{"id":28787,"date":"2025-08-29T13:35:51","date_gmt":"2025-08-29T16:35:51","guid":{"rendered":"https:\/\/www.inthemine.com.br\/site\/?p=28787"},"modified":"2025-08-29T13:40:01","modified_gmt":"2025-08-29T16:40:01","slug":"o-carste-de-peruacu","status":"publish","type":"post","link":"https:\/\/www.inthemine.com.br\/site\/o-carste-de-peruacu\/","title":{"rendered":"O CARSTE DE PERUA\u00c7U"},"content":{"rendered":"

Considerado um dos mais importantes s\u00edtios espeleol\u00f3gicos e geomorfol\u00f3gicos do Brasil, o conjunto de cavernas do vale do rio Perua\u00e7u, nas cidades de Janu\u00e1ria e Itacarambi (MG), foi tombado pelo IPHAN (Instituto do Patrim\u00f4nio Hist\u00f3rico Nacional) em mar\u00e7o de 1988, como Parque Nacional Cavernas do Perua\u00e7u. Em 13 de julho de 2025 foi oficializado como Patrim\u00f4nio Mundial pela UNESCO (Organiza\u00e7\u00e3o das Na\u00e7\u00f5es Unidas para a Educa\u00e7\u00e3o, a Ci\u00eancia e a Cultura). O nome Perua\u00e7u, dado pela tribo ind\u00edgena Xacriab\u00e1, que vive na \u00e1rea, significa fenda ou buraco (Peru) muito grande (A\u00e7u).<\/p>\n

O parque est\u00e1 inserido no Planalto C\u00e1rstico do S\u00e3o Francisco, a altitudes entre 500 e 700 m, e apresenta afloramentos de rocha calc\u00e1ria, que ficam expostos entre a vegeta\u00e7\u00e3o formada por ecossistemas da Mata Atl\u00e2ntica, Cerrado e Caatinga (Foto 1, acima). Nesse ambiente de grande geodiversidade, a dissolu\u00e7\u00e3o da rocha carbon\u00e1tica (dolomitos e calc\u00e1rios) e os processos de abatimento criaram vales cegos, escarpamentos na forma de c\u00e2nions, torres calc\u00e1rias, depress\u00f5es fechadas (dolinas e uvalas) e diversas microformas (karren) esculpidas sobre a rocha sol\u00favel. In\u00fameros abrigos e entradas das cavernas apresentam registros de ocupa\u00e7\u00e3o humana datados em at\u00e9 12 mil anos B.P.*, inicialmente por grupos ca\u00e7adores-coletores e mais recentemente por agricultores.<\/p>\n

\"minegaleria112-Foto2\"<\/a>
Foto2<\/figcaption><\/figure>\n

Entre as cavernas percorridas pelo rio Perua\u00e7u tem-se as grutas do Brejal, Cascudos, Troncos e Janel\u00e3o. O Arco do Andr\u00e9 (Foto 2) tamb\u00e9m integra essa rota, mas com o rio tornando-se subterr\u00e2neo em fun\u00e7\u00e3o do soterramento do piso pelos abatimentos. Predominam, nesse conjunto, amplas galerias, como as da gruta do Janel\u00e3o, com 4.740 m de proje\u00e7\u00e3o horizontal e alturas e larguras que podem atingir mais de 100 m.<\/p>\n

\"minegaleria112-Foto3\"<\/a>
Foto3<\/figcaption><\/figure>\n

J\u00e1 as cavernas secas desconectadas do aqu\u00edfero c\u00e1rstico est\u00e3o posicionadas, principalmente, nos pared\u00f5es recuados do c\u00e2nion principal ou em vales secund\u00e1rios, acima do n\u00edvel de base atual do rio Perua\u00e7u, e resultaram de fragmentos abandonados de galerias tribut\u00e1rias da rota de drenagem subterr\u00e2nea preferencial. S\u00e3o elas: Desenhos, Rezar (Foto 3), Caboclo, Bonita, e \u00cdndios, entre outras. H\u00e1 tamb\u00e9m as que est\u00e3o nos pared\u00f5es laterais do c\u00e2nion, como as lapas do Carl\u00facio, Bichos, F\u00f3ssil etc.<\/p>\n

