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Rio Tinto

Rio Tinto

Source: https://bit.ly/3hfnQ7Y Photographer: Jose A. CC License: https://bit.ly/2YefJzE

Rio Tinto
Source: https://bit.ly/3hfnQ7Y Photo: Jose A. CCL: https://bit.ly/2YefJzE

Rio Tinto Facts

Source: https://bit.ly/3cO7Ypa Photo: Gzzz CCL: https://bit.ly/2XKyT18

Rio Tinto Physical Description

The remarkable Rio Tinto immediately captivates all those fortunate enough to view its beauty. It also has a respectable length, measuring roughly 62 mi (100 km). Only part of the body of water, however, displays the unique appearance for which it’s now known.

This portion of the incredible creation of Nature extends for about 31 mi (50 km). Its greatest appeal comes in a subsection of the greater flow. Extending over a length equaling roughly half the total of the river, an incredible phenomenon exists.

That’s because it’s this portion of the natural marvel that manifests the incredible array of colors you see here. These include such hues as red, orange, and shades of brown, though the red predominates. These also tend to vary in concentration from day to day.

The water of this section of Rio Tinto itself has an extremely acidic nature. It’s also high in levels of certain metals, most specifically iron. Near the end of the multi-colored section, this aspect of the body of water also slowly begins to thin out, to eventually disappear.

Source: https://bit.ly/2XPDf7f Photo: Riotinto2006 Public Domain Image

Rio Tinto Location, Formation, and Ecology

The stunning wonder of Nature that man calls Rio Tinto further formed in a section of the world well known for its natural beauty. In point of fact, this geological gem formed in a small portion of the southwestern section of what’s now the continent of Europe.

More specifically, though, its precise region now constitutes the country of Spain. In this beautiful location, the waters of the river originate high in the Sierra Morena Mountains, in the Andalusia region. From there, though, the river flows primarily south-southwesterly.

At precisely what point in the past the river itself formed presently remains undetermined. The origin of the enormous deposits of the various ores in the region, however, has been uncovered. These deposited via hydrothermal activity between 300 – 350 million years ago.

Given the incredible extremes inherent to the nature of the water of Rio Tinto, one might not expect to find life within it. That would be an incorrect belief, though. Although life remains scant and quite unique within its waters, a small amount of its does appear.

This primarily consists of various types of microorganisms, largely consisting of different forms of algae. Relatively large quantities of anaerobic bacteria reside within the sediments it contains, possibly contributing to the condition of the waters.

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