{"id":21794,"date":"2025-08-28T11:16:04","date_gmt":"2025-08-28T10:16:04","guid":{"rendered":"https:\/\/www.gem.pt\/1\/?page_id=21794"},"modified":"2025-08-30T11:56:49","modified_gmt":"2025-08-30T10:56:49","slug":"algar-picos-i-alguns-apontamentos","status":"publish","type":"page","link":"https:\/\/www.gem.pt\/1\/en\/publicacoes\/carso-e-endocarso\/algar-picos-i-alguns-apontamentos\/","title":{"rendered":"Algar Picos I &#8211; Alguns Apontamentos"},"content":{"rendered":"<div data-elementor-type=\"wp-page\" data-elementor-id=\"21794\" class=\"elementor elementor-21794\">\n\t\t\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-42d2622 elementor-section-full_width elementor-section-height-default elementor-section-height-default\" data-id=\"42d2622\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"aux-parallax-section elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-ea19d18\" data-id=\"ea19d18\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-cc72f5f elementor-widget elementor-widget-image\" data-id=\"cc72f5f\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t<figure class=\"wp-caption\">\n\t\t\t\t\t\t\t\t\t\t<img decoding=\"async\" src=\"https:\/\/www.gem.pt\/wp-content\/uploads\/elementor\/thumbs\/Algar-Picos-I-pan-rm1ie3m7mtlbodfnu5qvrl4ao6a829qq9663ibpfog.jpeg\" title=\"Algar-Picos-I-pan\" alt=\"Algar-Picos-I-pan\" loading=\"lazy\" \/>\t\t\t\t\t\t\t\t\t\t\t<figcaption class=\"widget-image-caption wp-caption-text\">Algar Picos I - Alguns Apontamentos<\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-76edf0e elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"76edf0e\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"aux-parallax-section elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-f07a9a4\" data-id=\"f07a9a4\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-09446b1 elementor-widget elementor-widget-text-editor\" data-id=\"09446b1\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<div style=\"text-align: right; line-height: 0.8;\"><span style=\"letter-spacing: normal; font-family: Questrial; font-size: 14px; white-space: pre-line;\">28 de Agosto de 2025<\/span><\/div>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-1322330 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"1322330\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"aux-parallax-section elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-f837e70\" data-id=\"f837e70\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-a0c2aef elementor-widget elementor-widget-text-editor\" data-id=\"a0c2aef\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<div id=\"introducao\" style=\"letter-spacing: normal; margin: 0px; padding: 0px; font-family: Questrial; font-size: 14px; text-align: justify; white-space: pre-line;\"><p><span style=\"caret-color: #e78b00; color: #e78b00; font-size: 20px;\">Introdu\u00e7\u00e3o<\/span><\/p><div style=\"margin: 0px; padding: 0px;\"><p><span style=\"font-size: 16px; letter-spacing: 0px;\">O algar Picos I encontra-se no Maci\u00e7o Calc\u00e1rio Estremenho, na unidade morfoestrutural do planalto de Santo Ant\u00f3nio. perto da localidade de Penedos, Belos, concelho de Porto de M\u00f3s As coordenadas geogr\u00e1ficas de entrada da gruta (WGS84) s\u00e3o latitude: 39,50587\u00ba e Longitude: -8,747879 e Z aproximado de 385 metros.