You have already read, heard, and seen pictures of the
extent of the recent devastation. This report is focused on different
information, which you are unlikely to learn about—but which will help you
as you prepare for what is ahead.
On December 18, 2004, Dr. Kerry Sieh, an American expert,
presented a paper at a conference in San Francisco, warning that the next
giant earthquake off Sumatra could happen at any time. He said it could lift
the ocean floor six feet, causing a massive tsunami which would wreck
coastal areas over a very wide region.
Earlier in that year, Sieh was so concerned about the
danger that he had toured parts of Indonesia, lecturing officials about the
dangers. But he found that no one seemed to care. For the most part,
officials, high and low, just did not believe him. Sieh probably felt like
Noah warning the Antediluvians. Although small earthquakes had been felt for
years, everyone was used to them. It all seemed like an abstract theory;
and, besides, experts said such a catastrophe might not occur for decades.
So why worry?
Sieh had even distributed posters in Sumatra, in the hope
that they would be posted where the people might see them. Whether or not
they were put up, he did not know. Very likely, they were trashed, lest the
tourists become worried.
Seismologists elsewhere in the world knew gigantic quakes
occurred every so often. And, because of their instruments, they would learn
sooner than most when an immense earthquake would occur; however, no warning
system was in place in the Indian Ocean.
In 2003, one Australian seismologist, attending an
international conference on tsunamis, had urged the scientific community to
install such a warning system in that ocean. All those present agreed it
should be done. But who should do it? The scientists were busy; and the
governments in the region probably would not be interested. So the matter
was dropped.
Seven years earlier, Samith Dhamasaroj, Thailand’s
leading seismologist, had warned Thai government officials that a tidal
(seismic) wave could hit the entire coastal area and would be closest to the
tourist town of Phuket. "I predicted the possibility, but nobody paid any
attention." He had made two recommendations: Install alarm sirens in the
hotels and locate no resort buildings closer than 300 yards from the
beaches.
Ignoring the warning, the government moved Dhamasaroj to
another post of duty. They did not want to do anything that might upset
visitors from overseas. The tourist industry was increasing fast and
becoming the major source of income for Thailand. More and more resorts were
being built on all the beaches.
The last giant seismic wave to produce immense damage all
across the Indian Ocean was when the volcano of Krakatoa exploded in 1883.
The eruption darkened the skies with ash and lowered temperatures throughout
the world.
That explosion produced an immense tsunami, with massive
numbers of casualties, just as this present one has done.
Research studies of coral atolls indicate that clusters
of gigantic earthquakes tend to occur about every 230 years. The most recent
cluster began in 1797 and ended in 1861. So any month or year now, more big
jolts could occur.
On Sunday morning, December 26, 2004, shortly after Bayu
Pranata, the local geophysics officer in Padang, Central Indonesia, began
his shift at the seismic center—it happened.
At 7:58 a.m. hearing a strange sound, he looked out the
window to see what it could be. Then he realized that the tuk-tuk-tuk sound
came from a seismometer—a gauge in the room he was in. It was busily
recording powerful seismic activity somewhere not far away.
Shocked, Pranata hardly knew what to do. Apparently it
was a powerful earthquake which appeared to be about 8 on the Richter scale.
Fearing that the quake could cause a gigantic tsunami, he telephoned the
National Earthquake Center in Jakarta; but there was no response. Pranata
wept.
A powerful movement had occurred about six miles below
the floor of the Indian Ocean. Like lightning, the shock wave sped outward.
Unlike ordinary waves, which are whipped up on the surface of the ocean by
the wind, tsunamis are waves that speed outward in every direction as a
gigantic impact jolt, extending from the surface to the floor of the ocean.
As an earthquake lifts the ocean floor, it heaves up a
mass of water thousands of feet deep which then falls back. As the sea
flattens out again, gigantic ripples race outward. A tsunami is born!
Enormous energy, contained in billions of cubic yards of moving water, races
outward.
In the open ocean, that energy wave can travel at 500 to
700 miles per hour. The deeper the ocean, the faster it will travel (because
it is impeded the least). Yet it may only be barely detected on the surface
as a long, low swell whose crests may be hundreds of miles apart and only a
few feet high.
