{"id":25502,"date":"2025-01-30T13:09:18","date_gmt":"2025-01-30T16:09:18","guid":{"rendered":"http:\/\/gabrielpaladino.com\/?p=25502"},"modified":"2025-09-15T12:08:56","modified_gmt":"2025-09-15T15:08:56","slug":"textures-of-time","status":"publish","type":"post","link":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/2025\/01\/30\/textures-of-time\/","title":{"rendered":"Textures of Time"},"content":{"rendered":"<div><img decoding=\"async\" src=\"https:\/\/live.staticflickr.com\/65535\/54296708651_18138dbad7_k.jpg\" \/>\n<p>Caliche, a type of sedimentary rock, forms when calcium carbonate precipitates in the soil, especially in arid and semi-arid areas. This formation process begins as rainwater infiltrates the soil, dissolving carbonate minerals present. As the water evaporates, these minerals precipitate, cementing particles such as sand, clay, and gravel to create a hard, durable layer.<\/p>\n<p>In Ajuy, particularly near the Hornos de Cal, caliche is significantly prominent. These formations result from the interplay of local climatic and geological conditions. Despite its hardness, caliche is prone to erosion. Elements like wind, water, and human activity wear down these layers, forming unique patterns and textures and sometimes exposing softer soil underneath.<\/p>\n<p>The caliche in Ajuy ranges in color from white to light brown, contrasting sharply with the dark basaltic rocks and black sands of the nearby beaches. These layers can also create microhabitats, providing shelter to small organisms and aiding in soil moisture retention, crucial in Fuerteventura&#8217;s arid environment.<\/p>\n<p>Erosion of the caliche near the path to the Cuevas de Ajuy, especially around the Hornos de Cal area, is a continuous process that enhances the unique landscape and reveals the area&#8217;s rich geological history.<\/p>\n<p>&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;&#8212;-<\/p>\n<p><b>Versi\u00f3n en Espa\u00f1ol<\/b><\/p>\n<p>El caliche es una roca sedimentaria que se forma por la precipitaci\u00f3n de carbonato de calcio en el suelo, especialmente en regiones \u00e1ridas y semi\u00e1ridas. Este proceso comienza cuando el agua de lluvia se infiltra en el suelo y disuelve los minerales carbonatados presentes. A medida que el agua se evapora, los minerales se precipitan y cementan part\u00edculas como arena, arcilla y grava, creando una capa dura y resistente.<\/p>\n<p>En Ajuy, cerca de los Hornos de Cal, el caliche se presenta de manera notable. Estas formaciones son resultado de la combinaci\u00f3n de las condiciones clim\u00e1ticas y geol\u00f3gicas locales. A pesar de ser una roca dura, el caliche es susceptible a la erosi\u00f3n. Los agentes erosivos como el viento, el agua y la acci\u00f3n humana desgastan estas formaciones, creando patrones y texturas \u00fanicos y, en algunos casos, exponiendo secciones del suelo m\u00e1s blando.<\/p>\n<p>El caliche en Ajuy var\u00eda en color desde el blanco al marr\u00f3n claro, contrastando con las rocas bas\u00e1lticas oscuras y la arena negra de las playas cercanas. Estas capas de caliche tambi\u00e9n pueden servir como microh\u00e1bitats, proporcionando refugio a peque\u00f1os organismos y ayudando a retener la humedad en el suelo, lo cual es crucial en el entorno \u00e1rido de Fuerteventura.<\/p>\n<p>La erosi\u00f3n del caliche cerca del sendero a las Cuevas de Ajuy, particularmente en la zona de los Hornos de Cal, es un proceso continuo que a\u00f1ade al paisaje su car\u00e1cter \u00fanico y revela la rica historia geol\u00f3gica de la regi\u00f3n.<\/p>\n<p><b>Ajuy, Parque Rural de Betancuria, Fuerteventura, Islas Canarias<\/b><\/p>\n<p>Photo Taken: April 14, 2023<\/p>\n<p><a href=\"https:\/\/flic.kr\/p\/2qJ1PPa\">High resolution<\/a><br \/><a href=\"https:\/\/www.flickr.com\/photos\/gabouruguay-collection\/\">Flickr Gallery<\/a><\/p>\n<\/div>\n<p><b>Did you like this post?