{"id":1517,"date":"2022-04-20T13:37:19","date_gmt":"2022-04-20T18:37:19","guid":{"rendered":"http:\/\/geoparquemixtecaalta.org\/?page_id=1517"},"modified":"2024-08-13T21:01:20","modified_gmt":"2024-08-14T03:01:20","slug":"geositios-y-geosenderos","status":"publish","type":"page","link":"https:\/\/geoparquemixtecaalta.org\/en\/geositios-y-geosenderos\/","title":{"rendered":"Geosites and Geotrails"},"content":{"rendered":"<h1>\n<p><strong>Geosites and Geotrails<\/strong><\/p>\n<\/h1>\n<h1>\n<p><strong><span>WHAT ARE GEOTRAILS?<\/span><\/strong><\/p>\n<\/h1>\n<hr>\n<div>\n<p><span>The trail allows the visitor to discover thematically interconnected sites which are complementary to each other, so that the visitor, along the route, learns a coherent history and not an isolated knowledge of each of the sites visited. In this way, the trails are a didactic resource focused on the popularization of geoheritage and a service that enriches the geotourism offer for the benefit of visitors and the local communities in which they are located.<\/span><\/p>\n<\/div>\n<p><img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Geosenderos-mapa.jpg\" alt=\"\"><\/p>\n<div>\n<p><strong>NOTE:<\/strong><\/p>\n<p><span>Tours are conducted in local vehicles with a maximum capacity of 10 people. The maximum number of participants in each tour is 20 people. In all cases, the tours are led by local guides.<\/span><\/p>\n<\/div>\n<ul>\n<li>\n<h3>GT1 &#8211; LOS CORAZONES, 30 KM<\/h3>\n<div>\n<p><span>Longest route in the geopark, lithological contacts, lamabordos, plutonic structures, viewpoints.<\/span><\/p>\n<\/div>\n<p><a href=\"\/en\/wp-content\/uploads\/2022\/04\/Geosendero-Los-Corazones.pdf\">PDF<\/a><\/p>\n<\/li>\n<li>\n<h3>GT2 &#8211; LAS CONCHAS, 3 KM<\/h3>\n<div>\n<p><span>Badlands, gullies and erosional cirques in the Yanhuitl\u00e1n Formation, paleosols and alluvial forms, archaeological ruins.<\/span><\/p>\n<\/div>\n<p><a href=\"\/en\/wp-content\/uploads\/2022\/04\/Geosendero-Las-Conchas.pdf\">PDF<\/a><\/p>\n<\/li>\n<li>\n<h3>GT3 &#8211; CERRO DEL SOL, 3 KM<\/h3>\n<div>\n<p><span>Panoramic views of the Llano de Lobos Tuff, lithological contacts and local faults.<\/span><\/p>\n<\/div>\n<p><a href=\"\/en\/wp-content\/uploads\/2022\/04\/Geosendero-Cerro-del-Sol.pdf\">PDF<\/a><\/p>\n<\/li>\n<li>\n<h3>GT4 &#8211; R\u00cdO DEL \u00c1GUILA, 4 KM<\/h3>\n<div>\n<p><span>Lithological contacts, erosional cirques and lamabordo, volcanic lithology.<\/span><\/p>\n<\/div>\n<p><a href=\"\/en\/wp-content\/uploads\/2022\/04\/Geosendero-Rio-del-Aguila.pdf\">PDF<\/a><\/p>\n<\/li>\n<li>\n<h3>GT5 &#8211; YUTOTO<\/h3>\n<div>\n<p><span>Karstic landscapes, lamabordos, limestone quarries, fossils and archaeological remains.<\/span><\/p>\n<\/div>\n<p><a href=\"\/en\/wp-content\/uploads\/2022\/04\/Geosendero-Yutoto.pdf\">PDF<\/a><\/p>\n<\/li>\n<li>\n<h3>GT6 &#8211; EL JAZM\u00cdN, 4 KM<\/h3>\n<div>\n<p><span>Main archaeological site in the Geopark; alluvial archives, paleosoils and fluvial forms and panoramic views of the Yanhuitl\u00e1n Valley<\/span><\/p>\n<\/div>\n<p><a href=\"\/en\/wp-content\/uploads\/2022\/04\/Geosendero-Jazmin.pdf\">PDF<\/a><\/p>\n<\/li>\n<li>\n<h3>GT7 &#8211; TEJOCOTAL, 12.5 KM<\/h3>\n<div>\n<p><span>Outcrops of the Llano de Lobos Tuff, lithological contacts, main geological units, viewpoints of the valleys.<\/span><\/p>\n<\/div>\n<p><a href=\"\/en\/wp-content\/uploads\/2022\/04\/Geosendero-Tejocotal.pdf\">PDF<\/a><\/p>\n<\/li>\n<li>\n<h3>GT8 &#8211; SAN PEDRO A\u00d1A\u00d1E DYKES, 5 KM<\/h3>\n<div>\n<p><span>Lamabordos, plutonic structures, gullies and badlands.<\/span><\/p>\n<\/div>\n<p><a href=\"\/en\/wp-content\/uploads\/2022\/04\/Geosendero-Diques-de-San-Pedro-Anane.pdf\">PDF<\/a><\/p>\n<\/li>\n<\/ul>\n<hr>\n<ul>\n<li>\n<h3>SN1 &#8211; CERRO VERDE, 3 KM<\/h3>\n<div>\n<p><span>Route to the highest altitude of the Mixteca Alta, continental watershed, gullies, badlands, plutonic structures and archaeological sites.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<h3>SN2 &#8211; PE\u00d1A AZUL, 3 KM<\/h3>\n<div>\n<p><span>Panoramic view of the Yanhuitl\u00e1n, Yucuita and Nochixtl\u00e1n valleys; main geomorphological units, well-preserved forests and a variety of orchids (in season).