A tsunami can travel great distances without dissipating.
In 1960, an earthquake off the coast of Chile produced a seismic wave that,
in 22 hours, traveled 10,000 miles—and slammed into Japan.
As this mass of energy hurtles outward, it gradually
nears an island or coastal area. The ocean becomes more and more shallow.
This intensifies the force of the energy wave—and it comes crashing onto the
shore at great heights, depending on the magnitude of the initial earthquake
shock. The height of the wave may be 15 feet or much higher. This one on
December 26 was reported as 30, 35, or 40 feet high.
That wall of water just keeps rushing forward, hardly
losing any height, until hills and mountains are reached. If there are no
elevated areas, the wave moves right across the entire island. Later in this
article, we will consider past tsunamis which were over 100 feet high. It
can happen!
Not long after Bayu Pranata, in Padang, saw squiggles on
his seismic charts, an automatic computer alert sent a seismologist rushing
to his office in Australia.
Within 33 minutes after the quake, he issued a tsunami
warning—but sent it only to Australian embassies. Officials in nations
bordering the Indian Ocean were not warned, for fear of breaching
"diplomatic protocol." Those big words mean that the orderly way for
Australia to send messages to other governments is by contacting the
Australian embassy in that nation, who then in turn eventually pass the
warning along.
Precious time was slipping away.
In India, the seismic department dispatched an urgent fax
to warn a government minister—but sent it to the wrong person. And there it
set for awhile unopened.
A few minutes later, a seismic device at Nagano, Japan,
began erupting. Masashi Kobayashi stared at it in disbelief. "I thought it
was huge," he afterward said. "Our equipment calculated its magnitude at
over 8, and that only happens a few times a year."
That seismometer triggered a calculator which immediately
began comparing the jolt with 100,000 previous tremors in its memory. Yes,
this was a big one.
Kobayashi immediately sent an alert to the Japan
Meteorologic Agency in Tokyo. But they were not certain what to do with it;
since the Indian Ocean was not in their tsunami warning network.
Very soon, computer alarms began sounding at the seismic
center in Honolulu. The first scientist to look at the blue quake lines on
the graph thought it might be 7 on the Richter scale; but soon they realized
it was 8 or over. A huge earthquake!
A routine bulletin was issued, which predicted small
changes in sea level, but added the comment that there was "no tsunami
warning in effect" for the Pacific region. So relax everyone; it doesn’t
affect us.
Valuable time was slipping by as the scientists gradually
realized that this was 9 on the Richter scale! The way it is calibrated, a 9
is 32 times more powerful than an 8.
It was clear to the scientists that this powerful
undersea blast was centered in the Indian Ocean, not far from Sumatra (part
of Indonesia).
A terrible tragedy was in the making; for the seismic
wave, created by the quake, would soon hit many coasts. But what should be
done? Who should be notified? It was a major holiday weekend for America;
and most of its seismologists were gone till Monday. As for authorities in
the nations bordering the Indian Ocean, they had no phone numbers for any of
the coastal towns or tourist resorts. Oddly enough, they did not even have
phone numbers of government offices!
"We tried to do what we could," said Charles McCreery,
director of the Honolulu Earthquake Center. "We don’t have contacts in our
address book for anybody in that part of the world."
Some of the most sensitive earthquake equipment was the
network of the Comprehensive Nuclear Test Ban Treaty Organization, which
uses seismic equipment to listen for forbidden nuclear bomb blasts. The
headquarters is in Vienna, Austria. Using 300 monitoring points circling the
globe, it is able to gauge seismic activity, undersea disturbances, and even
changes in the atmosphere!
This equipment was well-able to provide all of the rim
nations around the Indian Ocean with accurate, fast warning—since many of
the sensors were right there in that area of the world.
Like clockwork, the machines began whirring and recording
the invaluable data, able to save thousands of lives.
But there was no one to pay any attention to it. Everyone
had taken off for a long Christmas holiday weekend. The place was empty.
By now, an hour or so after the main quake (although some
experts were at their posts and knew about the tragedy in the making), no
one knew how to warn the islands and coastal areas in the oncoming path of
devastation.
Not one general warning got through to anyone of
importance in any of the nations that needed to hear those warnings.
