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Secrets Of The Sea
by George Palmer
George is an attorney working on a M. A. degree from the
Rosenstiel School Of Marine & Atmospheric Science, a division of University
of Miami. Mr. Palmer will provide our readers with a unique look into a
variety of topics, some serious, some lighthearted. His topics may include
maritime law, aquaculture, environmental law and policy as it relates to the
sea and coastal zones, marine cultural resources, fisheries and much more!
He is a free-lance writer, and his thoughts, opinions and writings don’t
necessarily represent those of, The Weekly Fisherman. Now that we have the
disclaimer out of the way...enjoy!
You can contact Mr. Palmer by email at
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Right
There on Your Plate |
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Please pardon the pun, but my
publisher tells me we have been inundated with questions since the
recent Tsunamic catastrophe in southern Asia. Some time back, I wrote a
Secrets of the Sea column on tsunamis that you might have missed.
Therein I explained that the term “tidal wave” is a misnomer for the
devastatingly large waves such as the one that has recently caused so
much death and destruction. In fact, the correct terminology is
“tsunami”, which in Japanese (who have the most problems with these
natural disasters) means “harbor wave.” I have responded to emails about
the phenomena, and the biggest question is how they occur and are
created. This column will, I hope, answer in lay terms, that question.
First, let’s clear up one misconception. A tsunami is a huge
wave that, once it reaches shore, causes unspeakable calamity. However,
the fact that it is a wave has absolutely nothing to do with the tidal
occurrences in our oceans. The positioning of cosmic bodies, primarily
the moon and sun, causes tides. Tsunamis find their causation in
oceanic disturbances such as earthquakes. So, exactly what happens out
there in the depths that can cause problems on land? Well, it has to do
with the earth’s “plates” and the movement thereof.
Geologically speaking, a “plate” is a large, rigid hunk of
rock. These are constantly moving, although at a speed indiscernible to
the naked eye. But they are moving. This movement is a good way to
describe the word tectonics, which comes from the Greek verb meaning “to
build.” Earth has a dozen or so plates that kind of slip and slide along
a layer of liquid beneath them. This liquid acts as kind of a geological
ski slope on which the plates glide. Prior to our gaining knowledge of
plate tectonics, it was believed that continents “drifted” over the
oceans, which was the theory of “continental drift.” In fact, one
theory, long held, is that the world originally had a super-continent
called Pangaea, which eventually broke apart and formed various
landmasses that drifted and shifted around until they reached present
day status.
The theory of plate tectonics is only about thirty years
old. However, it is now widely accepted, and has combined many areas of
science, including geology, geography, paleontology, archaeology and
seismology. This theory has given us valid explanations for questions
such as why earthquakes occur where they do, volcanoes erupt when they
do, and how mountain ranges are formed. And remember, this is all still
going on as we speak.
In 1912, a young scientist named Alfred Wegener introduced
the idea that continents were moving. He postulated that two hundred
million years ago, Pangaea began to split apart. Wegener froze on an
expedition before fully developing his theory, but one of his disciples
further developed the idea, stating that Pangaea initially split in two,
forming two world continents, one in the northern hemisphere and another
in the southern. What a war these guys could have had. Of course, there
were no such things as humans at the time. These two continents, so the
theory went, continued to divide, drifting over the millennia until we
reached the present day situation. If you look at a world map, you will
notice the uncanny fit of the coasts of South America and Africa, now an
ocean apart. Also, there are identical fossils on each coast, which
could mean that they were once attached. Of course, Wegener’s guys knew
that this all took millions of years. It did not occur overnight. Prior
to this time, the prevailing view had been that the position of the
world’s landmasses had been caused by a catastrophic event, most likely
the Biblical flood. You go, Noah! But such is not the case. Continents
were not, nor are they now, permanent fixtures. Now, can you guess what
the problem with the theory of gradual drift might be? Well, what force
is there on earth that would move these continents? Gravity? No, that
goes up and down. Wind or water? Uh uh. Not strong enough. So
continental drift as an explanation was debunked and set aside. The
thing is, though, that Wegener’s theory led the modern world to the
supposedly correct theory, which is that of plate tectonics.