<\/span><\/p><\/div><\/div>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-e62d205 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"e62d205\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"aux-parallax-section elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-6a9477c\" data-id=\"6a9477c\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-5c6181a elementor-widget elementor-widget-text-editor\" data-id=\"5c6181a\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<div id=\"enquadramento\" style=\"letter-spacing: normal; margin: 0px; padding: 0px; font-family: Questrial; font-size: 14px; text-align: justify; white-space: pre-line;\"><p><span style=\"caret-color: #e78b00; color: #e78b00; font-size: 20px;\">Description<\/span><\/p><div style=\"margin: 0px; padding: 0px;\"><p><span style=\"font-size: 16px; letter-spacing: 0px;\">A gruta \u00e9 composta por um po\u00e7o de 16m, a partir do qual se tem acesso a uma galeria de sec\u00e7\u00e3o m\u00e9trica, e cerca de 30m de extens\u00e3o de orienta\u00e7\u00e3o NW-SE, fortemente concrecionada onde a gruta atinge os -25m, a sua profundidade m\u00e1xima.<\/span><\/p><\/div><\/div>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-840daf2 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"840daf2\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"aux-parallax-section elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-bbed6e6\" data-id=\"bbed6e6\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-e359efb elementor-widget__width-initial elementor-widget elementor-widget-image\" data-id=\"e359efb\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t<figure class=\"wp-caption\">\n\t\t\t\t\t\t\t\t\t\t\t<a href=\"https:\/\/www.gem.pt\/wp-content\/uploads\/2025\/08\/Figura_1_Topografia.jpg\" data-elementor-open-lightbox=\"yes\" data-elementor-lightbox-title=\"Figura 1 - Topografia da Gruta\" data-e-action-hash=\"#elementor-action%3Aaction%3Dlightbox%26settings%3DeyJpZCI6MjE3OTcsInVybCI6Imh0dHBzOlwvXC93d3cuZ2VtLnB0XC93cC1jb250ZW50XC91cGxvYWRzXC8yMDI1XC8wOFwvRmlndXJhXzFfVG9wb2dyYWZpYS5qcGcifQ%3D%3D\">\n\t\t\t\t\t\t\t<img decoding=\"async\" src=\"https:\/\/www.gem.pt\/wp-content\/uploads\/elementor\/thumbs\/Figura_1_Topografia-rm1ied0akgx4pebu9fex3cbp77c8mvqhnqvl39njjq.jpg\" title=\"Figura 1 &#8211; Topografia da Gruta\" alt=\"Figura 1 - Topografia da gruta, realizada pelo antigo Espeleoclube de Sintra\" loading=\"lazy\" \/>\t\t\t\t\t\t\t\t<\/a>\n\t\t\t\t\t\t\t\t\t\t\t<figcaption class=\"widget-image-caption wp-caption-text\">Figura 1 - Topografia da gruta, realizada pelo antigo Espeleoclube de Sintra<\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-aa11579 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"aa11579\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"aux-parallax-section elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-5818e4c\" data-id=\"5818e4c\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-3fab05a elementor-widget elementor-widget-text-editor\" data-id=\"3fab05a\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<div id=\"descricao\" style=\"letter-spacing: normal; margin: 0px; padding: 0px; font-family: Questrial; font-size: 14px; text-align: justify; white-space: pre-line;\"><p><span style=\"caret-color: #e78b00; color: #e78b00; font-size: 20px;\">Geological Setting<\/span><\/p><div style=\"margin: 0px; padding: 0px;\"><p><span style=\"font-size: 16px; letter-spacing: 0px;\">De acordo com a folha 27-A da Carta Geol\u00f3gica de Portugal &#8211; \u00e0 escala 1:50000 (Manupella et al), a gruta desenvolve se na forma\u00e7\u00e3o de Margas e Calc\u00e1rios margosos do Zambujal, datada do andar Aaleniano a Bajociano Inferior, do Jur\u00e1ssico M\u00e9dio. As camadas apresentam,\u00a0 regionalmente de acordo com a Carta acima referida atitude entre NW-SE e NNW-SSE a inclinar cerca de 10 a 30\u00ba para Sul.