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The AAPG/Datapages Combined Publications Database
Houston Geological Society Bulletin
Abstract
Abstract: The Northern Sumatra Earthquake of 2004:
Forty Years of Ignoring Plate Tectonics
By
Director PetroleumReports.com and
Houston Geological Society Bulletin Editor
The December 26, 2004 Northern Sumatra Earthquake has
been recently recalculated to be magnitude Mw = 9.3, making
it the second largest earthquake in recorded history along
with Maullín, Chile (1960). Due to the magnitude of the
December 2004 earthquake and ensuing
tsunami
, these types of
events are widely viewed as beyond the range of scientific predictability
or probability.
More disturbing than the presumption that the Sumatra earthquake
and
tsunami
were beyond probabilistic determination is
the nearly universally held notion that what is needed is a deep-ocean-
buoy monitoring and warning system, like the Deep
Ocean Assessment and Reporting of Tsunamis (DART) network
in the United States and Japan. The DART system is extremely
expensive and has never been proven to predict a
tsunami
. Initial
tsunami
waves arrived in 15–30 minutes of the earthquake in
Aceh Province, Sumatra, one hour in Thailand, and two hours in
Sri Lanka and India. The frequency of DART transmission (once
every hour) and associated processing time is inadequate to have
provided meaningful warning for any of the areas most affected
by the 2004
tsunami
in the Indian Ocean.
In the case of the
tsunami
that destroyed Hilo, Hawaii, following
the 1960 Maullín, Chile earthquake, ample warning was provided
from seismological information alone, yet many deaths and
injuries occurred due to lack of awareness about the behavior of
tsunamis.
Tsunami
detection is, after all, a second derivative approach.
Why not focus on the causal mechanism—earthquake—which is
something we can measure very effectively and quickly? I believe
that an appropriate, immediate response to the Indian Ocean
tsunami
disaster should focus on:
- Immediate awareness training about tsunamis for all coastal residents of the Indian Ocean region,
- Immediate implementation of a seismological first-warning system that uses existing monitoring stations in the region along with an inexpensive network of coastal sirens, and
- Assessment of the feasibility and cost benefit of a deep-ocean-buoy
tsunami
warning system like the U.S. DART network.
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