Antarctica’s “Blood Falls,” a rust-red cascade emerging at the terminus of the Taylor Glacier, has puzzled scientists for more than a century because of its bloodlike appearance. Reports describe the phenomenon as not involving blood or contamination. Instead, the red color comes from iron-rich, salty water that flows upward through cracks from a reservoir trapped beneath the glacier for an estimated 1.5 million years. Once the water reaches the surface, it mixes with oxygen in the air. The iron then oxidizes, producing iron oxides that create a reddish-brown hue resembling flowing blood against the ice. The event is studied to improve understanding of glacial and subglacial history, and some research also uses it to explore how life could persist in extreme, low-energy environments, including environments similar to those on icy moons. Overall, sources converge on the same scientific explanation: ancient briny meltwater, driven through the ice and altered by oxidation at the surface, produces the waterfall’s distinctive color.