At that time, the fissure spanned about 15 miles (24 km) in length and 164 feet (50 meters) in width, according to researchers at the Alfred Wegener Institute for Polar and Marine Research in Bremerhaven, Germany. In May 2012, satellite images revealed a second rift had formed near the northern side of the first crack. "As a result of these cracks, one giant iceberg broke away from the glacier tongue," Angelika Humbert, a glaciologist at the Alfred Wegener Institute, said in a statement. [Photo Gallery: Antarctica’s Pine Island Glacier Cracks]
An aerial shot of Antarctica's Pine Island Glacier. On July 8, 2013, a huge piece of the glacier's ice shelf (the portion that floats on the water) broke off to form a new iceberg. Humbert and her colleagues studied high resolution radar images taken by the TerraSAR-X satellite to track the changes in the two cracks, and to observe the processes behind glacier movements.
"Using the images we have been able to follow how the larger crack on the Pine Island Glacier extended initially to a length of 28 kilometers [17 miles]," Nina Wilkens, one of the team researchers from the Alfred Wegener Institute, said in a statement. "Shortly before the 'birth' of the iceberg, the gap then widened bit by bit so that it measured around 540 meters [1,770 feet] at its widest point."
As the Pine Island Glacier retreats and flows out to sea, it develops and drops icebergs as part of a natural and cyclical process, Humbert said. But, the way the ice breaks, or "calves," is still somewhat mysterious. "Glaciers are constantly in motion," she said. "They have their very own flow dynamics. Their ice is exposed to permanent tensions and the calving of icebergs is still largely unresearched."
The Pine Island Glacier ice shelf, the part of the glacier that extends out into the water, last produced large icebergs in 2001 and 2007.