<br \/><\/span><\/p><\/div><\/div>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-7167d60 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"7167d60\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"aux-parallax-section elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-4420a8b\" data-id=\"4420a8b\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-75ed408 elementor-widget elementor-widget-text-editor\" data-id=\"75ed408\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<div id=\"descricao\" style=\"letter-spacing: normal; margin: 0px; padding: 0px; font-family: Questrial; font-size: 14px; text-align: justify; white-space: pre-line;\"><p><span style=\"caret-color: #e78b00; color: #e78b00; font-size: 20px;\">Structural Control<\/span><\/p><div style=\"margin: 0px; padding: 0px;\"><p><span style=\"font-size: 16px; letter-spacing: 0px;\">A entrada da gruta \u00e9 controlada por uma fratura de atitude aproximada E-W\/Vertical. A galeria parece seguir a inclina\u00e7\u00e3o das camadas, que apresentam localmente atitude N70W\/10S.<br \/><\/span><\/p><\/div><\/div>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-2b1df99 elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"2b1df99\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"aux-parallax-section elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-0fb17ad\" data-id=\"0fb17ad\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-3ef5683 elementor-widget__width-initial elementor-widget elementor-widget-image\" data-id=\"3ef5683\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"image.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t\t\t\t<figure class=\"wp-caption\">\n\t\t\t\t\t\t\t\t\t\t\t<a href=\"https:\/\/www.gem.pt\/wp-content\/uploads\/2025\/08\/Figura_2.jpg\" data-elementor-open-lightbox=\"yes\" data-elementor-lightbox-title=\"Figura 2 - Aspeto do interior da galeria\" data-e-action-hash=\"#elementor-action%3Aaction%3Dlightbox%26settings%3DeyJpZCI6MjE3OTgsInVybCI6Imh0dHBzOlwvXC93d3cuZ2VtLnB0XC93cC1jb250ZW50XC91cGxvYWRzXC8yMDI1XC8wOFwvRmlndXJhXzIuanBnIn0%3D\">\n\t\t\t\t\t\t\t<img decoding=\"async\" src=\"https:\/\/www.gem.pt\/wp-content\/uploads\/elementor\/thumbs\/Figura_2-rm1idywppydtv8wbjrbijxvsaf9qff6ilt3aw48fnk.jpg\" title=\"Figura 2 &#8211; Aspeto do interior da galeria\" alt=\"Figura 2 - Aspeto do interior da galeria\" loading=\"lazy\" \/>\t\t\t\t\t\t\t\t<\/a>\n\t\t\t\t\t\t\t\t\t\t\t<figcaption class=\"widget-image-caption wp-caption-text\">Figura 2 - Aspeto do interior da galeria<\/figcaption>\n\t\t\t\t\t\t\t\t\t\t<\/figure>\n\t\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-8c2271a elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"8c2271a\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"aux-parallax-section elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-e2ea6c8\" data-id=\"e2ea6c8\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-aac0eb8 elementor-widget elementor-widget-text-editor\" data-id=\"aac0eb8\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<div id=\"descricao\" style=\"letter-spacing: normal; margin: 0px; padding: 0px; font-family: Questrial; font-size: 14px; text-align: justify; white-space: pre-line;\"><p><span style=\"caret-color: #e78b00; color: #e78b00; font-size: 20px;\">Genesis and Evolution<\/span><\/p><div style=\"margin: 0px; padding: 0px;\"><p><span style=\"font-size: 16px; letter-spacing: 0px;\">A gruta formou-se na zona fre\u00e1tica de acordo com a defini\u00e7\u00e3o de B\u00f6gli 1980, como o comprovam a sec\u00e7\u00e3o arredondada das galeria e vagas de eros\u00e3o. O Algar Picos I marca um antigo n\u00edvel de circula\u00e7\u00e3o de \u00e1gua que atualmente se encontra \u00e0 cota aproximada de 360-370m. A gruta, por uma descida relativa do n\u00edvel de base, passou da zona fre\u00e1tica para a zona vadosa inactiva. A entrada abriu-se posteriormente com o abatimento do tecto da gruta que se encontra muito perto da superf\u00edcie.