{"id":6259,"date":"2026-05-08T16:53:57","date_gmt":"2026-05-08T14:53:57","guid":{"rendered":"https:\/\/laboratorio.geolag.com\/eastern-coast-of-asturias\/"},"modified":"2026-06-25T18:27:53","modified_gmt":"2026-06-25T16:27:53","slug":"eastern-coast-of-asturias","status":"publish","type":"post","link":"https:\/\/geolag.com\/en\/eastern-coast-of-asturias\/","title":{"rendered":"Eastern coast of Asturias"},"content":{"rendered":"\n<p class=\"wp-block-paragraph\">The uniqueness of this stretch of coastline lies in the limestone nature of the rocks that make it up and in the complex geological history this part of the Earth\u2019s crust has undergone. On the one hand, karst dissolution processes have shaped a landscape on the surface made up of dolines (depressions) and cuetos (limestone rises). The karst within the rock massif is expressed by numerous underground conduits that form a complex network of galleries and vertical shafts. The rises and falls in sea level linked to glaciations and to the tectonic processes associated with the formation and erosion of the Cantabrian Mountains have generated large flattened surfaces (coastal platforms) that make up the so-called \u201cflat-topped ridges\u201d that dominate the higher areas of this region. These sea-level changes, in turn, have contributed to the connection of some shafts with sea level, forming cenotes, tidal dolines and blowholes\u2014karst-marine landforms that, during sea storms, can expel columns of seawater to more than 50 m in height.    <\/p>\n\n<figure class=\"wp-block-gallery has-nested-images columns-default is-cropped wp-block-gallery-1 is-layout-flex wp-block-gallery-is-layout-flex\">\n<figure class=\"wp-block-image size-large\"><img fetchpriority=\"high\" decoding=\"async\" width=\"1024\" height=\"652\" data-id=\"1356\" src=\"https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/castiello-1024x652.avif\" alt=\"\" class=\"wp-image-1356\" srcset=\"https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/castiello-1024x652.avif 1024w, https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/castiello-300x191.avif 300w, https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/castiello-768x489.avif 768w, https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/castiello-1536x977.avif 1536w, https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/castiello-2048x1303.avif 2048w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n\n\n\n<figure class=\"wp-block-image size-large\"><img decoding=\"async\" width=\"960\" height=\"640\" data-id=\"1357\" src=\"https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/cuevas_mar.avif\" alt=\"\" class=\"wp-image-1357\" srcset=\"https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/cuevas_mar.avif 960w, https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/cuevas_mar-300x200.avif 300w, https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/cuevas_mar-768x512.avif 768w\" sizes=\"(max-width: 960px) 100vw, 960px\" \/><\/figure>\n\n\n\n<figure class=\"wp-block-image size-large\"><img decoding=\"async\" width=\"960\" height=\"400\" data-id=\"918\" src=\"https:\/\/geolag.com\/wp-content\/uploads\/2014\/09\/olianco.avif\" alt=\"\" class=\"wp-image-918\" srcset=\"https:\/\/geolag.com\/wp-content\/uploads\/2014\/09\/olianco.avif 960w, https:\/\/geolag.com\/wp-content\/uploads\/2014\/09\/olianco-300x125.avif 300w, https:\/\/geolag.com\/wp-content\/uploads\/2014\/09\/olianco-768x320.avif 768w\" sizes=\"(max-width: 960px) 100vw, 960px\" \/><\/figure>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"960\" height=\"400\" data-id=\"912\" src=\"https:\/\/geolag.com\/wp-content\/uploads\/2014\/09\/buelna.avif\" alt=\"\" class=\"wp-image-912\" srcset=\"https:\/\/geolag.com\/wp-content\/uploads\/2014\/09\/buelna.avif 960w, https:\/\/geolag.com\/wp-content\/uploads\/2014\/09\/buelna-300x125.avif 300w, https:\/\/geolag.com\/wp-content\/uploads\/2014\/09\/buelna-768x320.avif 768w\" sizes=\"(max-width: 960px) 100vw, 960px\" \/><\/figure>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"768\" data-id=\"1039\" src=\"https:\/\/geolag.com\/wp-content\/uploads\/2013\/11\/IMG_4650-1024x768.avif\" alt=\"\" class=\"wp-image-1039\" srcset=\"https:\/\/geolag.com\/wp-content\/uploads\/2013\/11\/IMG_4650-1024x768.avif 1024w, https:\/\/geolag.com\/wp-content\/uploads\/2013\/11\/IMG_4650-300x225.avif 300w, https:\/\/geolag.com\/wp-content\/uploads\/2013\/11\/IMG_4650-768x576.avif 768w, https:\/\/geolag.com\/wp-content\/uploads\/2013\/11\/IMG_4650-1536x1152.avif 1536w, https:\/\/geolag.com\/wp-content\/uploads\/2013\/11\/IMG_4650-2048x1536.avif 2048w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"960\" height=\"640\" data-id=\"1121\" src=\"https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/pimiango_mendia_2.avif\" alt=\"\" class=\"wp-image-1121\" srcset=\"https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/pimiango_mendia_2.avif 960w, https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/pimiango_mendia_2-300x200.avif 