Pluto's heart shows a young, churned nitrogen glacier erasing its history

Sputnik Planitia, the bright nitrogen-ice plain at Pluto's heart, has no confirmed impact craters, implying a convecting, glacier-like surface that renews itself on timescales of about 500,000 years; while older, cratered terrain exists elsewhere on Pluto, this region's surface is continually renewed, making parts of it effectively younger than humans, though crater counts alone don’t give a precise age.