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The Incredible True Story of Minas Gerais: The Brazilian State That Once Had a Beach and a Red Sea That Turned Into Hills and Iron Ore

Written by Flavia Marinho
Published on 05/12/2025 at 13:37
FERRO - MINAS - MINÉRIO - PRAIA - MINAS GERAIS - MAR VERMELHO - CAVERNA - MONTANHA
Minas Gerais fica longe da praia, mas um dia foi fundo de mar e ricos em ferro que chegaram a ficar avermelhados. As rochas e fósseis do estado brasileiro contam essa virada gigante na história da Terra.
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Minas Gerais Is Far From the Beach, But One Day It Was Underwater and Rich in Iron That Turned Red. The Rocks and Fossils of This Brazilian State Tell the Giant Turn in the History of the Earth.

Have you ever looked at a map of Brazil and thought, “Poor Minas, not even a little beach to call its own?” Well, hold on to this: the Brazilian state of Minas used to have beaches, and not just once. In different chapters of geological time, areas that are now mountains, caves, and mines were once shallow seas.

And, in an even older past, these seas carried so much iron dissolved that the water could take on a red sea hue. It sounds like a movie script, but it’s written in stone. Literally.

Minas Was Once a Sea, and That’s No Exaggeration!

Let’s break it down. Long before Brazil existed, and even before the Atlantic Ocean opened up the way we know it today, much of what would become Minas was connected to ancient continents and supercontinents like Gondwana.

During phases of the Neoproterozoic/Ediacaran, around 600 to 540 million years ago, the northern and central parts of the state were submerged under shallow seas, like warm and shallow platforms.

This sea left a clear record in the Bambuí Group, especially in the Sete Lagoas Formation, full of carbonates and typical structures of shallow marine environments after a major transgression.

The “Last Coastal Area of Minas” Is in Januária

The most popular (and easiest to imagine) evidence of this sea comes from Januária, in northern Minas. There, researchers found fossils of Cloudina and Corumbella, marine creatures from the end of the Ediacaran period. In other words: that stone wall in the interior used to be the seafloor.

The very FAPESP Research describes this scenario as the “last coastal area of Minas,” because these marine fossils mark a shallow sea that covered the area about 550 million years ago.

And there’s a great quote to humanize this: geologist Lucas Warren (Unesp) explained that these little creatures “only lived in shallow seas” and appear in various parts of the world always in marine rocks.

But What About the “Red Sea”? That’s Much Older

Now comes the part that sounds like science fiction.

Billions of years ago, the Earth’s oceans were practically devoid of free oxygen and full of dissolved iron. The water was a chemical “brew.” But photosynthesizing microorganisms (like cyanobacteria) began to produce oxygen. This O₂ reacted with the iron in the water, forming oxides like hematic and magnetite, which precipitated to the ocean floor.

What was the result?

  • the iron left the water and ended up on the ocean floor;
  • the water turned reddish in many places due to excess minerals;
  • and gradually, oxygen stopped being “used up” by iron and began to accumulate in the atmosphere.

This is a central piece of the Great Oxygenation Event, around 2.4 billion years ago, a watershed moment for life to move beyond microscopic and gain complexity.

Quadrilátero Ferrífero: The Ancient Sea Turned Mountain… and Ore

So where does Minas fit into this global “red sea”? In the rocks.

The Quadrilátero Ferrífero holds some of the most important banded iron formations (BIFs) on the planet.

These are the alternating layers of iron oxides and silica that settled on the floors of primitive seas.

In Minas, after metamorphism, they appear as itabirites, the basis of the state’s major iron deposits.

A study from UFMG emphasizes the nature of these rocks and shows how the itabirite of the Quadrilátero is highly oxidized, dominated by hematite.

How the Sea Disappeared and the “Mine Beach” Became a Mountain

After these sediments accumulated on the ocean floor, the Earth’s game board changed again. Tectonic plates shifted, continents collided, and what was ocean bed was folded, lifted, and exposed. With millions of years of erosion, it turned into the mountainous terrain we know today.

This uplift had a gigantic side effect: it brought iron to the surface. And this is where the modern economic relevance of Minas comes in: these ancient marine layers now support one of the world’s largest mining hubs.

If this time travel surprised you, comment below: And if you know someone who swears that Minas “never had a sea,” send this text to that person.

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Flavia Marinho

Flavia Marinho é Engenheira pós-graduada, com vasta experiência na indústria de construção naval onshore e offshore. Nos últimos anos, tem se dedicado a escrever artigos para sites de notícias nas áreas militar, segurança, indústria, petróleo e gás, energia, construção naval, geopolítica, empregos e cursos. Entre em contato com flaviacamil@gmail.com ou WhatsApp +55 21 973996379 para correções, sugestão de pauta, divulgação de vagas de emprego ou proposta de publicidade em nosso portal.

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