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Indonesia hit by another devastating earthquake
By Peter Symonds
30 March 2005
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A massive earthquake off the west coast of the Indonesian island
of Sumatra has left hundreds of people confirmed dead and thousands
homeless. News of the quake late on Monday night (local time)
and fears of a repetition of the December 26 tsunami triggered
a mass exodus from coastal areas in Indian Ocean countries.
While no significant tsunami formed, the huge tremor measuring
8.7 on the Richter scale laid waste to areas immediately adjacent
to the epicentre. Indonesian Vice President Yusuf Kalla estimated
that the death toll on the islands of Nias and Simeulue could
be as high as 1,000 to 2,000 people. Television footage showed
survivors in Gunungsitoli, the main town on Nias, frantically
searching through the rubble of buildings searching for friends
and relatives.
From the air, about a third of Gunungsitoli appears to have
been flattened. There is no electricity or running water and damage
to the local airport hampered relief operations yesterday. Deputy
mayor Agus Mendrofa told the media that 10,000 of the towns
population of 27,000 had fled to higher ground. Gunungsitoli
is now like a dead town. The situation is extreme panic,
he explained in the London-based Times.
According to the Australian, 80 percent of the islands
second largest town of Teluk Dalam has been destroyed. Town chief
Ginding Nabari told the newspaper that at least 13 people were
dead. But there will be more, he said.
A UN Office for the Coordination of Humanitarian Affairs (OCHA)
report yesterday put the death toll on Nias alone at 200, with
more than 300 injured, many of them seriously. Around 1,780 people
were officially registered as internally displaced, but the actual
number of homeless is much higher. Media reports indicate that
damaged roads and bridges are hindering emergency operations in
the northern parts of the island, which were closer to the quakes
epicentre. The islands population is between 500,000 and
700,000.
On the neighbouring island of Simeulue, 18,000 people out of
a population of 78,000 are internally displaced. OCHA reported
that many of the concrete buildings on the island had been destroyed.
The initial toll was three dead and 47 injured at the Sinabang
Hospital, but again disrupted transport and communications make
any accurate assessment impossible.
Fears were held for the safety of an estimated 5,000 inhabitants
of the Banyak islandsa chain of small, low-lying islands
that were closest to the quakes epicentre. According to
the OCHA report, initial aerial reconnaissance yesterday indicated
little or no destruction. On the Sumatran mainland, the village
of Singkil was badly hit, but no casualty reports have been released.
The quake, while less forceful than the December 26 tremor,
was the worlds eighth largest since 1900. It was felt in
many parts of Sumatra and as far away as the west coast of Malaysia.
As reports of the quake filtered out, there were chaotic scenes
in the countries surrounding the Bay of Bengal. Throngs of people
in Sri Lanka, Thailand, Indonesia and India attempted to flee
to higher ground on foot, bicycle and motor vehicles. Conscious
of the lack of official warning three months ago, many did not
wait for alerts to be broadcast over TV and radio.
Rebuilding in many of the coastal towns and villages devastated
by the December 26 tsunami that claimed over 300,000 lives is
yet to even begin. Tens of thousands of survivors in these countries
are still living in makeshift emergency camps, temporary accommodation
or with relatives. They have been reduced to poverty, having lost
their homes, possessions and livelihoods. The lack of assistance
highlights the inadequacy of the much-vaunted international aid
promised.
Superficially, the reaction of governments to the latest earthquake
appeared markedly different from December. In Indonesia, President
Susilo Bambang Yudhoyono immediately declared a state of emergency
and postponed a visit to Australia in order to go to affected
areas. Three months ago, his administration blocked international
aid to the stricken province of Aceh and the Indonesian military
took days before making an aerial reconnaissance of the devastated
west coast of the island.
In Thailand, India and Sri Lanka, authorities issued immediate
tsunami alerts and praised themselves for the promptness of their
actions. Unlike last December, when he failed to make a statement
on the tsunami tragedy for days, US President George Bush immediately
expressed his condolences for the victims of the latest disaster.
In Australia, Prime Minister John Howard followed suit, pledged
$1 million in financial assistance and dispatched military transport
aircraft and a medical team to take part in relief efforts.
