词条 | Caverna Aroe Jari |
释义 |
GeologyIt occurs in the formations of Alto Garças e Vila Maria (Grupo Rio Ivaí of caves) and is formed in siliclastic sedimentary rock of ordovício-silurian age, in the Paraná Basin. The first scientific reports may be attributed to Ramis Bucair spelunker who have visited the cave in the early 1970s.[2] In 1989 the cave was included as part of the "Plano de Reordenamento da Ocupacao da Chapada" created by FEMA - Fundacao Estadual do Meio Ambiente. The region was considered an environmental preservation area by decree nr. 99556/90. Other caves in the area are Caverna do Lago Azul, Caverna Kiogo Brado.[2] See also
References1. ^{{cite web|last=Chapada dos Guimaraes|title=CAVERNA AROE JARI E LAGOA AZUL|url=http://www.chapadadosguimaraes.com.br/cav.htm|publisher=Eco Turismo Cultural|accessdate=1 January 2012}} 2. ^1 {{cite book|last=Marcio Ivan Carvalho Moreira|first=Leonardo Borghi|title=Caverna Aroe Jari, Chapada dos Guimaraes, MT|publisher=Sigep|pages=482–488|url=http://vsites.unb.br/ig/sigep/sitio030/sitio030.pdf}} External links
4 : Caves of Mato Grosso|Protected areas of Mato Grosso|Wild caves|Landforms of Mato Grosso |
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