The Secret of Blood Falls of Antarctica
“The Secret of Blood Falls of Antarctica” seems quite interesting, isn’t it?Read all about it here and fulfill your interest.
So many people enjoy the water falling from the height or formed when a river or stream flows over a precipice or steep incline, which is known as waterfalls.
people mostly visit waterfalls in summer & enjoy with their loved ones. enjoying waterfalls make you feel the love with nature these waterfalls show how beautiful our mother nature.
Jog Falls, Shimoga, (Karnataka)
Dudhsagar Falls, (Goa)
Nigara falls. [Ontario, Canada / New York, USA]
yosemite falls. [Yosemite National Park (California), USA]
people visit waterfalls & enjoy with their friends, family, love…
But how’ll you react when someone says there is a BLOOD FALLS ?
yes, you read the right word…its blood falls
let’s talk about here & know more about blood falls
This blood falls is found 1911 by the Australian geologist Griffith Taylor who first explored the valley that bears his name.
There are so many theory on this Blood Falls of Antarctica which shows the reason for this red water
when we talk about mysterious things we’ll predict so many theory in our mind…
But the The Secret of Blood Falls of Antarctica is revealed now, the scientific method reason behind blood falls is…
Sparingly soluble hydrous iron oxides are deposited on the ice surface after the iron ions present in the unfrozen salt water are oxidized in contact with atmospheric oxygen. The more soluble iron ions are initially dissolved in old seawater trapped in an ancient pocket left over from the Antarctic Ocean when a fjord was isolated by the glacier in its course during the Miocene about 5 million years ago, when the sea level was higher than today. ..
Unlike most glaciers in the Antarctic, the Taylor Glacier is not frozen to the rocks, probably because of the presence of salts concentrated by the crystallization of the ancient seawater trapped beneath it. Salt cryopreservation occurred in the deep relic of seawater when pure ice crystallized and released its dissolved salts when it cooled due to the heat exchange of trapped liquid seawater with the glacier’s massive ice mass. As a result, the trapped seawater was concentrated in brine, the salinity of which was two to three times that of the middle seawater. A second mechanism, which sometimes explains the formation of hypersaline saline solutions, is the evaporation of water from surface lakes directly exposed to the very dry polar atmosphere in the McMurdo dry valleys. The analysis of stable isotopes of water makes it possible in principle to distinguish between the two processes, as long as there is no mixture between differently formed sols.
Hypersaline fluid, accidentally taken through a crack in the ice, was oxygen-free and rich in sulfate and iron ions. Sulphate is a remanent geochemical signature of marine conditions, while soluble divalent iron is likely released under reducing conditions from subglacial rock minerals weathered by microbial activity
In December 2014, scientists and engineers led by Mikucki returned to Taylor Glacier and used a probe called IceMole, designed by a German collaboration, to melt into the glacier and directly sample the brine that feeds Blood Falls.