For example, it took an hour and a half for the tsunami
to reach Sri Lanka. If they had been warned, thousands upon thousands of
people would be alive today.
By the time the earthquake wave had traveled 3,500 miles
and was nearing the coast of East Africa, news of the horrible disasters and
loss of life in Asia had preceded it. The waves still produced terrible
destruction, especially in Somalia; but in one nation—Kenya—word of the
thousands of deaths had arrived. The authorities were able to evacuate the
people. However, the warning had come from news of deaths in Asia, not
from seismic monitoring centers!
On one island in the Indian Ocean, Simeulue, most of the
people escaped unharmed. Over the decades, they had taught their children
about the seismic wave of 1907, which had killed thousands on the island.
The citizens never forgot the message; and, when they felt the quake, they
immediately fled to the hills behind the coastal areas. The majority of the
island’s 70,000 people remembered what their parents had taught them and
escaped the waves which followed the quake.
But there were others who also escaped:
Suddenly, with great beating of wings, thousands of
egrets and cormorants rose from the placid coastal water off Sri Lanka and
flew inland. Yet, to the people, nothing seemed amiss. Wildlife was sensing
what had occurred thousands of miles away.
Animals of all kinds, with no exceptions, rushed
inland to higher ground. Wild elephants trumpeted as they ran to safety.
Some elephants were carrying tourists at the time. They hurried to higher
ground, carrying their mahouts and astonished tourists with them—and saving
their lives. As soon as the elephants reached an elevation slightly higher
than the highest wave would later reach, they stopped. Eventually, the waves
arrived—and stopped at the feet of those elephants.
Elephants that were chained generally broke their chains
and ran off. In one instance, an elephant, as it ran, reached down and
picked up a child which had fallen and carried it to safety.
Men in charge of wildlife reserves saw the animals
fleeing to the hills. Throughout the entire devastated areas surrounding the
Indian Ocean—not one dead animal was found (unless it was tied securely by a
rope or chain, or inside a house and unable to leave). Planes and
helicopters, flying overhead, could not spot a single dead animal. None
could be seen on the ground by the survivors.
This entire tragedy occurred on a day when the weather
was mild, the sun was warm, and no tropical storms were anywhere. As for the
sea, it was unusually calm.
Is the United States in danger of a tsunami? The
newspapers may tell you that we are comparatively safe, because a special
Pacific warning system is in place. (It is a 26-nation network of seismic,
tidal, and sea-level monitors.)
Yet this is only a warning system; it is not going to
stop the waves! They will still hit the U.S. coast and cause great
desolation.
Seismic waves can be generated by earthquakes in various
parts of the Pacific Basin. As we have learned, each wave can travel
thousands of miles with little loss of energy. Every low-lying coastal area
on the West Coast is in danger.
Here is information on what could easily happen if a
powerful earthquake occurred along one of several underwater faults (crack
lines) in the Pacific Northwest:
Hundreds of minor quakes have been recorded along the
Juan de Fuca and Explorer cracks over the past 25 years. Those faults are
quite similar to the subterranean system of cracks that recently triggered
the gigantic tsunami in the Indian Ocean. The faults off the coast of
Oregon, Washington, Canada, and Alaska are capable of producing earthquakes
fully as large as the December 25 quake.
About 45,000 people in Washington State live within 0.6
miles of the ocean. In Oregon, about 90,000 people live within 0.6 miles of
the ocean. If a quake was powerful enough, it could drive a wall of water
toward Seattle and Vancouver. The Puget Sound basin has its own network of
faults—right next to those cities—which would be fully capable of generating
large earthquakes and seismic waves.
Flooding from a major earthquake would cover a sizeable
amount of inhabited coastal land in Vancouver, Seattle, Tacoma, and adjacent
areas.
Almost instantly, such a shock would overflow those
cities—almost before a warning could be sounded.
It is known that a very powerful earthquake, close to the
Puget Sound, occurred in 1700.
So much for Oregon and Washington. Southern Alaska is
also a dangerous place; and so is California.
Much of the population of the San Francisco Bay Area, Los
Angeles, and San Diego live and work in localities not far above sea level.
