Pine Island Glacier is one of the main outlets for ice from the interior of the West Antarctic Ice Sheet to flow into the ocean.
The image above was taken on September 21, 2017 by the Landsat 8 satellite. It shows a clear rift visible across the centre of the glacier’s floating ice shelf.
Not long afterward, the rift resulted in the calving of a large iceberg, with an area of about 185 square kilometres, now floating in the Amundsen Sea.
Originally published by Cosmos as Glacial rift
Cosmos
Curated content from the editorial staff at Cosmos Magazine.
Read science facts, not fiction...
There’s never been a more important time to explain the facts, cherish evidence-based knowledge and to showcase the latest scientific, technological and engineering breakthroughs. Cosmos is published by The Royal Institution of Australia, a charity dedicated to connecting people with the world of science. Financial contributions, however big or small, help us provide access to trusted science information at a time when the world needs it most. Please support us by making a donation or purchasing a subscription today.