Brazilian relief

Brazilian relief

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The relief of Brazil has old formation and currently there are several classifications for it. These include the following teachers:

  • Aroldo de Azevedo - This classification dates from 1940, being the most traditional. It mainly considers the altimeter level to determine what a plateau or a plain is.
  • Aziz Nacib Ab'Saber - Created in 1958, this classification despises the altimetric level, prioritizing the geomorphological processes, that is, erosion and sedimentation. Thus, the professor considers plateau as a surface on which the process of wear predominates, while plain is considered a sedimentation area.
  • Jurandyr Ross - is the most recent classification, created in 1995. It is based on the Radambrasil project, a survey made between 1970 and 1985, where aerial photos were taken of the surface of the Brazilian territory, using a sophisticated radar. Jurandyr also uses geomorphological processes to elaborate his classification, highlighting three main forms of relief:
    1) Plateaus
    2) Plains
    3) Depressions

According to this classification, Highland It is an irregular surface, with altitude above 300 meters and erosion product. Flat land It is a flat area formed by the recent accumulation of sediment.

Lastly, depression It is a surface between 100 and 500 meters in altitude, with gentle slope, flatter than the plateau and formed by erosion process. The following figure shows this representation of the Brazilian relief.

Below is another map that represents the Brazilian relief, showing some of the best known regions of the same.