<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<h3>SN3 &#8211; YUXACINO, 4 KM<\/h3>\n<div>\n<p><span>Alluvial profiles and local faults. Collection of edible insects.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<h3>SN4 &#8211; \u00d1U&#8217;UN YUCU, 4 KM<\/h3>\n<div>\n<p><span>Well-preserved oak forests, panoramic views of the Yanhuitl\u00e1n Valley, bird watching and a variety of orchids depending on the season.<\/span><\/p>\n<\/div>\n<\/li>\n<\/ul>\n<h1><strong>Geosites<\/strong><\/h1>\n<hr>\n<div>\n<p><span>Geosites are sites of geological interest representative of the geoheritage of the geopark. There are 35 identified geosites, although others that have been identified are under study.<\/span><\/p>\n<\/div>\n<ul>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Mirador-los-dos-corazones.jpg\" alt=\"\"><\/p>\n<h3>Mirador de los dos corazones<\/h3>\n<div>\n<p><span>Mass removal processes, erosive cirques, gullies and lamabordos.<\/span><\/p>\n<p><span>\u00a0<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Mirador-Sta.-Maria-Pozoltepec.jpg\" alt=\"\"><\/p>\n<h3> Sta. Mar\u00eda Pozoltepec viewpoint<\/h3>\n<div>\n<p><span>Lithological contours of main units: Yanhuitl\u00e1n- Toba Llano de lobos Formation.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Cascada-Sta.-Maria-Pozoltepec.jpg\" alt=\"\"><\/p>\n<h3>Sta. Mar\u00eda Pozoltepec Waterfall<\/h3>\n<div>\n<p><span>Dikes, contact metamorphism, structural control of rivers.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Mirador-vista-hermosa.jpg\" alt=\"\"><\/p>\n<h3>Vista Hermosa Viewpoint<\/h3>\n<div>\n<p><span>Badlands, dykes, contact between physiographic provinces.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Andesita-Yucudaac.jpg\" alt=\"\"><\/p>\n<h3>Andesite Yucudaac<\/h3>\n<div>\n<p><span>Exfoliation, spheroidal weathering.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Deslizamientos-Yucuita.jpg\" alt=\"\"><\/p>\n<h3>Yucuita landslides<\/h3>\n<div>\n<p><span>Processes of mass removal, landslides and lamabordos.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Mirador-de-los-valles-de-Nochixtlan-y-Yanhuitlan.jpg\" alt=\"\"><\/p>\n<h3>Nochixtl\u00e1n and Yanhuitl\u00e1n valleys viewpoint.<\/h3>\n<div>\n<p><span>Gullies, badlands, regional faults and lamabordos systems.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Rio-Yanhuitlan.jpg\" alt=\"\"><\/p>\n<h3>Yanhuitl\u00e1n River<\/h3>\n<div>\n<p><span>Alluvial files and paleosoils.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Sitio-Las-Conchas.jpg\" alt=\"\"><\/p>\n<h3>Las Conchas Site<\/h3>\n<div>\n<p><span>Landslide processes, erosional cirques, gullies and lamabordos.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Mirador-Las-Conchas.jpg\" alt=\"\"><\/p>\n<h3>Las Conchas viewpoint<\/h3>\n<div>\n<p><span>Gullies, badlands, regional faults, exocarstic features and lamabordos systems.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Prismas-de-Pena-azul.jpg\" alt=\"\"><\/p>\n<h3>Pe\u00f1a Azul Prisms<\/h3>\n<div>\n<p><span>Lava structures, waterfalls.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/12-Diques-de-San-Pedro-Anane.jpg\" alt=\"\"><\/p>\n<h3>San Pedro A\u00f1a\u00f1e dykes<\/h3>\n<div>\n<p><span>Dikes and sill, differential erosion, gullies, badlands, regional faults and lamabordos systems.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Archivos-aluviales-del-rio-Yanhuitlan.jpg\" alt=\"\"><\/p>\n<h3>Yanhuitl\u00e1n river alluvial archives.<\/h3>\n<div>\n<p><span>Alluvial archives, paleosoils and lamabordos.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Sitio-Rio-Verde.jpg\" alt=\"\"><\/p>\n<h3>R\u00edo Verde Site<\/h3>\n<div>\n<p><span>Lithological contacts of main units, tectonics, regional faults.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Mirador-Valle-de-Yanhuitlan.jpg\" alt=\"\"><\/p>\n<h3>Yanhuitl\u00e1n Valley Viewpoint<\/h3>\n<div>\n<p><span>Landslide processes, erosional cirques, gullies and badlands, lamabordos systems.