300w, https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/pimiango_mendia_2-768x512.avif 768w\" sizes=\"(max-width: 960px) 100vw, 960px\" \/><\/figure>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"900\" height=\"598\" data-id=\"1365\" src=\"https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/pano_gulpiyuri.avif\" alt=\"\" class=\"wp-image-1365\" srcset=\"https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/pano_gulpiyuri.avif 900w, https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/pano_gulpiyuri-300x199.avif 300w, https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/pano_gulpiyuri-768x510.avif 768w\" sizes=\"(max-width: 900px) 100vw, 900px\" \/><\/figure>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"683\" data-id=\"1366\" src=\"https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/IMG_4594-1024x683.avif\" alt=\"\" class=\"wp-image-1366\" srcset=\"https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/IMG_4594-1024x683.avif 1024w, https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/IMG_4594-300x200.avif 300w, https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/IMG_4594-768x512.avif 768w, https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/IMG_4594-1536x1024.avif 1536w, https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/IMG_4594-2048x1365.avif 2048w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"683\" data-id=\"1367\" src=\"https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/IMG_5764-1024x683.avif\" alt=\"\" class=\"wp-image-1367\" srcset=\"https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/IMG_5764-1024x683.avif 1024w, https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/IMG_5764-300x200.avif 300w, https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/IMG_5764-768x512.avif 768w, https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/IMG_5764-1536x1024.avif 1536w, https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/IMG_5764-2048x1365.avif 2048w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n\n\n\n<figure class=\"wp-block-image size-large\"><img loading=\"lazy\" decoding=\"async\" width=\"1024\" height=\"408\" data-id=\"1368\" src=\"https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/panorama_andrin_ballota-1024x408.avif\" alt=\"\" class=\"wp-image-1368\" srcset=\"https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/panorama_andrin_ballota-1024x408.avif 1024w, https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/panorama_andrin_ballota-300x120.avif 300w, https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/panorama_andrin_ballota-768x306.avif 768w, https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/panorama_andrin_ballota-1536x612.avif 1536w, https:\/\/geolag.com\/wp-content\/uploads\/2012\/08\/panorama_andrin_ballota-2048x816.avif 2048w\" sizes=\"(max-width: 1024px) 100vw, 1024px\" \/><\/figure>\n<\/figure>\n\n<p class=\"wp-block-paragraph\">The presence of caves, the mild climate of the coastal areas and the presence of the sea as a food source have been factors that favoured the occupation of this part of the coastline by prehistoric people. Remains of tools and implements, cave paintings and shell middens (accumulations of shell remains at the entrance to some caves) are some of the elements we can find on the eastern Asturian coast. In more recent times, human use of the environment is evident in the abundance of remains of lime kilns (limestone calcination kilns where lime is produced), tileworks that take advantage of areas where clays are concentrated, utensils for collecting seaweed, and even mills and shellfish nurseries found inside some karst-marine landforms such as certain tidal dolines.  <\/p>\n\n<p class=\"wp-block-paragraph\">We offer you different routes through the municipalities of Ribadesella, Llanes and Ribadedeva, where coastal karst is the main attraction.<\/p>\n\n<p class=\"wp-block-paragraph\"><strong>Would you like to discover this landscape with a geologist?<\/strong><br\/><strong><span style=\"color: #a6b500;\">GEO<\/span>LAG<\/strong> organises educational routes adapted for families, groups and educational centres.<br\/><strong><a href=\"https:\/\/geolag.com\/en\/contact\/\" title=\"Contact\">Request information about this route<\/a><\/strong><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Explore the eastern coast of Asturias: a paradise of blowholes and flat-topped ridges between Ribadesella, Llanes and Ribadedeva. Discover its karst magic and prehistoric traces. The east will captivate you!  <\/p>\n","protected":false},"author":1,"featured_media":6143,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[77,79,83],"tags":[],"class_list":["post-6259","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-guided-routes-asturias","category-guided-routes","category-asturias"],"aioseo_notices":[],"aioseo_head":"\n\t\t<!-- All in One SEO 4.9.9 - aioseo.com -->\n\t<meta name=\"description\" content=\"Eastern coast: A paradise of blowholes and flat-topped ridges. 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