Antarctic Glacier’s Breakup Is Controlled by Seafloor Topography – Scientific American
Credit: ALAMY.
Article Synopsis – Scientists have discovered that submerged rock ridges contribute to the break up of Antarctic glaciers by creating cracks that eventually lead to calving events. These ridges “can also help stabilize the glacier by grinding against its underside, buttressing it against flowing faster out to sea”. To read the actual article click here.