Once again, the demise of floating ice removed the backstop that
stabilized glaciers behind it.
The shelves slow and
stabilize the glaciers behind them, but they are succumbing to a hidden force: Deep, warming ocean currents are melting the ice from beneath.
Not exact matches
At the grounding line, the ice detaches from the bedrock and juts out into the water as a kind of floating ledge, or ice shelf, which helps to
stabilize the
glacier and hold back the flow of ice
behind it.
These ice shelves are responsible for
stabilizing the
glacier and hold back the flood of ice
behind them.
At the grounding line, the ice detaches from the bedrock and juts out into the water as a kind of floating ledge, or ice shelf, which helps to
stabilize the
glacier and hold back the flow of ice
behind it.