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Sitio-Yudayo.jpg\" alt=\"\"><\/p>\n<h3>Yudayo Site<\/h3>\n<div>\n<p><span>Eroded lamabordos and alluvial deposits.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Sitio-San-Isidro-y-Suchixtlahuaca.jpg\" alt=\"\"><\/p>\n<h3>San Isidro and Suchixtlahuaca Site<\/h3>\n<div>\n<p><span>Lithological contacts of main units and intrusive bodies.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Sitio-Boqueron.jpg\" alt=\"\"><\/p>\n<h3>Boquer\u00f3n Site<\/h3>\n<div>\n<p><span>Landslide processes, erosional cirques, gullies and lamabordos.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Sitio-Yuxacino.jpg\" alt=\"\"><\/p>\n<h3> Yuxacino Site<\/h3>\n<div>\n<p><span>Paleontology (mammoths), alluvial deposits.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Mirador-Tonaltepec.jpg\" alt=\"\"><\/p>\n<h3> Tonaltepec Viewpoint<\/h3>\n<div>\n<p><span>Gullies, badlands, regional faults and lamabordos systems.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Cerro-del-Sol-Yucunchi.jpg\" alt=\"\"><\/p>\n<h3>Cerro del Sol (Yucunchi)<\/h3>\n<div>\n<p><span>Lithological contacts of main units, tectonism, regional faults.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Cerro-Verde.jpg\" alt=\"\"><\/p>\n<h3>Cerro Verde<\/h3>\n<div>\n<p><span>Continental watershed.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Sitio-Dequenini.jpg\" alt=\"\"><\/p>\n<h3>Dequenini Site<\/h3>\n<div>\n<p><span>Lithological contacts of main units.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Rio-del-Aguila.jpg\" alt=\"\"><\/p>\n<h3>Eagle River<\/h3>\n<div>\n<p><span>Lithological contacts of main units, fluvial forms and tectonism.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Rio-Yutzateche.jpg\" alt=\"\"><\/p>\n<h3>Yutzateche river<\/h3>\n<div>\n<p><span>Lithologic contacts, base of the stratigraphic column (Cretaceous-Paleogene).<\/span><\/p>\n<p><span>\u00a0<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Sitio-Yutoto.jpg\" alt=\"\"><\/p>\n<h3>Yutoto site<\/h3>\n<div>\n<p><span>Endo- and exocarstic features and fluvial features.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Sitio-Agencia-Guadalupe-Gavillera.jpg\" alt=\"\"><\/p>\n<h3>Guadalupe Gavillera Agency Site<\/h3>\n<div>\n<p><span>Karstic features: lapiaz, caves, Cretaceous fossils.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Cantera-de-calizas.jpg\" alt=\"\"><\/p>\n<h3>Limestone quarry<\/h3>\n<div>\n<p><span>Limestones.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Mirador-San-Isidro-Tejocotal.jpg\" alt=\"\"><\/p>\n<h3>San Isidro Tejocotal viewpoint.<\/h3>\n<div>\n<p><span>Main geomorphological units of the geopark.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Cantera-Caliza-Teposcolula.jpg\" alt=\"\"><\/p>\n<h3>Teposcolula Limestone Quarry<\/h3>\n<div>\n<p><span>Abandoned quarry, limestone blocks.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Sitio-La-Laguna.jpg\" alt=\"\"><\/p>\n<h3>La Laguna site<\/h3>\n<div>\n<p><span>Karstic features: lapiaz, caves, terra rossa.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Sitio-La-Laguna.jpg\" alt=\"\"><\/p>\n<h3>Yutzateche site<\/h3>\n<div>\n<p><span>Lava structures.<\/span><\/p>\n<p><span>\u00a0<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Sitio-Yucudaac.jpg\" alt=\"\"><\/p>\n<h3>Yucudaac site<\/h3>\n<div>\n<p><span>Exfoliation, spheroidal weathering.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Sitio-Cerro-Corneta.jpg\" alt=\"\"><\/p>\n<h3> Cerro Corneta site<\/h3>\n<div>\n<p><span>Mass removal processes, erosive cirques, gullies and lamabordos.<\/span><\/p>\n<\/div>\n<\/li>\n<li>\n<p>        <img decoding=\"async\" src=\"\/en\/wp-content\/uploads\/2022\/04\/Sitio-Caballo-Blanco.jpg\" alt=\"\"><\/p>\n<h3>Caballo Blanco site<\/h3>\n<div>\n<p><span>Mass removal processes, erosive cirques, gullies and lamabordos.<\/span><\/p>\n<\/div>\n<\/li>\n<\/ul>\n<p><!--more--><br \/>\n<!