Antarctica’s Blood Falls Finally Explained: Pressure-Driven Brine and Iron From Ancient Microbes
New research published in Antarctic Science explains Blood Falls: the red water is iron oxide formed by ancient subterranean bacteria, while the liquid is a hypersaline brine kept unfrozen at -20°C; eruptions occur when pressure builds in subglacial channels beneath Taylor Glacier, forcing brine out in bursts and briefly slowing the glacier, with warming's future effects still unknown.