On September 24 a major earthquake rocked western Pakistan killing at least 515 people and leaving more than 100,000 homeless. While the death and devastation caused by the 7.7 magnitude temblor makes the mind and heart reel, amid the chaos a new island was born. Its muddy top surfaced offshore in West Bay near Gwadar, Pakistan some 230 miles (370 km) from the epicenter.
Great little video of local people exploring the newly-birthed island
Two days later on Sept. 26, the advanced Land Imager (ALI) on NASA’s Earth Observing-1 (EO-1) satellite took the picture above of the newly exposed sea bottom located 0.6 miles (1 km) from shore.
“The island is really just a big pile of mud from the seafloor that got pushed up,” said Bill Barnhart, a geologist at the U.S. Geological Survey who studies earthquakes in Pakistan and Iran.
The island, seen closeup in the aerial view, extends 250 to 300 feet (75-90 meters) across and stands 60 to 70 feet (15-20 meters) above the water line. The surface is a mixture of mud, fine sand, and solid rock. In the video, you’ll see people already treading on what a day before had been the bottom of the sea.
Small, short-lived islands are fairly common in this part of the world. As the Arabian continental plate dives beneath the Eurasian crustal plate, accumulated mud (sediments) are scraped off and deposited as temporary islands. Earthquakes can create new islands, too. When a shallow pockets of gas like methane or carbon dioxide get trapped under pressure by layers of muddy sediments, powerful seismic waves can trigger their sudden release.
“When that layer becomes disturbed by seismic waves (like an earthquake), the gases and fluids become buoyant and rush to the surface, bringing the rock and mud with them,” said Barnhart.
Watch out! Highly-flammable methane still vents from the brand new island. When I saw someone setting it afire in the video, it made me wonder how we’ve managed survived so long on this planet without blowing ourselves up.
Like the fate of many islands before it, this one will likely disappear. Underground gas will cool and compress or simply escape, allowing the raised crust to sink back down into the sea bottom. Waves and weather will nibble the island to pieces, returning it back to the sea in a matter of months.