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" ... If you want to understand the lives of our planet's vanishing glaciers, Thwaites is one of the most important glaciers to get to know. Thwaites Glacier is a broad slab of ice flowing downhill and into west Antarctica's Pine Island Bay at a speed of about 2km (1.25 miles) per year. It's one of the fastest-moving — and most unstable — glaciers in Antarctica, and it flows alongside another large, rapidly changing (read: unstable and disappearing) glacier called Pine Island, on a stretch of coastline, the Walgreen Coast, which has become known as the "weak underbelly" of the West Antarctic Ice Sheet. Thwaites flows offshore in a tongue of floating ice, which regrounds itself on a ridge of land offshore. The part of the glacier that's grounded on the offshore ridge seems fairly stable, but the part that's floating between the ridge and the coast is exposed to ocean water — which was warmer than the ice even back when sea temperatures were cooler — and melting from the bottom. ... "