- Blood Falls, Antarctica
In Antarctica's Taylor Glacier, there is a place in the frozen ice from which the red color flows. Seeing this, it seems that this spring is bleeding. However, scientists did much research on this but did not get any definite results. One of their estimates is that in this place under the ice there is probably a lot of iron element which gives the water red color. Although this Lala Fall is still a mystery.
After exposure to the atmospheric oxidative oxygen in the inorganic solids, the frequent oxidative humid ferries oxide deposited is reduced. During the summer, when the separation of a diode in the Miocene period, about 5 million years ago, when the sea level was higher than today, these more soluble iron ions initially stuck in the ancient climate, which is stuck in an ancient pocket.
Like most Antarctic glaciers, the Telar glacier is not empty, probably under the presence of salts stored by the ancient sea crystallization. The saline particle-density occurs deeply on the seafront when pure ice swells and carries its dissolved salt because it is cooled due to the heat transfer of the fluid by the huge ice mass of the ocean. As a result, salinity is two to three times rich in sea level water from the sea level. A second process is to explain the formation of hypersaline brines that evaporate directly below the surface of the dry pole atmosphere in the McMurdo Drill
Valleys. The analysis of the water stable isotopes are allowed in the policies, in the absence of differences between the processes of both the compounds are mixed separately.
Hyperalin liquid was strongly tested by a fracture of ice, rich in oxygen-free and sulfate and iron ions. Sulphate is a residual geochemical sign of marine status when the soluble bilingual iron was probably released by microbial activity by reducing the condition from subglacial bedroom minerals to seeds.