-- {\"name\":\"Post\",\"type\":\"layout\",\"children\":[{\"type\":\"section\",\"props\":{\"style\":\"default\",\"width\":\"default\",\"vertical_align\":\"middle\",\"title_position\":\"top-left\",\"title_rotation\":\"left\",\"title_breakpoint\":\"xl\",\"image_position\":\"center-center\",\"padding\":\"none\",\"padding_remove_horizontal\":true},\"children\":[{\"type\":\"row\",\"children\":[{\"type\":\"column\",\"props\":{\"position_sticky_breakpoint\":\"m\",\"image_position\":\"center-center\",\"media_overlay_gradient\":\"\"},\"children\":[]}]}],\"name\":\"HEADER \"},{\"type\":\"section\",\"props\":{\"style\":\"secondary\",\"width\":\"default\",\"vertical_align\":\"middle\",\"title_position\":\"top-left\",\"title_rotation\":\"left\",\"title_breakpoint\":\"xl\",\"image_position\":\"center-center\"},\"children\":[{\"type\":\"row\",\"children\":[{\"type\":\"column\",\"props\":{\"position_sticky_breakpoint\":\"m\",\"image_position\":\"center-center\",\"media_overlay_gradient\":\"\"},\"children\":[{\"type\":\"headline\",\"props\":{\"title_element\":\"h1\",\"title_style\":\"heading-medium\",\"block_align\":\"center\",\"text_align\":\"center\",\"margin_remove_top\":true,\"content\":\"\n\n<p><strong>Geosites and Geotrails<\\\/strong><\\\/p>\"}}]}]}]},{\"type\":\"section\",\"props\":{\"style\":\"default\",\"width\":\"expand\",\"vertical_align\":\"middle\",\"title_position\":\"top-left\",\"title_rotation\":\"left\",\"title_breakpoint\":\"xl\",\"image_position\":\"center-center\"},\"children\":[{\"type\":\"row\",\"props\":{\"layout\":\"3-5,2-5\"},\"children\":[{\"type\":\"column\",\"props\":{\"position_sticky_breakpoint\":\"m\",\"image_position\":\"center-center\",\"media_overlay_gradient\":\"\",\"width_medium\":\"3-5\",\"vertical_align\":\"middle\"},\"children\":[{\"type\":\"headline\",\"props\":{\"title_element\":\"h1\",\"content\":\"\n\n<p><strong><span>WHAT ARE GEOTRAILS?<\\\/span><\\\/strong><\\\/p>\",\"title_color\":\"danger\"}},{\"type\":\"text\",\"props\":{\"margin\":\"default\",\"column_breakpoint\":\"m\",\"content\":\"\"}},{\"type\":\"divider\",\"props\":{\"divider_element\":\"hr\"}},{\"type\":\"text\",\"props\":{\"margin\":\"default\",\"column_breakpoint\":\"m\",\"content\":\"\n\n<p><span>The trail allows the visitor to discover thematically interconnected sites which are complementary to each other, so that the visitor, along the route, learns a coherent history and not an isolated knowledge of each of the sites visited. In this way, the trails are a didactic resource focused on the popularization of geoheritage and a service that enriches the geotourism offer for the benefit of visitors and the local communities in which they are located.<\\\/span><\\\/p>\",\"text_color\":\"secondary\",\"text_align\":\"justify\"}},{\"type\":\"image\",\"props\":{\"margin\":\"default\",\"image_svg_color\":\"emphasis\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Geosenderos-mapa.jpg\"}},{\"type\":\"text\",\"props\":{\"margin\":\"default\",\"column_breakpoint\":\"m\",\"content\":\"\n\n<p><strong>NOTE:<\\\/strong><\\\/p>\\n\n\n<p><span>Tours are conducted in local vehicles with a maximum capacity of 10 people. The maximum number of participants in each tour is 20 people. In all cases, the tours are led by local guides.<\\\/span><\\\/p>\"}}]},{\"type\":\"column\",\"props\":{\"position_sticky_breakpoint\":\"m\",\"image_position\":\"center-center\",\"media_overlay_gradient\":\"\",\"width_medium\":\"2-5\",\"vertical_align\":\"middle\",\"style\":\"secondary\"},\"children\":[{\"type\":\"accordion\",\"props\":{\"show_image\":true,\"show_link\":true,\"collapsible\":true,\"content_column_breakpoint\":\"m\",\"image_svg_color\":\"emphasis\",\"image_align\":\"top\",\"image_grid_width\":\"1-2\",\"image_grid_breakpoint\":\"m\",\"link_text\":\"PDF\",\"link_style\":\"primary\",\"link_target\":true,\"link_margin\":\"small\"},\"children\":[{\"type\":\"accordion_item\",\"props\":{\"title\":\"GT1 - LOS CORAZONES, 30 KM\",\"content\":\"\n\n<p><span>Longest route in the geopark, lithological contacts, lamabordos, plutonic structures, viewpoints.<\\\/span><\\\/p>\",\"link\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Geosendero-Los-Corazones.pdf\"}},{\"type\":\"accordion_item\",\"props\":{\"title\":\"GT2 - LAS CONCHAS, 3 KM\",\"content\":\"\n\n<p><span>Badlands, gullies and erosional cirques in the Yanhuitl\\u00e1n Formation, paleosols and alluvial forms, archaeological ruins.