
Red Outflow Unmasks Ancient Subglacial Brine on Taylor Glacier
Researchers document a red, iron‑oxidizing brine outflow from Taylor Glacier in Antarctica, captured across three instruments during Sep–Oct 2018; the event briefly slowed ice flow and cooled near-base lake water, with the red color arising after exposure to air. The observation supports a model of pressurized brine injection through basal crevasses but leaves the trigger mechanism unsettled, and scientists call for expanded, high-frequency monitoring to determine how often such discharges occur.




