged, one can visualize an ongoing central spreading rift in the
Pacific that begun already in Jurassic times. Then, when the Antarctic Plate
was loosened from North-America during the Eocene, as it was moving southward
(or rather, “being spread southward”), the Pacific spreading rift and the
severance rift that was shared with North America merged in
the “wake” of that plate.
Of course, this “merging” of the
two rifts is figurative speech. While the wake behind the moving plate was soft
and flexible, no actual spreading rift was necessary or even possible. A joint
rift became possible when the crust was sufficiently hardened and ready to
crack. One may also suspect that in the wake of the moving plate most forms of
oceanic life have become extinguished. This means that we face a discontinuity
when we attempt paleontological dating.
Geological happenings in
the Indic Ocean, during the Eocene epoch, were part of a larger
pattern of events that involved Australia and Antarctica, as
well as South America. This combined Eocene “event” opened and widened the
entire (Pacific and) Southern Ocean.
Nostalgic
Methodology
Focusing my subject matter for
additional contrast, it may be helpful to approach the Eocene epoch and
the Pacific Ocean first with a feeling of nostalgia for the time
before any of us needed to worry about tectonic plates, isochrones, and ocean
floor chronology.
For this reason, I have selected
three NASA satellite photographs, of the southern hemisphere, which are
centered on points that tectonically may have (could have) converged on our present South Pole. As I have dealt with
the Indic Ocean earlier, so I will choose the Paleocene epoch as
my staging point for the expanded “Eocene Event.” I believe that during the
Eocene epoch, which followed the Paleocene, some connections between continents
have been broken and some positions have been
altered.
With no isochrones to worry about,
back in the good old days, we could have contemplated my Paleocene
reconstruction and then focused on the NASA image of the present Earth. The
task would have been to separate Antarctica, over a time of 43 million
years, from Point “A” to Point “B.” Scientists always prefer the simplest
possible route. Therefore, by placing a couple of thumbnails between “A” and
“B,” the animation can begin. I can complete this procedure without inflicting
excessive separation unto Antarctica. Most proponents of Plate Tectonics,
as well as of Earth Expansion, in the past, have engendered similar and even
greater conjectures.
The
“Eocene Event” (ca. 58-37 mya)
But geological reality and Plate
Tectonics are more convoluted. From Jurassic to Eocene times the Pacific has
widened, and the continent of Antarctica has grown by surrounding
itself with ocean floor crust. In other words, Eocene Antarctica could not move
anymore as a continent, but only as being contained in a larger plate. Its
movement required space between itself and Austral-Asia -- more space than a
simplistic animation has available. In our simulation
we must allow enough space for the Antarctic plate, to slip into the capacious
Southern Ocean, where it could have turned.
As I read the isochrones-map, it
was the circum-global belt of continents -- consisting of South-America,
North-America, Asia and Austral-Asia -- that Earth expansion has
stretched, still a considerable span of time into the Eocene. The first fifteen
million years of the Eocene epoch (58-43 mya) are
characterized by slow severance between the tip of South-America
and Australia, and between Antarctica along the western shores of
Middle- and South-America.
The Atlantic end-point of the
tear-line had been established already during the Lower Cretaceous, where the
Cape of Africa broke away from the toe of South America. Then during the Paleocene a gash was torn into the global belt from the
other side, along Tasmania. Finally, during the early Eocene an even curve
was sliced all the way to the Atlantic. The global belt tore in a curve
along the Australian Great Bight and the Cape of South America.
The remaining six million years of
the Eocene (43-37 mya) brought cataclysmic speeds of
continental separation between Australia and South America. By
the same jolt of rupture that loosened the circum-global belt, the Antarctic
Plate was sprung loose from North America, along a widening rift. The
Plate was invited to slip southward into the soft region that was opening up
between South America and Australia. To all these happenings I refer,
collectively, as the “Eocene Event.” The greatest continental movements (read
“separations”) on our planet seem to have occurred between 43 and 37 million
years ago.
Of course, this process happened
more tightly than I can animate here without damaging the contours. In
addition, my morphing tool has the bad habit of shrinking everything that
turns. So, please visualize this progression as happening a little more tightly
than I am able to show.
The Eocene epoch has ended with a
squeeze-play between Australia and South-America, whereby
Antarctica was caught in the middle and was shoved against
the cape of South-America. In general, the continents do not
collide, because they are cushioned by ocean floors that lie between them. So,
this Eocene rebound-collision may be the only one that has happened on our
planet.
When Australia snapped
northeastward it scooped and pushed some of the older ocean floors against
Antarctica, and it pushed Antarctica against the foot of South
America where it fractured the toe. It scooped the tip of South-America
eastward into the Atlantic as far as the Islas Orcadas
Rise.
Today we can
see Antarctica leaving the scene of a minor
accident. Antarctica’s gradual disengagement began during the Oligocene.
We know this because in the Scotia Sea one finds -- amidst a lot
of debris -- some Oligocene patches of ocean floor. Of course, during
cataclysmic continental adjustments most oceanic forms of life have been
eliminated, and the discontinuities that result do make paleontological dating
somewhat difficult.
Polishing the Metaphor
New theories tend to get
remembered by the simplest motion that they imply. Wegener’s continents became
famous as wanderers -- and mine -- let me say that most of the continents are
still “clinging” to the partners with whom they have slept encrusted for
billions of years.
Nevertheless, it is necessary to
mention the exceptions. Africa has left South
America during the Cretaceous, and with a break in the global belt, during
the Eocene, Australia and South-America got severed. While
celebrating their separation, the Antarctic Plate was invited to “dance”
southward between them, half a turn. Australia pushed the whirling
dancer against the tip of her former mate, South America. Finally, after
the Antarctic Plate had wedged its tip into the southern Indic Ocean,
Australia stepped back from this encounter and curtsied, at Celebes.
Only one continent on Planet Earth
appears so far to have achieved complete emancipation. It is Antarctica,
the whirling occupant of the South Pole. Our other five continents have shunned
such reckless freedom. They remain draped over the North Pole, together, as
leftovers of the original Pangaea crust. Australia’s shelves have snugged
up to Eurasia while the shelves of Eurasia are reaching
around the North Pole to hold on to North America which, in turn, has
locked arms with South America. In the same mode of Arctic
togetherness and anchorage, Africa accepts the hold
of Eurasia that embraces the Mediterranean Sea, and
thereby Africa, too, still clings to the original Pangaea configuration.
A 2004 PostScript:
At the
regional GSA conference in Boise, Idaho, on May 5, 2004, I learned that the
coastal mountain tops, along the states of Washington and Oregon, all do
feature basalts from the Eocene [exactly the break-up time which is implied by
my theory of Antarctica’s partition from the Pacific]. Two scholars
from Puget Sound University suggested a scenario of “extensive
rifting” -- without being able to name a plate that might have gotten torn away
from there. This independent fact should at least persuade some earth
scientists to admit my theory as a “working hypothesis,” alongside others.