<\\\/span><\\\/p>\",\"link\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Geosendero-Las-Conchas.pdf\"}},{\"type\":\"accordion_item\",\"props\":{\"title\":\"GT3 - CERRO DEL SOL, 3 KM\",\"content\":\"\n\n<p><span>Panoramic views of the Llano de Lobos Tuff, lithological contacts and local faults.<\\\/span><\\\/p>\",\"link\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Geosendero-Cerro-del-Sol.pdf\"}},{\"type\":\"accordion_item\",\"props\":{\"title\":\"GT4 - R\\u00cdO DEL \\u00c1GUILA, 4 KM\",\"content\":\"\n\n<p><span>Lithological contacts, erosional cirques and lamabordo, volcanic lithology.<\\\/span><\\\/p>\",\"link\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Geosendero-Rio-del-Aguila.pdf\"}},{\"type\":\"accordion_item\",\"props\":{\"title\":\"GT5 - YUTOTO\",\"content\":\"\n\n<p><span>Karstic landscapes, lamabordos, limestone quarries, fossils and archaeological remains.<\\\/span><\\\/p>\",\"link\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Geosendero-Yutoto.pdf\"}},{\"type\":\"accordion_item\",\"props\":{\"title\":\"GT6 - EL JAZM\\u00cdN, 4 KM\",\"content\":\"\n\n<p><span>Main archaeological site in the Geopark; alluvial archives, paleosoils and fluvial forms and panoramic views of the Yanhuitl\\u00e1n Valley<\\\/span><\\\/p>\",\"link\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Geosendero-Jazmin.pdf\"}},{\"type\":\"accordion_item\",\"props\":{\"title\":\"GT7 - TEJOCOTAL, 12.5 KM\",\"content\":\"\n\n<p><span>Outcrops of the Llano de Lobos Tuff, lithological contacts, main geological units, viewpoints of the valleys.<\\\/span><\\\/p>\",\"link\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Geosendero-Tejocotal.pdf\"}},{\"type\":\"accordion_item\",\"props\":{\"title\":\"GT8 - SAN PEDRO A\\u00d1A\\u00d1E DYKES, 5 KM\",\"content\":\"\n\n<p><span>Lamabordos, plutonic structures, gullies and badlands.<\\\/span><\\\/p>\",\"link\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Geosendero-Diques-de-San-Pedro-Anane.pdf\"}}]},{\"type\":\"divider\",\"props\":{\"divider_element\":\"hr\"}},{\"type\":\"accordion\",\"props\":{\"show_image\":true,\"show_link\":true,\"collapsible\":true,\"content_column_breakpoint\":\"m\",\"image_svg_color\":\"emphasis\",\"image_align\":\"top\",\"image_grid_width\":\"1-2\",\"image_grid_breakpoint\":\"m\",\"link_text\":\"PDF\",\"link_style\":\"primary\",\"link_target\":true,\"link_margin\":\"small\",\"multiple\":false},\"children\":[{\"type\":\"accordion_item\",\"props\":{\"title\":\"SN1 - CERRO VERDE, 3 KM\",\"content\":\"\n\n<p><span>Route to the highest altitude of the Mixteca Alta, continental watershed, gullies, badlands, plutonic structures and archaeological sites.<\\\/span><\\\/p>\",\"link\":\"\"}},{\"type\":\"accordion_item\",\"props\":{\"title\":\"SN2 - PE\\u00d1A AZUL, 3 KM\",\"content\":\"\n\n<p><span>Panoramic view of the Yanhuitl\\u00e1n, Yucuita and Nochixtl\\u00e1n valleys; main geomorphological units, well-preserved forests and a variety of orchids (in season).<\\\/span><\\\/p>\",\"link\":\"\"}},{\"type\":\"accordion_item\",\"props\":{\"title\":\"SN3 - YUXACINO, 4 KM\",\"content\":\"\n\n<p><span>Alluvial profiles and local faults. Collection of edible insects.<\\\/span><\\\/p>\",\"link\":\"\"}},{\"type\":\"accordion_item\",\"props\":{\"title\":\"SN4 - \\u00d1U'UN YUCU, 4 KM\",\"content\":\"\n\n<p><span>Well-preserved oak forests, panoramic views of the Yanhuitl\\u00e1n Valley, bird watching and a variety of orchids depending on the season.