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Geological Diversity
Serra Geral Orogen

Serra Geral   Serra Geral   Serra Geral 
The Serra Geral Formation is one of the formations of the Paraná Basin. It is the result of the largest continental volcanic magmatism known on Earth which ocurred during the Upper Cretaceous (145 - 100 Ma). At that time, the prototypes of today´s continents South America (the South American Platform) and Africa were still united as part of the supercontinent Pangea (see geology).

The separation of South America and Africa (which led to the opening of the South Atlantic) was preceded by a voluminous tholeitic magmatism whose basaltic lava flooded the basins in the south of the two continents (Paraná, Etendeka, Angola), giving rise to the Paraná - Etendeka Magmatic Province. The heat source which caused this magmatism, was probably generated by a large mantle plume situated below the Earth´s crust.
Paraná - Etendeka Magmatic Province

The volcanic rocks of the lava sequences which reach thicknesses of up to 1.700 m and the canyons originated by tectonic movements and by the erosion of wind and water, are the main ecotouristic attraction of many national parks in southern Brazil (e.g. São Joaquim, Serra Geral, Aparados da Serra and Iguaçu).
 

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