![]() |
| A side view of the Ross Ice Shelf, the largest ice shelf in Antarctica. Washington University in St. Louis seismologist Doug Wiens discovered that unexpected movements of the Ross Ice Shelf are triggered by the sudden slipping of parts of the Willans Ice Stream. Photo Credit: Lin Padgham (CC BY 2.0.) |
In Antarctica, heavy glaciers are always on the move. Conveyor belts of ice known as ice streams are the corridors of faster flow that carry most of the vast glaciers’ ice and sediment debris out toward the ocean.
One such ice stream jostles the entire Ross Ice Shelf out of place at least once daily, according to new research from Washington University in St. Louis.
This finding is significant because of the scale of the Ross Ice Shelf: It is the largest ice shelf in Antarctica, about the same size as the country of France.
“We found that the whole shelf suddenly moves about 6 to 8 centimeters (or 3 inches) once or twice a day, triggered by a slip on an ice stream that flows into the ice shelf,” said Doug Wiens, the Robert S. Brookings Distinguished Professor of earth, environmental and planetary sciences in Arts & Sciences. “These sudden movements could potentially play a role in triggering icequakes and fractures in the ice shelf.”
The Ross Ice Shelf is a floating lip of ice that extends out over the ocean from inland glaciers.
.jpg)









.jpg)

.jpg)

