Beardmore Glacier Gateway to the Polar Plateau

The Beardmore Glacier drops off the Transantarctic Mountains onto the Ross Ice Shelf in a violent cascade of crevasse fields and pressure ridges stretching roughly 125 miles long and 25 miles wide. Shackleton’s Nimrod expedition first ascended it in 1908; Scott’s doomed Terra Nova team followed in 1911. Standing at its base — if you’re one of the rare expedition members or scientists to get here — the scale is genuinely humbling. Blue ice, seracs, and the constant groan of a living glacier moving three feet a day.

Access is exclusively by ski-equipped aircraft from McMurdo Station. No ground vehicle has traversed this route in any practical expedition sense. Scientists study it for paleoclimate records buried in the ice. No infrastructure whatsoever. It exists here because overlanders need to know what the real interior of this continent looks and sounds like.

Shackleton's highway to the Pole.