Despite this stability of some parts of Antarctica's ice sheets, scientists worry that rising temperatures can affect the ice along with the coastline leading to rise in the sea level.
Central parts of Antarctica's ice sheet have been stable for millions of years, even when conditions were considerably warmer than present, new research suggests.
The study of mountains in West Antarctica may help scientists improve their predictions of how the region might respond to continuing climate change.
The findings could also show how ice loss might contribute to sea level rise.
Although the discovery demonstrates the long-term stability of some parts of Antarctica's ice sheet, scientists remain concerned that ice at its coastline is vulnerable to rising temperatures.
Researchers from the Universities of Edinburgh and Northumbria in the UK studied rocks on slopes of the Ellsworth Mountains, whose peaks protrude through the ice sheet.
By mapping and analysing surface rocks - including measuring their exposure to cosmic rays - researchers calculated that the mountains have been shaped by an ice sheet over a million-year period, beginning in a climate some 20 degrees Celsius warmer than at present.
The last time such climates existed in the mountains of Antarctica was 14 million years ago when vegetation grew in the mountains and beetles thrived.
Antarctica's climate at the time would be similar to that of modern day Patagonia or Greenland. This time marked the start of a period of cooling and the growth of a large ice sheet that extended offshore around the Antarctic continent.
Glaciers have subsequently cut deep into the landscape, leaving a high-tide mark - known as a trimline - in the exposed peaks of the Ellsworth range.
The extended ice sheet cooled the oceans and atmosphere, helping form the world of today, researchers said. The study is among the first to find evidence for this period in West Antarctica.
"These findings help us understand how the Antarctic Ice Sheet has evolved, and to fine-tune our models and predict its future," said David Sugden, of the University of Edinburgh.
"The preservation of old rock surfaces is testimony to the stability of at least the central parts of the Antarctic Ice Sheet - but we are still very concerned over other parts of Antarctica amid climate change," Sugden said.
The research was published in Earth and Planetary Science Letters.
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 "Antarctica, ice sheet, Climate Change, University of Edinburg, University of Northumbria, Ellsworth")
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