In the 1950’s, four things were learned that brought Wegener
and his ideas back to the forefront of earth science. First, technology
made it known how rugged and youthful the ocean floor is. Before the 19th
century, everyone believed that the ocean floor was flat, with no
topography. Now we know that most of the occurrences of a geological
nature on land are directly or indirectly linked to ones on the ocean
floor and that the seabed is anything but flat. There are deep valleys,
mountains higher than Everest, craters, rills, ridges and anything else
you might see up top. Additionally, in 1947 it was learned that the
sediment atop the ocean floor was much thinner than earlier believed.
Scientists’ best guess was the oceans are about 4 billion years old. If
so, how could there be such a thin layer of sediment. It should have
been very thick. Plate tectonics provide an answer.
There also have been many reversals of the earth’s magnetic
fields in the past. It is a difficult scientific explanation, but
basically there are two different types of magnetic rock on the sea
floor, laid out in stripes like on a Zebra. This is called “magnetic
striping.” They form along ocean ridges. There are weak spots in between
the stripes that allow molten magma to rise to the surface. The rising
of this magma is known as “sea floor spreading.” This has formed what is
known as the mid-ocean ridges, which is important to the theory of plate
tectonics. The most significant thing about sea floor spreading is that
new earth crust is constantly being formed. This crust has to go
somewhere. So it moves. It pushes. Are you starting to get it?
The third thing that happened was the development of seismic
instrumentation. This enabled us to find that earthquakes happen in some
areas a great deal more often than in others. It was found that
earthquakes were much more common along oceanic ridges. Scientists now
believe that sea floor spreading, and the constant “recycling” of the
ocean floor, is one of the causes of all these earthquakes concentrated
parallel to the oceanic ridges.
Finally, satellite imagery shows beyond a doubt that things
down there are moving all the time. There are processes known as
convergence and divergence, and subduction. Subduction is apparently the
real big deal. Plates grind up against each other, bump each other, and
contend to be “top dog.” When one plate slips underneath the other,
subduction occurs, and quakes are likely. Additionally, the subduction
process causes the formation of volcanoes beneath the water. Eventually,
after such volcanoes erupt enough, they build themselves up to the point
they become island volcanoes, like Hawaii.
So, scientists now believe that it is the process of plate
tectonics, the shifting of the earth’s crust, and the dynamics thereof,
that cause the problems. When things down there start bumping and
grinding, slipping and sliding, something’s got to give, and usually
that involves an earthquake. So then what happens?
When a major earthquake occurs along a subduction zone, then
is the time to watch out! This is especially hazardous, because the
formation of a Tsunami is likely to occur. Tsunamis are seismic events,
waves, if you will, caused by the quakes, volcanic eruptions, and
underwater avalanches. The latter two are very rare. Normally the
culprit is that earthquake. When a large earthquake happens down below,
the seabed crust can move several meters. This may not sound like a
great deal, but the results are. Enormous quantities of water are set
into motion, rocking back and forth for hours. This rocking causes a
series of waves, which can race across open expanses of water at speeds
exceeding 700 mph. That’s about how fast passenger jets go. They travel
for great distances, often unobserved, until they find shallow water,
rise to heights of up to 100 feet, and do their thing to the land.
Let me tell you this. Prior to the most recent tsunami, the
worst catastrophe in terms of human life was some time ago, in which
26,000 lives were lost. That, friends, is miniscule to what we are
experiencing right now. Some reports have the death toll at 150,000 and
rising. Property and environmental damage cannot possibly be assessed at
present. Lots of people are talking about the fact that these poor
people were not warned. But, in reality, you tell me. What could have
been done? We are a long way from preventing small tropical storms, much
less earthquakes and resulting tsunamis. There are all kinds of relief
funds through which we can help these unfortunates. Think about it.
Interestingly, where do you think would be the safest place
when a tsunami is approaching? Well, what do you naturally do when a
wave is about to crest right on top of you? Dive under, right? So, if
you have enough warning (unlikely), put on your scuba gear and go out to
Crocker’s. You’ll most likely be the safest person in the Keys. Of
course, there won’t be anything left when you come up.
But now, you know how they happen. It was right there on
your plate. Thanks for reading, and keep it up. We love those emails and
other contact with the paper. It let’s us know you’re there.
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