Here is a look at the mountains of Antarctica if you removed all the ice.
Bedmap2 gives scientists a more detailed view of Antarctica’s landmass
Scientists at the British Antarctic Survey have been working with a host of international collaborators to present the most detailed map yet of Antarctica’s landmass. Bedmap2 reveals a landscape of mountain ranges and plains cut by gorges and valleys much deeper than previously seen.
In addition, the map allows scientists to analyse, in much greater detail, the bed below the Antarctic ice sheet.
Several features of the bed have been revealed for the first time including a new deepest point. The bed under the Byrd Glacier in Victoria Land is 2,870 metres below sea level making it the lowest point on any of the Earth’s continental plates.
The map was compiled using datasets collected from radio echo sounding measurements, seismic techniques, satellite readings and cartographic data.
A number of key statistics emerge;
- The volume of ice in Antarctica is 4.6% greater than previously thought
- The mean bed depth of Antarctica, at 95 metres, is 60 m lower than estimated
- The volume of ice that is grounded with a bed below sea level is 23% greater than originally thought meaning there is a larger volume of ice that is susceptible to rapid melting. The ice that rests just below sea level is vulnerable to warming from ocean currents
- The total potential contribution to global sea level rise from Antarctica is 58 metres, similar to previous estimates but a much more accurate measurement
- The new deepest point, under Byrd Glacier, is around 400 metres deeper than the previously identified deepest point
