Megaquakes
caused volcanoes to sink: Research
PARIS:
Massive earthquakes can cause distant volcanoes to sink, according to
research in Japan and Chile published on Sunday.
30
June, 2013
The
magnitude 9.0 tsunami-generating quake that occurred off northeastern
Japan in 2011 caused subsidence of up to 15 centimetres (9.3 inches)
in a string of volcanoes on the island of Honshu as much as 200
kilometres (120 miles) from the epicentre, a Japanese study said.
And
the 8.8 magnitude Maule quake in Chile in 2010 caused a similar
degree of sinking in five volcanic regions located up to 220km (130
miles) away, according to a US-led paper.
It
was not clear whether the phenomenon boosted eruption risk, the
authors wrote.
Both
the Japan and Chile quakes were of the subduction type, caused when
one part of Earth's crust slides beneath another.
If
the movement is not smooth, tension can build up over decades or
centuries before it is suddenly released, sometimes with catastrophic
effect.
In
both cases, the sinking occurred in mountain ranges running
horizontally to the quake.
The
2011 quake "caused east-west tension in eastern Japan,"
Youichiro Takada of the Disaster Prevention Research Institute at
Kyoto University told AFP in an email.
"Hot
and soft rocks beneath the volcanoes, with magma at the centre, were
horizontally stretched and vertically flattened. This deformation
caused the volcanoes to subside."
The
researchers for the Chilean volcanoes said subsidence occurred along
a stretch spanning 400km (250 miles).
As
in Japan, the ground deformation in Chile occurred in huge
ellipse-shaped divots up to 15km by 30km (nine miles by 18 miles) in
size, although the cause appears to be different.
Pockets
of hot hydrothermal fluids that underpinned the volcanic areas may
have escaped through rock that had been stretched and made permeable
by the quake.
Two
earthquakes in the Chilean subduction zone in 1906 and 1960 were
followed by eruptions in the Andean southern volcanic zone within a
year of their occurrence.
However,
no big eruptions in this volcanic hotspot can be associated with the
2010 temblor, says the study led by Matthew Pritchard of Cornell
University in New York.
Takada
said the impact of the 2011 quake on volcano risk on Honshu was
unclear.
"At
this stage we do not know the relation between volcanic eruption and
the subsidence we found. Further understanding of the magmatic
movement would be necessary," he said
The
subsidence in Japan was spotted at the volcanoes Akitakoma, which
last erupted in 1971; Kurikoma (1950); Zao (1940); Azuma (1977); and
Nasu (1963).
The
studies, published in the journal Nature Geoscience, used data from
satellite radar which mapped terrain before and after the quakes.
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