{"id":5396,"date":"2020-10-08T15:20:24","date_gmt":"2020-10-08T15:20:24","guid":{"rendered":"https:\/\/joycecountrygeoparkproject.ie\/?p=5396"},"modified":"2020-10-08T15:23:49","modified_gmt":"2020-10-08T15:23:49","slug":"the-last-300-million-years-after-the-carboniferous","status":"publish","type":"post","link":"https:\/\/joycecountrygeoparkproject.ie\/en\/geological-stories\/the-last-300-million-years-after-the-carboniferous\/","title":{"rendered":"The Last 300 Million years \u2013 After the Carboniferous"},"content":{"rendered":"<div class=\"wpb-content-wrapper\"><section class=\"vc_section vc_custom_1602034973827\"><section class=\"vc_row wpb_row vc_row-fluid vc_custom_1602019536803 liquid-row-shadowbox-69d52af84beb1\"><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-12 liquid-column-69d52af84bff8\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"   ><div class=\"wpb_wrapper-inner\">\n\t<div class=\"wpb_text_column wpb_content_element\" >\n\t\t<div class=\"wpb_wrapper\">\n\t\t\t<h4 style=\"text-align: center;\"><span style=\"color: #00656a;\"><strong>250 Million Years Ago<\/strong><\/span><\/h4>\n<h1 style=\"text-align: center;\"><strong>The Last 300 Million Years \u2013 After the Carboniferous<\/strong><\/h1>\n\n\t\t<\/div>\n\t<\/div>\n<\/div><\/div><\/div><\/div><\/div><\/div><\/section><section class=\"vc_row wpb_row vc_row-fluid vc_custom_1602035061065 row-contains-padding-top row-contains-padding-bottom liquid-row-shadowbox-69d52af84c120\"><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-3\/5 liquid-column-69d52af84c200\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"   ><div class=\"wpb_wrapper-inner\">\n\t<div class=\"wpb_text_column wpb_content_element\" >\n\t\t<div class=\"wpb_wrapper\">\n\t\t\t<p>There are no rock records in our geopark region for the following 250 million years. We know from other parts of Ireland that the landmass continued to move north, after colliding with another landmass to its south, which prompted some deformation of the bedrock and an uplift of most of the Irish landmass to a level higher than the sea-level at\u00a0 that time. As most sediments tend to settle and accumulate in basins, such as the seabed, the uplift of the Irish landmass above the sea-level meant that hardly any sediments were deposited in Ireland during these 250 million years.<\/p>\n<p>Tectonically speaking, the next major event recorded in the geopark area was the opening of the <strong>Atlantic<\/strong> Ocean about 65 million years ago, at the end of the <strong>Cretaceous<\/strong> and the start of the <strong>Palaeogene<\/strong> <strong>Period<\/strong>. This started with the thinning of the continental crust followed by the opening of rifts.<\/p>\n\n\t\t<\/div>\n\t<\/div>\n<\/div><\/div><\/div><\/div><div class=\"wpb_column vc_column_container vc_col-sm-2\/5 liquid-column-69d52af84c329\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"   ><div class=\"wpb_wrapper-inner\">\n\t<div  class=\"wpb_single_image wpb_content_element vc_align_center  liquid_vc_single_image-69d52af85e0ea\">\n\t\t\n\t\t<figure class=\"wpb_wrapper vc_figure\">\n\t\t\t<a data-rel=\"prettyPhoto[rel-5396-1649424447]\" href=\"https:\/\/joycecountrygeoparkproject.ie\/wp-content\/uploads\/2020\/10\/View-NE-from-top-of-Droim-Chagaidh-1024x683.jpg\" target=\"_self\" class=\"vc_single_image-wrapper   vc_box_border_grey prettyphoto\"><img loading=\"lazy\" decoding=\"async\" width=\"2560\" height=\"1707\" src=\"data:image\/svg+xml;charset=utf-8,&lt;svg xmlns%3D&#039;http%3A%2F%2Fwww.w3.org%2F2000%2Fsvg&#039; viewBox%3D&#039;0 0 2560 1707&#039;%2F&gt;\" class=\"vc_single_image-img attachment-full ld-lazyload\" alt=\"\" title=\"View NE from top of Droim Chagaidh\" srcset=\"\" sizes=\"auto, (max-width: 2560px) 100vw, 2560px\" data-src=\"https:\/\/joycecountrygeoparkproject.ie\/wp-content\/uploads\/2020\/10\/View-NE-from-top-of-Droim-Chagaidh-scaled.jpg\" data-srcset=\"https:\/\/joycecountrygeoparkproject.ie\/wp-content\/uploads\/2020\/10\/View-NE-from-top-of-Droim-Chagaidh-scaled.jpg 2560w, https:\/\/joycecountrygeoparkproject.ie\/wp-content\/uploads\/2020\/10\/View-NE-from-top-of-Droim-Chagaidh-300x200.jpg 300w, https:\/\/joycecountrygeoparkproject.ie\/wp-content\/uploads\/2020\/10\/View-NE-from-top-of-Droim-Chagaidh-1024x683.jpg 1024w, https:\/\/joycecountrygeoparkproject.ie\/wp-content\/uploads\/2020\/10\/View-NE-from-top-of-Droim-Chagaidh-scaled-16x12.jpg 16w\" data-aspect=\"1.4997070884593\" \/><\/a>\n\t\t<\/figure>\n\t<\/div>\n<\/div><\/div><\/div><\/div><\/div><\/div><\/section><section class=\"vc_row wpb_row vc_row-fluid liquid-row-shadowbox-69d52af85e281\"><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-12 liquid-column-69d52af85e408\"><div class=\"vc_column-inner\"><div class=\"wpb_wrapper \"   ><div class=\"wpb_wrapper-inner\">\n\t<div class=\"wpb_text_column wpb_content_element\" >\n\t\t<div class=\"wpb_wrapper\">\n\t\t\t<p>Cracks in the bedrock were formed and were \u201cplugged\u201d by limited intrusions of magma in our geopark area, as seen by the <em>dolerite<\/em> sill on top of the Partry mountains at Droimchogaidh. This <strong>rifting<\/strong> activity that separated Ireland from Greenland and North America is also now thought to be responsible for the formation of the mountains that we see today in the west of Ireland. A section of Carboniferous <em>sandstone<\/em> that predates the Carboniferous <em>limestone<\/em> of Ireland is found on top of the <a href=\"https:\/\/joycecountrygeoparkproject.ie\/attractions\/maumtrasna-mountain-building-lough-nafooey-viewpoint\/175\/\">Maumtrasna<\/a> plateau, which sits 400m above the sea level. The same <em>sandstone<\/em>is also found at a depth of 300m below the surface around Clonbur. This indicates that the rocks west of Lough Mask and Lough Corrib were uplifted by about 700m. This would have occurred when the early spread of oceanic crust pushed the two landmasses apart, which would have locally pinned blocks of bedrock against one another in a limited space and pushed them upwards.<\/p>\n\n\t\t<\/div>\n\t<\/div>\n<\/div><\/div><\/div><\/div><\/div><\/div><\/section><\/section>\n<\/div>","protected":false},"excerpt":{"rendered":"250 Million Years Ago The Last 300 Million Years \u2013 After the Carboniferous There are...","protected":false},"author":1,"featured_media":5231,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[27],"tags":[],"class_list":["post-5396","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-geological-stories"],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v24.0 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>The Last 300 Million years \u2013 After the Carboniferous &#8212; 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