A warning system might give them advance notice (for those who heard the
warning); but the oncoming tsunami waves would inundate large areas,
regardless of how much warning the citizens had received. Very likely, the
water would pour in while many were still in traffic jams, trying to flee to
higher ground.
In 1883, Krakatoa volcano in the East Indies erupted; and
the entire island collapsed in 820 feet of water. A tsunami of tremendous
force traveled around Java and Sumatra, killing 36,000 people with walls of
water that reached 115 feet in height.
In 1896, on the eastern coast of Japan, waves, 82 to 115
feet high, smashed more than 100,000 homes and drowned 26,000 people.
In 1946 at Unimak Island, near Alaska, a magnitude 7.2
earthquake set in motion a seismic sea wave great enough to wipe out not
only Scotch Cap Lighthouse and five men inside—32 feet above sea level—but
also the radio antenna perched at 103 feet!! The wave traveled onward to
Hawaii and killed 159 people and produced millions of dollars of damage.
The 1964 Alaska earthquake produced great damage, not only from the quake
but also from tsunamis which repeatedly struck Anchorage and Valdez. —vf
The eruption of the Cumbre Vieja volcano, in the Canary
Islands, could trigger a "mega-tsunami" that would devastate Atlantic
coastlines with waves as high as 330 feet, scientists said on Wednesday,
December 29, 2004. More on this later in this brief article.
The largest island group in the Atlantic Ocean is the
Canaries. Because they can be reached by favorable winds from Europe and
Africa, the islands were an important base for early voyages to the new
world. Although they were claimed by Portugal in 1341, because the pope was
greater than kings—he gave them to Spain three years later! (But, ignoring
the infallibility of a papal decree, Spain took them back later and today
owns them.)
There are several volcanoes on the Canaries. One, on the
island of Tenerife is 3,715-meters high. Christopher Columbus recorded a
1492 eruption (probably Teide) on Tenerife. Over the centuries, one after
the other of the volcanoes has exploded, collapsed, or caused landslides.
Thick pumice deposits occur on the sides of all the volcanoes, showing
strong activity in past centuries.
In some instances, one volcano after another has blown up
within just a few months. For example, Siete Fuentes erupted on January 31,
1704. Volcan Fasnia on January 5, 1705, and Montana Arenas on February 2,
and Montana Negra on May 5, 1706.
The Las Canada Caldera formed after a major collapse at
an earlier time. Volcan Chahorra erupted in 1798; and another eruption blew
out its side on 1909. Many of these eruptions were quite violent. Orotava
and Guimar valleys, on the island of Tenerife, were formed when the steep
volcanic sides of Teide slid into the sea. It erupted most recently in 1909.
In the past, the northern segment of Teide has produced several landslides
into the ocean. Teide, elevation 12,188 feet, is the third largest volcano
on Earth, after Mauna Loa and Mauna Kea in Hawaii.
Then there is the Cumbre Vieja volcano on La Palma
Island. This is the one mentioned in the first paragraph of this brief
article, which experts especially point to as one the experts are especially
concerned about.
It is believed that such an eruption would cause a
massive chunk of rock to break off and crash into the ocean, producing a
gigantic wave of water that would crash into the coast of Eastern United
States.
Simon Day, of the Hazard Research Center at the
University College of London, said that Cumbre Vieja should be carefully
monitored for any signs of activity, so a warning could quickly be sounded.
Such a wave would devastate areas, some more and some less, extending from
South America, the Caribbean Islands, eastern America, Greenland, Iceland,
Ireland, Britain, Europe, and Africa. The energy released by the collapse
would be equal to the electricity consumption of the entire United States in
half a year. Immediately after the landslide, a dome of water (possibly
3,000 feet high and tens of miles wide) would form, then collapse and
rebound outward. Within 10 minutes, the tsunami would have moved a distance
of almost 155 miles.
On the west Saharan shore, waves would probably reach
heights of 330 feet. Florida and the Caribbean would be hit with waves that
could be 165 feet high, about 8-9 hours after the landslide.
Wave heights toward Europe would be smaller; but
substantial waves would hit the coasts of Britain, Spain, Portugal, and
France.
It is estimated that the water would penetrate several miles inland; and
the devastation would cause trillions of dollars in damage.