<\\\/span><\\\/p>\",\"link\":\"\"}}]}]}]}]},{\"type\":\"section\",\"props\":{\"style\":\"default\",\"width\":\"xlarge\",\"vertical_align\":\"middle\",\"title_position\":\"top-left\",\"title_rotation\":\"left\",\"title_breakpoint\":\"xl\",\"image_position\":\"top-left\",\"image\":\"\",\"image_width\":\"900\",\"image_effect\":\"parallax\",\"image_parallax_bgy_start\":\"70\",\"image_parallax_bgy_end\":\"120\"},\"children\":[{\"type\":\"row\",\"children\":[{\"type\":\"column\",\"props\":{\"image_position\":\"center-center\",\"media_overlay_gradient\":\"\",\"position_sticky_breakpoint\":\"m\",\"width_medium\":\"1-3\",\"vertical_align\":\"middle\"},\"children\":[{\"type\":\"headline\",\"props\":{\"title_element\":\"h1\",\"content\":\"<strong>Geosites<\\\/strong>\",\"title_color\":\"danger\"}},{\"type\":\"divider\",\"props\":{\"divider_element\":\"hr\"}},{\"type\":\"text\",\"props\":{\"margin\":\"default\",\"column_breakpoint\":\"m\",\"content\":\"\n\n<p><span>Geosites are sites of geological interest representative of the geoheritage of the geopark. There are 35 identified geosites, although others that have been identified are under study.<\\\/span><\\\/p>\",\"text_color\":\"secondary\",\"text_align\":\"justify\"}}]},{\"type\":\"column\",\"props\":{\"position_sticky_breakpoint\":\"m\",\"image_position\":\"center-center\",\"media_overlay_gradient\":\"\",\"width_medium\":\"2-3\",\"vertical_align\":\"middle\"},\"children\":[{\"type\":\"panel-slider\",\"props\":{\"show_title\":true,\"show_meta\":true,\"show_content\":true,\"show_image\":true,\"show_link\":true,\"slider_width\":\"fixed\",\"slider_width_default\":\"1-1\",\"slider_width_medium\":\"1-3\",\"slider_gap\":\"default\",\"slider_autoplay_pause\":false,\"nav\":\"dotnav\",\"nav_align\":\"center\",\"nav_breakpoint\":\"s\",\"slidenav\":\"\",\"slidenav_margin\":\"medium\",\"slidenav_breakpoint\":\"xl\",\"slidenav_outside_breakpoint\":\"xl\",\"panel_card_match\":true,\"title_hover_style\":\"reset\",\"title_element\":\"h3\",\"title_align\":\"top\",\"title_grid_width\":\"1-2\",\"title_grid_breakpoint\":\"m\",\"meta_style\":\"meta\",\"meta_align\":\"below-title\",\"meta_element\":\"div\",\"content_column_breakpoint\":\"m\",\"icon_width\":80,\"image_align\":\"top\",\"image_grid_width\":\"1-2\",\"image_grid_breakpoint\":\"m\",\"image_svg_color\":\"emphasis\",\"link_text\":\"Read more\",\"link_style\":\"default\",\"margin\":\"default\",\"slider_autoplay\":true,\"slider_autoplay_interval\":\"4\",\"slider_width_large\":\"3-5\",\"slidenav_large\":true},\"children\":[{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Mirador de los dos corazones\",\"content\":\"\n\n<p><span>Mass removal processes, erosive cirques, gullies and lamabordos.<\\\/span><\\\/p>\\n\n\n<p><span>\\u00a0<\\\/span><\\\/p>\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Mirador-los-dos-corazones.jpg\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\" Sta. Mar\\u00eda Pozoltepec viewpoint\",\"content\":\"\n\n<p><span>Lithological contours of main units: Yanhuitl\\u00e1n- Toba Llano de lobos Formation.<\\\/span><\\\/p>\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Mirador-Sta.-Maria-Pozoltepec.jpg\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Sta. Mar\\u00eda Pozoltepec Waterfall\",\"content\":\"\n\n<p><span>Dikes, contact metamorphism, structural control of rivers.<\\\/span><\\\/p>\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Cascada-Sta.-Maria-Pozoltepec.jpg\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Vista Hermosa Viewpoint\",\"content\":\"\n\n<p><span>Badlands, dykes, contact between physiographic provinces.<\\\/span><\\\/p>\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Mirador-vista-hermosa.jpg\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Andesite Yucudaac\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Andesita-Yucudaac.jpg\",\"content\":\"\n\n<p><span>Exfoliation, spheroidal weathering.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Yucuita landslides\",\"content\":\"\n\n<p><span>Processes of mass removal, landslides and lamabordos.<\\\/span><\\\/p>\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Deslizamientos-Yucuita.jpg\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Nochixtl\\u00e1n and Yanhuitl\\u00e1n valleys viewpoint.\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Mirador-de-los-valles-de-Nochixtlan-y-Yanhuitlan.jpg\",\"content\":\"\n\n<p><span>Gullies, badlands, regional faults and lamabordos systems.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Yanhuitl\\u00e1n River\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Rio-Yanhuitlan.jpg\",\"content\":\"\n\n<p><span>Alluvial files and paleosoils.