Pakistan quake island unlikely to last, say experts
26 September, 2013
GWADAR: A small island of mud and rock created by the huge earthquake that hit Balochistan 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 Balochistan'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 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 a private television news.
The island is about 60 to 70 feet 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. A similar event happened in the same area in 1945 when an 8.1-magnitude earthquake at Makran triggered the formation of mud volcanoes off Gwadar. Professor Shamim Ahmed Shaikh, chairman of the department of geology at Karachi University, said the island, which has not been officially named, would disperse within a couple of months.
He said it happens along the Makran coast because of the complex relationship between tectonic plates in the area. Pakistan sits close to the junction of three plates – the Indian, Arabian and Eurasian. "About a year back an island of almost similar size had surfaced at a similar distance from the coast in the Makran region. This would disperse in a week to a couple of months," Shaikh told AFP.
Gibson said the temporary island was very different from the permanent uplift seen during major "subduction zone" earthquakes, where plate collisions force the Earth's crust suddenly and sometimes dramatically upwards. For example, in the massive 9.5-magnitude earthquake in Chile in 1960 – known as the world's largest ever – whole fishing villages were thrust "several metres" upwards and wharves suddenly located hundreds of metres inland, Gibson said.
Such uplift events are relatively common in the Pacific's so-called "Ring of Fire", a hotbed of seismic and volcanic activity at the junction of several tectonic plates. A thundering 8.0-magnitude quake in the Solomon Islands in 2007 thrust Ranogga Island upwards by three metres, exposing submerged reefs once popular with divers and killing the vibrant corals, while expanding the shoreline outwards by several metres in the process.
During the massive 9.2-magnitude earthquake off Sumatra which triggered a devastating tsunami across the Indian Ocean in 2004, several islands were pushed upwards while others subsided into the ocean. The Aceh coast dropped permanently by one metre while Simeulue Island was lifted by as much as 1.5 metres, exposing the surrounding reef, which became the island's new fringe.