A British expedition to study Antarctica early next year hopes to find the remains of the Endurance, the ship at the heart of one of history’s great survival epics.
The Endurance was carrying Antarctic explorer Ernest Shackleton when it was stranded in the ice of the Weddell Sea in February 1915. It drifted in the icepack for months before the floes ruptured the hull, leaving Shackleton and his party stranded.
Julian Dowdeswell, director of the Scott Polar Research Institute at the University of Cambridge, told Seeker that finding the Endurance is a secondary goal of the January 2019 expedition. The main purpose is to study the Antarctic Peninsula’s Larsen C ice shelf, which shed a roughly Delaware-sized chunk of ice in 2017.
But Dowdeswell said the Endurance may be “relatively intact” on the floor of the neighboring Weddell Sea, about 3,200 meters (10,000 feet) down.
“The timbers were sprung, which is why the ship sank in the end,” Dowdeswell said. “But the ship wasn’t crushed into little pieces, and the hull, for the most part, we think is still integral.”
Since there’s no natural wood in the Antarctic, there are no organisms known to feed on it, Dowdeswell said. Previous experiments have left pieces of wood and whale bone on the sea floor to find the wood largely intact, “while the whale bones were largely gone.”
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Endurance’s captain, Frank Worsley, recorded the ship’s position before it sank as about 270 miles east of the peninsula. Worsley was a master navigator whose sextant work also guided Shackleton and a handful of his men across 800 miles of open ocean to the British territory of South Georgia Island. That sextant and Worsley’s handwritten records are in the institute’s archives, Dowdeswell said.
“We think the accuracy of that is probably better than about a kilometer, and maybe within half a kilometer,” he said.
But while finding the grave of the Endurance is of historical interest, the expedition’s primary goal is to help understand the future — what might happen to Antarctica’s ice shelves and ice sheets, which are up to three miles thick in some spots, in a warming climate.
The split in the Larsen C ice shelf in 2017 was the third major breakup in 22 years. In 1995, about 1,500 square kilometers (589 square miles) of the northern ice shelf collapsed, while the 3,200-square-km (1,250-square-mile) Larsen B ice shelf abruptly disintegrated in 2002.
The ice from those shelves didn’t add to sea-level rise, since the ice was already in the water. But they remove a barrier to the continent’s land-based glaciers, which sped up their flow toward the sea after the earlier breakups, according to NASA.
Dowdeswell, a glaciologist, and his team will map the contours of the Larsen C ice shelf from above and below, using unmanned submarines and drones. They’ll also take core samples and use radiocarbon dating in the hopes of learning how the shelf may have behaved in the 20,000 years since the last ice age was at its peak, he said.
“If they have broken up at other times over that period, then perhaps we can worry a little bit less, and one might regard that as a more natural long-term process,” he said. “Whereas if nothing has happened until recently over the whole of that time span, then that would imply the changing climate of the last few decades is impacting those areas quite strongly.”