The Wilkins Ice Shelf is a large ice formation located off the coast of Antarctica, specifically in the Amundsen Sea. It is part of the larger Antarctic ice system and plays a crucial role in stabilizing the glaciers that flow into the ocean. The ice shelf has been monitored for changes due to climate change, which has led to significant melting and structural weakening. In recent years, the Wilkins Ice Shelf has experienced notable calving events, where large chunks of ice break off and float away. These events are concerning as they contribute to rising sea levels and can impact global ocean currents. Scientists continue to study the ice shelf to understand its dynamics and the effects of warming temperatures on the Antarctic region.