Lack of a warning system
There is no doubt that these responses were purely for public
consumption. All of these leaders are acutely aware that their
obvious contempt and ineptitude last December provoked disgust
and anger among ordinary working people around the world, who
reacted in precisely the opposite fashion. But behind the latest
official displays of concern lie the same indifference for the
plight of the Asian masses.
Despite the obvious need, there is still no adequate tsunami
warning system for the Indian Ocean. Some changes have been made
over the past three months: the Pacific Tsunami Warning Centre
in Honolulu now has a list of contacts to alert in South and South
East Asia; and each of the countries has put in place its own
emergency and evacuation measures. Within 20 minutes of the latest
quake, the Honolulu centre issued a bulletin warning of its potential
to generate a widely destructive tsunami and advised evacuation
of coastlines within 1,000 km of the epicentre.
In the absence of other information, the bulletin was certainly
justified given the magnitude of the quake. But the makeshift
character of the present warning system is highlighted by the
failure of a tsunami to develop. Scientists are still speculating
on the possible reasons: while the tremor was of a similar size
to the December quake, it was in deeper water, was not as quite
as large, did not extend for the same distance and may not have
ruptured the seabed floor. Whatever the exact explanation, it
is well known that not every undersea earthquake produces a tsunami.
To determine accurately whether a tsunami has formed requires
a network of tidal level monitors and deep-sea pressure sensors
connected to a central monitoring centreas is in place for
the Pacific Ocean.
Despite a series of meetings over the past three months about
the necessity of such a system, scientists on Monday were limited
to largely the same equipment that was in place on December 26.
The first confirmation that a tsunami had not formed was provided
by a sea-level gauge on Cocos Islandhalfway between Indonesia
and Australiasome two and a half hours after the earthquake.
If we had [readings from] water-level instruments within
the first half-hour to 45 minutes, we could have point-blank told
people in Sri Lanka and Thailand, Dont worry,
Barry Hirshorn, a geophysicist at the Honolulu centre, told a
local newspaper.
Plans for an Indian Ocean tsunami warning system have bogged
down in national rivalries and arguments over who will foot the
costs. Both the Indian and Thai governments have announced their
intention to build their own warning systemsignoring
the obvious need for regional and international coordination and
cooperation. While Germany has offered to pay for the relatively
modest $35 million needed to build a warning system, it is unlikely
to be operational before mid-2006.
A number of experts are warning, however, that there is a possibility
of further large earthquakes in the same region. While unable
to make accurate predictions of tremors, several scientists have
pointed out that the December 26 quake has generated new stresses
in fault lines in the region, making new earthquakes more likely.
In fact, a scientific group at the University of Ulster published
a paper less than two weeks ago, warning of new quakes in two
specific areas. One was near the epicentre of Mondays quake
and the second was along a fault line running down the centre
of Sumatra, including under the city of Banda Aceh. In comments
at the time, Professor John McCloskey stressed the urgency of
building an adequate warning system.
The loss of much of the life in the December earthquake
was avoidable, he explained. The science is well understood,
the warning systems are in place in the Pacific region. The levels
of preparedness, public awareness and education in this region
are high and do save lives. Unfortunately the people of the Indian
Ocean have neither benefitted from this knowledge nor from the
available technology. Our results indicate unambiguously that
there is a real danger of another earthquake in the region. It
is vital that disaster fatigue does not delay the implementation
of the Indian Ocean Tsunami Warning System.
Speaking after Mondays tremor, McCloskey again warned
against complacency. We have all heard that lightning does
not strike twice in the same placebut earthquakes do. One
of the strongest observations in seismology is that earthquakes
cluster in space and time. Where you have one earthquake you are
likely to have others, he said.
Prior to the December 26 tragedy, governments in the region
and internationally for years ignored calls by scientists for
an Indian Ocean tsunami warning system. There is no guarantee
that the latest quake and expert appeals will accelerate plans
for such a system. It is far more likely, once the immediate crisis
has passed, that there will simply be a collective sigh of relief
in ruling circles around the world. Just as tens of thousands
of tsunami victims have been left struggling to survive as best
they can, the plans to build a warning system, let alone construct
buildings and infrastructure capable of withstanding natural disasters,
will remain limited and half-hearted.
See Also:
The social roots of the tsunami
disaster
[22 January 2005]
The Asian tsunami: why there
were no warnings
[3 January 2005]
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