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Online edition of India's National Newspaper Thursday, December 07, 2000 |
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Koyna earthquakes may become more frequent
WITH RECURRING earthquakes in Maharashtra, Indian geologists warn
the fault zone under the Koyna Dam has been weakened by annual
reservoir filling and that with the passage of time the region
will experience earthquakes even with slight fluctuations in
reservoir level.
Kusala Rajendran and C. M. Harish at the Center for Earth Science
in Thiruvananthapuram claim that the spatial and temporal
patterns of the recurring earthquakes in Koyna region suggest the
possibility of the fault zone becoming further unstable,
progressively lowering the stress needed to trigger an
earthquake.
Their conclusion is based on analysis of earthquakes that had
occurred in the region since Koyna experienced the first
earthquake in 1967 five years after water was impounded in the
reservoir.
Reporting their findings in Current Science they say that
seismicity associated with Koyna reservoir is unique in the world
because it is one of the few sites where earthquakes of magnitude
greater than five continue to occur three decades after the
initial spurt of activity.
Reservoir induced earthquakes have occurred in other parts of the
world too, but seismicity in these regions had tapered off with
time, the scientists said.
Persistence of moderate seismicity at Koyna is enigmatic
considering also the fact that the Indian peninsular shield is
relatively stable region, they said.
Most earthquakes in the last three decades occurred in an area of
about 25 kilometre long and 10 kilometre wide extending south of
the Koyna reservoir.
According to the geologists, the ongoing seismicity at Koyna
suggests that the annual loading cycles in the reservoir, that
was impounded in 1962, continue to influence the overall
stability of the region.
Scientists said earthquakes in Koyna region have been occurring
with striking regularity two to three months after reservoir
filling. According to the scientists, the annual filling cycles
of the reservoir continue to weaken this fault.
``With the passage of time the fault zone will become further
unstable, progressively lowering the threshold changes required
to initiate a failure,'' they said.
- PTI
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