{"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\/ga\/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-69d55b8206a9f\"><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-12 liquid-column-69d55b8206c22\"><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>An 300 Milli\u00fan Bliain Seo Caite \u2013 I nDiaidh na Tr\u00e9imhse Carb\u00f3nmhaire<\/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-69d55b8206e79\"><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-3\/5 liquid-column-69d55b8207011\"><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>N\u00edl aon taifid chloiche in\u00e1r r\u00e9igi\u00fan geoph\u00e1irce le haghaidh an 250 milli\u00fan bliain ina dhiaidh sin. T\u00e1 a fhios againn \u00f3 cheantair eile in \u00c9irinn gur lean an mh\u00f3rchr\u00edoch ag bogadh \u00f3 thuaidh, i ndiaidh m\u00f3rchr\u00edoch eile ar a taobh \u00f3 dheas a bhuaileadh, a spreag roinnt d\u00edfhoirmi\u00fach\u00e1in ar an mbuncharraig agus ard\u00fa fhormh\u00f3r mh\u00f3rchr\u00edoch na h\u00c9ireann go leibh\u00e9al n\u00ed b\u2019airde n\u00e1 leibh\u00e9al na farraige mar a bh\u00ed ag an am sin. Toisc gur gn\u00e1ch le formh\u00f3r na dr\u00edodar lu\u00ed agus baili\u00fa in imchuacha, amhail grinneall na farraige, chiallaigh ard\u00fa mh\u00f3rchr\u00edoch na h\u00c9ireann os cionn leibh\u00e9al na farraige gur bheag dr\u00edodar a sil-leagadh in \u00c9irinn le linn an 250 milli\u00fan bliain seo.<\/p>\n<p class=\" translation-block\">\u00d3 thaobh na teicteonaice de, ba \u00e9 an ch\u00e9ad mh\u00f3rimeacht eile a taifeada\u00edodh sa r\u00e9igi\u00fan geoph\u00e1irce oscailt an Aig\u00e9in <strong>Atlantaigh<\/strong> thart ar 65 milli\u00fan bliain \u00f3 shin, ag deireadh na Tr\u00e9imhse <strong>Cailc\u00ed<\/strong> agus t\u00fas na Tr\u00e9imhse <strong>Pail\u00e9ig\u00e9in\u00ed<\/strong>. Cuireadh t\u00fas leis seo le tan\u00fa na screimhe ilchr\u00edocha\u00ed agus oscailt scoilteanna ina dhiaidh sin.<\/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-69d55b8207217\"><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-69d55b821917d\">\n\t\t\n\t\t<figure class=\"wpb_wrapper vc_figure\">\n\t\t\t<a data-rel=\"prettyPhoto[rel-5396-1258941629]\" 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-69d55b8219294\"><div class=\"ld-container container\"><div class=\"row ld-row\"><div class=\"wpb_column vc_column_container vc_col-sm-12 liquid-column-69d55b8219394\"><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\/ga\/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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