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Encyclopedia > Gruta Rei do Mato

Gruta Rei do Mato means "Cave of the Forest King" in Portuguese. It is named after a fugitive who lived in it.


Gruta Rei do Mato is located near Sete Lagoas in Minas Gerais, Brazil at the border of BR 040 highway, close to the access clover to the city. From Sete Lagoas, the cave can easily be reached by bus, taxi or car. Sete Lagoas is 70 kilometres away from Belo Horizonte.


The limestone area north of Belo Horizonte is called the Sete Lagoas Formation. It is in this limestone that the Lagoa Santa Karst was developed. The area around Sete Lagoas has many caves, of which the Gruta Rei do Mato is the most famous one.


The Gruta Rei do Mato has three large chambers with numerous stalactites, stalagmites and rimstone dams. In the Room of the Rarities has are identical columns, parallel, formed by the crystals of Calcita. These columns are more than 20 meters of height with only 30 centimetres of diameter.


The Rei do Mato (the fugitive called "the Forest King") actually lived in a small cave next to the Gruta Rei do Mato. It is in this cave that 4,000 to 6,000 years old cave paintings were discovered. Also, the skelleton of Xenorrinoterium bahiense, an extinct animal, was discovered here. At nowedays, there is a replica of this animal in the cave.


See also

External links

  • Showcaves.com on Gruta Rei do Mato (http://www.showcaves.com/english/br/showcaves/ReiDoMate.html)
  • Pictures of Gruta Rei do Mato (http://www.viagensmaneiras.com/viagens/grutareidomatoING.htm)

  Results from FactBites:
 
Cola da Web [ www.coladaweb.com ] (358 words)
Gruta da Lapinha - A gruta da Lapinha fica na cidade de Lagoa Santa e supõe-se que tenha sido formada há cerca de 900 milhões de anos.
Gruta Rei do Mato - A Gruta Rei do Mato fica na cidade de Sete Lagoas, a 62 quilômetros de Belo Horizonte.
A Rei do Mato ainda é uma gruta considerada "viva" pelos cientistas, porque continua se formando pela ação da água.
ambientebrasil - ambiente natural (Cavernas no Brasil) (4080 words)
E a estalagmite "cresce" do piso da caverna para cima, bem embaixo da estalactite, a partir do gotejamento de água saturada em calcita que se precipita da estalactite.
Cascatas - a água ao escorrer pela parede rochosa da gruta, vai depositando calcita durante seu percurso descendente.
As cavernas têm ambientes muito diferenciados dos do meio externo, caracterizados pela ausência de luz e de vegetação superior, pela pequena variação de umidade e temperatura e pela composição química do ar e da água.
  More results at FactBites »


 
 

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