<br \/><\/span><\/p><\/div><\/div>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<section class=\"elementor-section elementor-top-section elementor-element elementor-element-b77ae8e elementor-section-boxed elementor-section-height-default elementor-section-height-default\" data-id=\"b77ae8e\" data-element_type=\"section\" data-e-type=\"section\">\n\t\t\t\t\t\t<div class=\"elementor-container elementor-column-gap-default\">\n\t\t\t\t\t<div class=\"aux-parallax-section elementor-column elementor-col-100 elementor-top-column elementor-element elementor-element-c228968\" data-id=\"c228968\" data-element_type=\"column\" data-e-type=\"column\">\n\t\t\t<div class=\"elementor-widget-wrap elementor-element-populated\">\n\t\t\t\t\t\t<div class=\"elementor-element elementor-element-4262646 elementor-widget elementor-widget-text-editor\" data-id=\"4262646\" data-element_type=\"widget\" data-e-type=\"widget\" data-widget_type=\"text-editor.default\">\n\t\t\t\t<div class=\"elementor-widget-container\">\n\t\t\t\t\t\t\t\t\t<div style=\"letter-spacing: normal; margin: 0px; padding: 0px; font-family: Questrial; font-size: 14px; text-align: justify; white-space: pre-line;\"><p><span style=\"caret-color: #e78b00; color: #e78b00; font-size: 20px; text-align: left;\">Bibliography<\/span><span style=\"caret-color: #e78b00; color: #e78b00; font-size: 20px; text-align: left;\"><br \/><\/span><\/p><ul style=\"margin-right: 0px; margin-bottom: 0px; padding-right: 0.3em; padding-left: 2em; clear: both;\"><li><span style=\"caret-color: #000000; color: #000000;\">Baro\u00f1, I. 2002. Speleogenesis along subvertical joints: A model of plateau karst shaft development: A case study: the Doln\u00fd Vrch Plateau (Slovak Republic), Cave&amp; Karst Science 29 (1), 2002, 5-12.\u00a0 Available at <a href=\"https:\/\/cloud3.bcra.org.uk\/cdn\/cavescience\/3_CaveAndKarstScience\/cks085.pdf\">https:\/\/cloud3.bcra.org.uk\/cdn\/cavescience\/3_CaveAndKarstScience\/cks085.pdf<\/a><\/span><\/li><li><span style=\"caret-color: #000000; color: #000000;\">B\u00f6gli, A. (1980), Karst Hydrology and Physical Speleology, Springer-Verlag, Berlin Heildelberg New York.<\/span><span style=\"caret-color: #000000; color: #000000;\"><br \/><\/span><\/li><li style=\"line-height: 26.6px;\"><span style=\"caret-color: #000000; color: #000000;\">Manupella, G., Telles Antunes, M., Costa Almeida, C.A., Azer\u00eado, A.C., Barbosa, B., Cardoso, J.L., Crispim, J.A., Duarte, L.V., Henriques, M.H., Martins, L.T., Ramalho, M.M.; Santos, V.F.; Terrinha. P.; (2000). Carta Geol\u00f3gica de Portugal \u2013 Vila Nova de Our\u00e9m, Folha 27-A, \u00e0 escala 1:50.000, e Nota Explicativa, Instituto Geol\u00f3gico e Mineiro, Lisboa.<\/span><\/li><\/ul><\/div>\t\t\t\t\t\t\t\t<\/div>\n\t\t\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/div>\n\t\t\t\t\t<\/div>\n\t\t<\/section>\n\t\t\t\t<\/div>","protected":false},"excerpt":{"rendered":"<p>Algar Picos I &#8211; Alguns Apontamentos 28 de Agosto de 2025 Introdu\u00e7\u00e3o O algar Picos I encontra-se no Maci\u00e7o Calc\u00e1rio Estremenho, na unidade morfoestrutural do planalto de Santo Ant\u00f3nio. perto da localidade de Penedos, Belos, concelho de Porto de M\u00f3s As coordenadas geogr\u00e1ficas de entrada da gruta (WGS84) s\u00e3o latitude: 39,50587\u00ba e Longitude: -8,747879 e [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":1574,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"footnotes":""},"class_list":["post-21794","page","type-page","status-publish","hentry"],"_links":{"self":[{"href":"https:\/\/www.gem.pt\/1\/en\/wp-json\/wp\/v2\/pages\/21794","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/www.gem.pt\/1\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/www.gem.pt\/1\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/www.gem.pt\/1\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/www.gem.pt\/1\/en\/wp-json\/wp\/v2\/comments?post=21794"}],"version-history":[{"count":0,"href":"https:\/\/www.gem.pt\/1\/en\/wp-json\/wp\/v2\/pages\/21794\/revisions"}],"up":[{"embeddable":true,"href":"https:\/\/www.gem.pt\/1\/en\/wp-json\/wp\/v2\/pages\/1574"}],"wp:attachment":[{"href":"https:\/\/www.gem.pt\/1\/en\/wp-json\/wp\/v2\/media?parent=21794"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}