{"id":29982,"date":"2026-03-02T12:25:57","date_gmt":"2026-03-02T15:25:57","guid":{"rendered":"https:\/\/www.inthemine.com.br\/site\/?p=29982"},"modified":"2026-03-02T12:25:57","modified_gmt":"2026-03-02T15:25:57","slug":"as-demoiselles-coiffees-de-goias","status":"publish","type":"post","link":"https:\/\/www.inthemine.com.br\/site\/as-demoiselles-coiffees-de-goias\/","title":{"rendered":"AS DEMOISELLES COIFF\u00c9ES DE GOI\u00c1S"},"content":{"rendered":"
\"Foto1\"<\/a>
Foto1<\/figcaption><\/figure>\n

As \u201cdonzelas penteadas\u201d ou \u201ccom chap\u00e9us\u201d, assim chamadas por sua apar\u00eancia que lembra figuras humanas femininas esguias com um penteado alto ou usando um chap\u00e9u, soube-se h\u00e1 pouco tempo, mais exatamente em 2022, habitam uma vasta \u00e1rea entre 5 e 5,5 hectares, n\u00e3o na Fran\u00e7a, mas em Campos Belos, no nordeste de Goi\u00e1s, que fica pr\u00f3xima \u00e0 divisa com o Tocantins e a Bahia. A partir da divulga\u00e7\u00e3o p\u00fablica das imagens, a regi\u00e3o passou a ser conhecida como \u201cVale de Marte\u201d.<\/p>\n

\"Foto<\/a>
Foto 2<\/figcaption><\/figure>\n

A forma\u00e7\u00e3o geol\u00f3gica rara no Brasil, que atende tamb\u00e9m pelo nome de \u201cChamin\u00e9 de Fada\u201d, foi apresentada em fotos por uma moradora local \u00e0 ge\u00f3loga e pesquisadora do Laborat\u00f3rio de Geologia em \u00c1reas Tur\u00edsticas da UFG (Universidade Federal de Goi\u00e1s), Joana Paula Sanchez, que organizou uma equipe de pesquisadores para um estudo de campo (Fotos 1 a 3).<\/p>\n

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

Segundo Joana, a ocorr\u00eancia desse tipo de forma\u00e7\u00e3o \u00e9 resultado de uma eros\u00e3o diferencial causada pela presen\u00e7a de diferentes tipos de rochas que se desgastam em ritmos distintos. A fazenda onde as chamin\u00e9s de fada est\u00e3o \u00e9 de propriedade de Domingos Ferreira da Silva, que acompanhou a pesquisadora na visita (Foto 4).<\/p>\n

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

No caso do Vale de Marte havia, antigamente, um rio local que, durante as \u00e9pocas de cheia ou tempestades, carregava grandes rochas vindas das montanhas ao redor. Com o tempo, o rio foi escavando a base dos conglomerados, moldando as estruturas que podem chegar entre tr\u00eas e quatro m de altura, explicou a pesquisadora. A rocha formada no alto da torre, semelhante a um penteado ou chamin\u00e9, ocorre porque a rocha inferior \u00e9 mais macia que a camada superior, que atua como uma esp\u00e9cie de \u201ctampa\u201d\u00a0protegendo o topo do t\u00f3tem. \u201cDiferentemente de outras chamin\u00e9s de fada conhecidas, geralmente formadas por rochas vulc\u00e2nicas sobre tufos, as dessa regi\u00e3o t\u00eam origem sedimentar. Elas se formaram em um antigo leito de rio que secou, e, gra\u00e7as \u00e0 atual desertifica\u00e7\u00e3o, permanecem preservadas, j\u00e1 que n\u00e3o h\u00e1 mais fluxo de \u00e1gua suficiente para erodi-las”, afirma Joana.<\/p>\n

Ao longo do tempo, uma rocha mais dura acabava depositada sobre outra mais fr\u00e1gil, que erode facilmente. A a\u00e7\u00e3o da chuva e do vento retira os sedimentos que se acumularam em torno das rochas mais consistentes, mantendo a parte que fica sob cada bloco, que funciona como um chap\u00e9u de prote\u00e7\u00e3o. \u201cTemos a impress\u00e3o de que as torres se ergueram, mas foi o entorno delas que cedeu\u201d, conclui a ge\u00f3loga.<\/p>\n

A Serra Geral de Goi\u00e1s \u00e9 parte de um extenso pared\u00e3o que corta o centro do Brasil de norte a sul, dividindo os estados do Maranh\u00e3o, Tocantins e Bahia. Segundo Joana, a forma\u00e7\u00e3o dessa regi\u00e3o aconteceu em uma das movimenta\u00e7\u00f5es tect\u00f4nicas mais antigas que temos no pa\u00eds, a Sanfranciscana, h\u00e1 mais de 400 milh\u00f5es de anos. O movimento das placas, ainda na \u00e9poca em que os continentes estavam juntos, causou uma depress\u00e3o, uma bacia, onde o arenito, que \u00e9 sedimentar, se depositou. O grande diferencial dessa forma\u00e7\u00e3o em Goi\u00e1s \u00e9 sua grande extens\u00e3o.<\/p>\n

O Instituto Chico Mendes de Conserva\u00e7\u00e3o da Biodiversidade (ICMBio), que visitou a \u00e1rea em setembro de 2025, abriu um processo para transform\u00e1-la em uma unidade de conserva\u00e7\u00e3o. Discute-se a abertura de visitas guiadas ao local a partir de abril deste ano (2026).<\/p>\n

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

As chamin\u00e9s de fada mais conhecidas est\u00e3o na Capad\u00f3cia, na Turquia (Foto 5), Alpes franceses, desertos de Utah (EUA) e em pequenas \u00e1reas do Canad\u00e1, It\u00e1lia e Taiwan. Essa denomina\u00e7\u00e3o deriva de lendas do folclore europeu, que contavam de seres m\u00e1gicos que habitariam o interior das torres.<\/p>\n

Fotos 1 a 4: Cr\u00e9dito: Joana S\u00e1nchez\/Divulga\u00e7\u00e3o – Foto 5: Portal Headout\/Divulga\u00e7\u00e3o<\/h5>\n","protected":false},"excerpt":{"rendered":"

Forma\u00e7\u00f5es sedimentares raras em Campos Belos revelam torres moldadas por eros\u00e3o e podem virar \u00e1rea protegida<\/p>\n","protected":false},"author":3,"featured_media":29983,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[12],"tags":[],"class_list":["post-29982","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-mine-galeria"],"yoast_head":"\nAS DEMOISELLES COIFF\u00c9ES DE GOI\u00c1S - Revista In The Mine<\/title>\n<meta name=\"description\" content=\"Forma\u00e7\u00f5es sedimentares raras em Campos Belos revelam torres moldadas por eros\u00e3o e podem virar \u00e1rea protegida\" \/>\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\/as-demoiselles-coiffees-de-goias\/\" \/>\n<meta property=\"og:locale\" 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