A team of scientists from Lamont-Doherty Earth Observatory at Columbia University has discovered paleolake basin situated beneath the ice sheet in northwest Greenland; geomorphological analysis and hydrological modeling indicate that the basin once hosted a lake with a surface area of up to 7,100 km2 and a volume of up to 580 km3; it may be hundreds of thousands or millions of years old and contain unique fossil and chemical traces of past climates...
