ds-suit domain was triggered too early. This is usually an indicator for some code in the plugin or theme running too early. Translations should be loaded at the init action or later. Please see Debugging in WordPress for more information. (This message was added in version 6.7.0.) in /home1/cuellars/public_html/wp-includes/functions.php on line 6131gotmls domain was triggered too early. This is usually an indicator for some code in the plugin or theme running too early. Translations should be loaded at the init action or later. Please see Debugging in WordPress for more information. (This message was added in version 6.7.0.) in /home1/cuellars/public_html/wp-includes/functions.php on line 6131Limestone is born on tropical seabed and its sea coasts, as a build-up of fragmented, microscopic and dissolved seashells \u2013 mineral calcite \u2013 and sometimes with clay layers or lenses of sand.<\/p>\n
The tropical shoals from which limestone is raised aren\u2019t indefinitely motionless: the bottom of the ocean slowly moves, slipping underneath the continental plates, gradually reorganizing the world map.<\/p>\n
When this movement takes place, it drives the limestone bed into earth\u2019s crust and high temperatures are achieved, causing calcite grains fusion. This is a dynamic process that buries, twists and pushes the rock layers. In this phase, rock doesn\u2019t melt, but gets flexible, just like a chocolate bar in summer. This process is responsible for the trademark veins of marble.<\/p>\n
A Marble piece is the result of its birth, growth and long way of life. We collect it marked with its \u2018scars\u2019, a product of the Nature with unique personality and which irradiates a strong energy, endowing the ambiences with an incomparable character.<\/p>","protected":false},"excerpt":{"rendered":"
La caliza nace en los lechos marinos tropicales y sus costas, como una acumulaci\u00f3n de conchas fragmentadas, microsc\u00f3picas y disueltas \u2013 calcita mineral – \u00a0y en ocasiones con capas de arcilla o cristales de arena. Los bancos tropicales que originan la caliza no se quedan inm\u00f3viles indefinidamente: el fondo del oc\u00e9ano se mueve lentamente, desliz\u00e1ndose […]<\/p>","protected":false},"author":3,"featured_media":2013,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"_et_pb_use_builder":"","_et_pb_old_content":"","_et_gb_content_width":"","pgc_sgb_lightbox_settings":"","footnotes":""},"categories":[183],"tags":[185,186,184],"class_list":["post-2011","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-sabiasque","tag-caliza","tag-lechos-marinos","tag-marmol"],"acf":[],"yoast_head":"\n