Blood Falls of Antarctica

There are thousands of stunning waterfalls worldwide. However, none are as unique as Antarctica’s Blood Falls. The aptly-named waterfall, which flows from the tip of Taylor Glacier, spruts out bright red water, we can think of it as a pressure releasing valve. The existence of the five story tall waterfall has been known for over a century. But the reason behind its crimson waters has remained a mystery.

A bright red waterfall isn’t something you’d expect to see on the icy landscape of Antarctica, but that’s exactly what’s pouring out from the foot of Taylor Glacier. A team of scientists now claims to have solved the long-standing mystery behind the crimson waters of Antarctica’s Blood Falls.

The bizarre and apparently grisly sight was first discovered in 1911 by geologist Thomas Griffith Taylor, who attributed it to red algae. It was only half a century later that the crimson color was identified as being caused by iron salts. Most intriguingly, the water starts off clear but turns red soon after it emerges from the ice, as the iron oxidizes on exposure to the air for the first time in millennia.

The blood falls were discovered in 1962 by Robert Black and Thomas Berg, geologists from the University of Wisconsin. Black and Berg were exploring the Taylor Valley when they noticed a “striking reddish-yellow” ice cone at the glacier’s terminus. Lacking access to sophisticated remote sensing technology, the two scientists tried to trace the source the only way possible, by following the colorful flow back to its source.

Expecting to find ice-melt or a river, they were shocked to discover that the falls had no source. The red water simply emerged from beneath the ice. They were further shocked when water samples revealed that the discharge was composed of hypersaline brine.

Expecting to find ice-melt or a river, they were shocked to discover that the falls had no source. The red water simply emerged from beneath the ice. They were further shocked when water samples revealed that the discharge was composed of hypersaline brine.

But where did it come from? The explorers compared it to sea water and determined that the brine discharge could not be ocean spray carried by the wind. They immediately recognized the significance of their discovery: a large salt source was present underneath an Antarctic Glacier with no apparent cause. The flow might even have begun shortly before their visit, according to observations from Navy pilots, so that brine might have been completely sealed under the Taylor glacier for millennia until merely a couple of months before Berg and Black showed up — a truly amazing coincidence.

The riddle of the brine was not solved until 2005, when an expedition drilled a core under the thick ice at nearby Lake Vida. The glacial cores, when retrieved, were coated in brine at the bottom. Further analysis revealed that the brine contained a thriving microbial community, in anoxic (low or no oxygen) conditions at -13°C.

The bacteria engages in an oxidation reaction with the rock, resulting in the color of the blood falls where the brine is exposed to atmosphere. The entire process takes place in complete darkness, so these bacteria grow and thrive on geochemical processes since photosynthesis is out of the question. These processes, as well as some non-biological reactions, are responsible for much of the salt and mineral content of the brine.

It took 43 years, but a chance discovery in 1962 led to the discovery of one of the most extreme and bizarre ecosystems on Earth, not to mention the striking appearance of the area. Life can thrive anywhere, it seems, given a chance.