<\/b><\/p>\n\n","protected":false},"excerpt":{"rendered":"<p>Caliche, a type of sedimentary rock, forms when calcium carbonate precipitates in the soil, especially in arid and semi-arid areas. This formation process begins as rainwater infiltrates the soil, dissolving carbonate minerals present. As the water evaporates, these minerals precipitate, cementing particles such as sand, clay, and gravel to create a hard, durable layer. In [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"advanced_seo_description":"","jetpack_seo_html_title":"","jetpack_seo_noindex":false,"jetpack_seo_schema_type":"","_jetpack_newsletter_access":"","_jetpack_dont_email_post_to_subs":false,"_jetpack_newsletter_tier_id":0,"_jetpack_memberships_contains_paywalled_content":false,"_jetpack_feature_clip_id":0,"_jetpack_memberships_contains_paid_content":false,"footnotes":"","jetpack_post_was_ever_published":false},"categories":[2],"tags":[16,264,366,866,940,941,2200,2208,2309,2311,2327,2380,2388,3163,3166,3167,3196,3760,4634,4670,5092,5188,5189,5289,5355,5356,5576,5578,6425,1271,6567,6731,6742,6749,6750,6755,6985,7297,7386,7564,7565,7798,8362,8363,8555,8863,8867,8869,8871,9539,9883,9744,11832,11833,12145,12268,12621,12966,12968,12991,13217,13286,13339,13467,14768,13795],"class_list":["post-25502","post","type-post","status-publish","format-standard","hentry","category-related-posts","tag-travel","tag-africa","tag-ajuy","tag-archipielago","tag-arid","tag-arido","tag-caliche","tag-calizo","tag-canaria","tag-canarias","tag-canaryislands","tag-canon","tag-capas","tag-cliffs","tag-clima","tag-climate","tag-coast","tag-cuevasdeajuy","tag-erosion","tag-espana","tag-flickr","tag-formacion","tag-formation","tag-fuerteventura","tag-gabrielpaladinocom","tag-gabrielpaladinoibanez","tag-geologia","tag-geology","tag-hornosdecal","tag-ilescanaries","tag-ilhascanarias","tag-isla","tag-island","tag-islascanarias","tag-islascanarias2023","tag-isolecanarie","tag-kanarischeinseln","tag-landscape","tag-layers","tag-limekilns","tag-limestone","tag-macaronesia","tag-minerales","tag-minerals","tag-monumentonaturaldeajuy","tag-natural","tag-naturaleza","tag-naturalezas","tag-nature","tag-paisaje","tag-pajara","tag-parqueruraldebetancuria","tag-sedimentaria","tag-sedimentary","tag-soil","tag-spain","tag-suelo","tag-texturas","tag-textures","tag-thecanaries","tag-tourism","tag-travelling","tag-trip","tag-turismo","tag-updated","tag-viaje","has-post-thumbnail"],"tags_input":"#travel,Africa,ajuy,archipi\u00e9lago,arid,arido,caliche,calizo,canaria,canarias,canaryislands,canon,capas,cliffs,clima,climate,coast,cuevasdeajuy,erosion,espa\u00f1a,Flickr,formacion,formation,fuerteventura,gabrielpaladinocom,gabrielpaladinoiba\u00f1ez,geologia,geology,hornosdecal,\u00eelescanaries,ilhascan\u00e1rias,isla,island,islascanarias,IslasCanarias2023,isolecanarie,kanarischeinseln,landscape,layers,limekilns,limestone,macaronesia,minerales,minerals,monumentonaturaldeajuy,natural,naturaleza,naturalezas,nature,paisaje,p\u00e1jara,parqueruraldebetancuria,sedimentaria,sedimentary,soil,spain,suelo,texturas,textures,thecanaries,tourism,travelling,trip,turismo,Updated,viaje","jetpack_shortlink":"https:\/\/wp.me\/phjlBv-6Dk","jetpack_sharing_enabled":true,"jetpack_likes_enabled":true,"jetpack-related-posts":[{"id":33743,"url":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/2025\/08\/13\/fossil-dunes\/","url_meta":{"origin":25502,"position":0},"title":"Fossil dunes","author":"Gabriel Paladino Ib\u00e1\u00f1ez","date":"August 13, 2025","format":false,"excerpt":"The Ajuy's Fossil Dunes stand as a striking testament to Fuerteventura's deep geological past. Situated along the path leading to the famous caves, these magnificent sand walls are not ordinary rock formations. They are a specific type of sedimentary rock known as calcarenite, formed during the Pliocene epoch, approximately 2\u2026","rel":"","context":"In &quot;Related posts&quot;","block_context":{"text":"Related posts","link":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/category\/related-posts\/"},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":7400,"url":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/2020\/11\/14\/eriosyce-napina-glabrescens\/","url_meta":{"origin":25502,"position":1},"title":"Eriosyce napina ssp. glabrescens","author":"Gabriel Paladino Ib\u00e1\u00f1ez","date":"November 14, 2020","format":false,"excerpt":"Origin and Habitat: From coastal Chile (Region III Atacama) South of Freirina in the Huasco valley (Atacama Desert) Scientific classification: Kingdom: Plantae Subkingdom: Tracheobionta Division: Magnoliophyta Class: Magnoliopsida Subclass: caryophyllidae Order: Caryophyllales Family: Cactaceae Subfamily: Cactoideae Tribe: Cacteae Genre: Eriosyce Habitat: Eriosyce napina grows in one of the most arid\u2026","rel":"","context":"In &quot;Related posts&quot;","block_context":{"text":"Related