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by Staff Writers Gwadar, Pakistan (AFP) Sept 25, 2013
A
small island of mud and rock created by the huge earthquake that hit
southwest Pakistan has fascinated locals but experts -- who found
methane gas rising from it -- say it is unlikely to last long.
The
7.7-magnitude quake struck on Tuesday in Baluchistan's remote Awaran
district, killing at least 271 people and affecting hundreds of
thousands.
Off the coastline near the port of Gwadar, some 400
kilometres (250 miles) from the epicentre, locals were astonished to see
the dark grey mass of rock and mud that had emerged from the waves in
the Arabian Sea.
"It is not a small thing, but a huge thing which has emerged from under the water," Gwadar resident Muhammad Rustam told AFP.
"It looked very, very strange to me and also a bit scary because suddenly a huge thing has emerged from the water."
Enterprising
boat owners were doing a brisk trade ferrying curious sightseers to the
island -- dubbed "Earthquake Mountain" by locals.
Mohammad
Danish, a marine biologist from Pakistan's National Institute of
Oceanography, said a team of experts had visited the island and found
methane gas rising.
"Our team found bubbles rising from the
surface of the island which caught fire when a match was lit and we
forbade our team to start any flame. It is methane gas," Danish said on
GEO television news.
The island is about 60 to 70 feet (18 to 21
metres) high, up to 300 feet wide and up to 120 feet long, he said. It
sits about 650 feet from the coast.
The surface was a solid but
muddy mix of stones, sand and water with visible cracks, said an AFP
cameraman who visited the island. Dead fish and sea plants lay on the
surface.
Gary Gibson, a seismologist with Australia's University
of Melbourne, said the new island was likely to be a "mud volcano",
created by methane gas forcing material upwards during the violent
shaking of the earthquake.
"It's happened before in that area but
it's certainly an unusual event, very rare," Gibson told AFP, adding
that it was "very curious" to see such activity some 400 kilometres from
the quake's epicentre.
The so-called island is not a fixed
structure but a body of mud that will be broken down by wave activity
and dispersed over time, the scientist said.
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