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Sitio-Las-Conchas.jpg\",\"content\":\"\n\n<p><span>Landslide processes, erosional cirques, gullies and lamabordos.<\\\/span><\\\/p>\",\"title\":\"Las Conchas Site\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Las Conchas viewpoint\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Mirador-Las-Conchas.jpg\",\"content\":\"\n\n<p><span>Gullies, badlands, regional faults, exocarstic features and lamabordos systems.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Pe\\u00f1a Azul Prisms\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Prismas-de-Pena-azul.jpg\",\"content\":\"\n\n<p><span>Lava structures, waterfalls.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"San Pedro A\\u00f1a\\u00f1e dykes\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/12-Diques-de-San-Pedro-Anane.jpg\",\"content\":\"\n\n<p><span>Dikes and sill, differential erosion, gullies, badlands, regional faults and lamabordos systems.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Yanhuitl\\u00e1n river alluvial archives.\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Archivos-aluviales-del-rio-Yanhuitlan.jpg\",\"content\":\"\n\n<p><span>Alluvial archives, paleosoils and lamabordos.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"R\\u00edo Verde Site\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Sitio-Rio-Verde.jpg\",\"content\":\"\n\n<p><span>Lithological contacts of main units, tectonics, regional faults.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Yanhuitl\\u00e1n Valley Viewpoint\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Mirador-Valle-de-Yanhuitlan.jpg\",\"content\":\"\n\n<p><span>Landslide processes, erosional cirques, gullies and badlands, lamabordos systems.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Yudayo Site\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Sitio-Yudayo.jpg\",\"content\":\"\n\n<p><span>Eroded lamabordos and alluvial deposits.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"San Isidro and Suchixtlahuaca Site\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Sitio-San-Isidro-y-Suchixtlahuaca.jpg\",\"content\":\"\n\n<p><span>Lithological contacts of main units and intrusive bodies.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Boquer\\u00f3n Site\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Sitio-Boqueron.jpg\",\"content\":\"\n\n<p><span>Landslide processes, erosional cirques, gullies and lamabordos.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\" Yuxacino Site\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Sitio-Yuxacino.jpg\",\"content\":\"\n\n<p><span>Paleontology (mammoths), alluvial deposits.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\" Tonaltepec Viewpoint\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Mirador-Tonaltepec.jpg\",\"content\":\"\n\n<p><span>Gullies, badlands, regional faults and lamabordos systems.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Cerro del Sol (Yucunchi)\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Cerro-del-Sol-Yucunchi.jpg\",\"content\":\"\n\n<p><span>Lithological contacts of main units, tectonism, regional faults.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Cerro Verde\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Cerro-Verde.jpg\",\"content\":\"\n\n<p><span>Continental watershed.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Dequenini Site\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Sitio-Dequenini.jpg\",\"content\":\"\n\n<p><span>Lithological contacts of main units.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Eagle River\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Rio-del-Aguila.jpg\",\"content\":\"\n\n<p><span>Lithological contacts of main units, fluvial forms and tectonism.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Yutzateche river\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Rio-Yutzateche.jpg\",\"content\":\"\n\n<p><span>Lithologic contacts, base of the stratigraphic column (Cretaceous-Paleogene).