posts","link":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/category\/related-posts\/"},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":7819,"url":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/2021\/01\/16\/eriosyce-napina-glabrescens-rain\/","url_meta":{"origin":25502,"position":2},"title":"Eriosyce napina ssp. glabrescens","author":"Gabriel Paladino Ib\u00e1\u00f1ez","date":"January 16, 2021","format":false,"excerpt":"Origin and Habitat: From coastal Chile (Region III Atacama) South of Freirina in the Huasco valley (Atacama Desert) Scientific classification: Kingdom: Plantae Subkingdom: Tracheobionta Division: Magnoliophyta Class: Magnoliopsida Subclass: caryophyllidae Order: Caryophyllales Family: Cactaceae Subfamily: Cactoideae Tribe: Cacteae Genre: Eriosyce Habitat: Eriosyce napina grows in one of the most arid\u2026","rel":"","context":"In &quot;Related posts&quot;","block_context":{"text":"Related posts","link":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/category\/related-posts\/"},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":25419,"url":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/2025\/01\/25\/dracaena-draco\/","url_meta":{"origin":25502,"position":3},"title":"Dracaena draco","author":"Gabriel Paladino Ib\u00e1\u00f1ez","date":"January 25, 2025","format":false,"excerpt":"Dracaena draco, also known as the Dragon Tree, is a truly remarkable plant native to the Canary Islands and nearby regions. With its thick trunk, spiky leaves, and umbrella-like canopy, this tree is easily recognizable. One of its most fascinating features is the red resin it produces, famously referred to\u2026","rel":"","context":"In &quot;Related posts&quot;","block_context":{"text":"Related posts","link":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/category\/related-posts\/"},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":22095,"url":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/2024\/02\/11\/montana-sagrada-de-tindaya\/","url_meta":{"origin":25502,"position":4},"title":"Monta\u00f1a Sagrada de Tindaya","author":"Gabriel Paladino Ib\u00e1\u00f1ez","date":"February 11, 2024","format":false,"excerpt":"The mountain of Tindaya is located in the northwest of Fuerteventura, very close to La Oliva. The ancient aborigines of Fuerteventura considered Tindaya a sacred mountain to which magical properties were attributed, as attested by more than 300 foot-shaped engravings of great archaeological value, which have been found on it.\u2026","rel":"","context":"In &quot;Related posts&quot;","block_context":{"text":"Related posts","link":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/category\/related-posts\/"},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]},{"id":22325,"url":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/2024\/03\/07\/blacksandbeach\/","url_meta":{"origin":25502,"position":5},"title":"B L A C K S A N D","author":"Gabriel Paladino Ib\u00e1\u00f1ez","date":"March 7, 2024","format":false,"excerpt":"Ajuy beach boasts black sand due to its volcanic composition. This unique feature can be attributed to the formation of the island of Fuerteventura, which occurred millions of years ago through the combination of lava and sediment. The coarse texture and dark hue of the sand give it a distinct\u2026","rel":"","context":"In &quot;Related posts&quot;","block_context":{"text":"Related posts","link":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/category\/related-posts\/"},"img":{"alt_text":"","src":"","width":0,"height":0},"classes":[]}],"jetpack_featured_media_url":"","_links":{"self":[{"href":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/wp-json\/wp\/v2\/posts\/25502","targetHints":{"allow":["GET"]}}],"collection":[{"href":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/wp-json\/wp\/v2\/comments?post=25502"}],"version-history":[{"count":1,"href":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/wp-json\/wp\/v2\/posts\/25502\/revisions"}],"predecessor-version":[{"id":34348,"href":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/wp-json\/wp\/v2\/posts\/25502\/revisions\/34348"}],"wp:attachment":[{"href":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/wp-json\/wp\/v2\/media?parent=25502"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/wp-json\/wp\/v2\/categories?post=25502"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/pelecyphora.ddns.net:60123\/GabrielPaladino.com\/wp-json\/wp\/v2\/tags?post=25502"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}