\"minegaleria112-Foto4\"<\/a>
Foto4<\/figcaption><\/figure>\n

Destacam-se, ainda, as gigantescas estalactites e estalagmites do Janel\u00e3o, al\u00e9m das \u201cp\u00e9rolas de caverna\u201d. Ao fundo dessa gruta, na\u00a0dolina dos Macacos, encontra-se a \u201cPerna da Bailarina\u201d, maior estalactite do mundo, com cerca de 28 m de comprimento (Foto 4).<\/p>\n

\"minegaleria112-Foto5\"<\/a>
Foto5<\/figcaption><\/figure>\n

Na gruta Bonita ocorrem helictites, \u201ccascatas\u201d e \u201ccanudos de refresco\u201d e represas de travertinos e colunas podem ser vistas nas grutas do Carl\u00facio, \u00cdndios e Desenhos. O ac\u00famulo de detritos tamb\u00e9m formou outros espeleotemas gigantes (Foto 5), suportados por uma matriz argilosa local cimentada por calcita. Registra-se, ainda, nos pared\u00f5es calc\u00e1rios, grande n\u00famero de inscri\u00e7\u00f5es rupestres em excelente estado de preserva\u00e7\u00e3o (Foto 6).<\/p>\n

\"minegaleria112-Foto6\"<\/a>
Foto6<\/figcaption><\/figure>\n

*Before Present (Antes do Presente) ou antes de 1950 d.C.<\/p>\n

Fotos: Lucas Ninno\/Instituto Ekos – Foto 4: Ataliba Coelho\/IGC-USP<\/h5>\n
Fonte do texto: Artigo \u201cCavernas do Vale do Rio Perua\u00e7u (Janu\u00e1ria e Itacarambi), MG – Obra-prima de carste brasileiro\u201d, de autoria de Lu\u00eds B.Pil\u00f3 e Ezio Rubbioli, que integra a colet\u00e2nea \u00a0\u201cS\u00edtios Geol\u00f3gicos e Paleontol\u00f3gicos do Brasil\u201d, organizada pela Comiss\u00e3o de S\u00edtios Geol\u00f3gicos e Paleobiol\u00f3gicos (SIGEP) e publicada, em 2002, pelo DNPM, atual ANM (Ag\u00eancia Nacional de Minera\u00e7\u00e3o), e CPRM, atual SGB (Servi\u00e7o Geol\u00f3gico do Brasil), com edi\u00e7\u00e3o de Carlos Schobbenhaus, Diogenes de Almeida Campos, Emanuel Teixeira de Queiroz, Manfredo Winge e Myl\u00e8ne Lu\u00edza Cunha Berbert-Born<\/h5>\n

 <\/p>\n","protected":false},"excerpt":{"rendered":"

Parque Nacional Cavernas do Perua\u00e7u, em MG, reconhecido pela UNESCO em 2025, re\u00fane geodiversidade \u00fanica, cavernas monumentais e arte rupestre<\/p>\n","protected":false},"author":3,"featured_media":28788,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[12],"tags":[],"class_list":["post-28787","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-mine-galeria"],"yoast_head":"\nO CARSTE DE PERUA\u00c7U - Revista In The Mine<\/title>\n<meta name=\"description\" content=\"Parque Nacional Cavernas do Perua\u00e7u, em MG, reconhecido pela UNESCO em 2025, re\u00fane geodiversidade \u00fanica, cavernas monumentais e arte rupestre\" \/>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/www.inthemine.com.br\/site\/o-carste-de-peruacu\/\" \/>\n<meta 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