<\\\/span><\\\/p>\\n\n\n<p><span>\\u00a0<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Yutoto site\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Sitio-Yutoto.jpg\",\"content\":\"\n\n<p><span>Endo- and exocarstic features and fluvial features.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Guadalupe Gavillera Agency Site\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Sitio-Agencia-Guadalupe-Gavillera.jpg\",\"content\":\"\n\n<p><span>Karstic features: lapiaz, caves, Cretaceous fossils.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Limestone quarry\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Cantera-de-calizas.jpg\",\"content\":\"\n\n<p><span>Limestones.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"San Isidro Tejocotal viewpoint.\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Mirador-San-Isidro-Tejocotal.jpg\",\"content\":\"\n\n<p><span>Main geomorphological units of the geopark.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Teposcolula Limestone Quarry\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Cantera-Caliza-Teposcolula.jpg\",\"content\":\"\n\n<p><span>Abandoned quarry, limestone blocks.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"La Laguna site\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Sitio-La-Laguna.jpg\",\"content\":\"\n\n<p><span>Karstic features: lapiaz, caves, terra rossa.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Yutzateche site\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Sitio-La-Laguna.jpg\",\"content\":\"\n\n<p><span>Lava structures.<\\\/span><\\\/p>\\n\n\n<p><span>\\u00a0<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Yucudaac site\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Sitio-Yucudaac.jpg\",\"content\":\"\n\n<p><span>Exfoliation, spheroidal weathering.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\" Cerro Corneta site\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Sitio-Cerro-Corneta.jpg\",\"content\":\"\n\n<p><span>Mass removal processes, erosive cirques, gullies and lamabordos.<\\\/span><\\\/p>\"}},{\"type\":\"panel-slider_item\",\"props\":{\"title\":\"Caballo Blanco site\",\"image\":\"wp-content\\\/uploads\\\/2022\\\/04\\\/Sitio-Caballo-Blanco.jpg\",\"content\":\"\n\n<p><span>Mass removal processes, erosive cirques, gullies and lamabordos.<\\\/span><\\\/p>\"}}]}]}],\"props\":{\"layout\":\"1-3,2-3\"}}],\"name\":\"Post\"}],\"version\":\"2.7.22\"} --><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Geosites and Geotrails WHAT ARE GEOTRAILS? The trail allows the visitor to discover thematically interconnected sites which are complementary to each other, so that the visitor, along the route, learns a coherent history and not an isolated knowledge of each of the sites visited. In this way, the trails are a didactic resource focused on [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_acf_changed":false,"om_disable_all_campaigns":false,"_monsterinsights_skip_tracking":false,"_monsterinsights_sitenote_active":false,"_monsterinsights_sitenote_note":"","_monsterinsights_sitenote_category":0,"_uf_show_specific_survey":0,"_uf_disable_surveys":false,"footnotes":""},"class_list":["post-1517","page","type-page","status-publish","hentry"],"acf":[],"aioseo_notices":[],"_links":{"self":[{"href":"https:\/\/geoparquemixtecaalta.org\/en\/wp-json\/wp\/v2\/pages\/1517","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/geoparquemixtecaalta.org\/en\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/geoparquemixtecaalta.org\/en\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/geoparquemixtecaalta.org\/en\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/geoparquemixtecaalta.org\/en\/wp-json\/wp\/v2\/comments?post=1517"}],"version-history":[{"count":226,"href":"https:\/\/geoparquemixtecaalta.org\/en\/wp-json\/wp\/v2\/pages\/1517\/revisions"}],"predecessor-version":[{"id":2589,"href":"https:\/\/geoparquemixtecaalta.org\/en\/wp-json\/wp\/v2\/pages\/1517\/revisions\/2589"}],"wp:attachment":[{"href":"https:\/\/geoparquemixtecaalta.org\/en\/wp-json\/wp\/v2\/media?parent=1517"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}