{"id":4422,"date":"2015-12-11T20:46:45","date_gmt":"2015-12-11T20:46:45","guid":{"rendered":"http:\/\/geopark.org.uk\/pub\/?p=4422"},"modified":"2023-06-19T09:22:37","modified_gmt":"2023-06-19T09:22:37","slug":"route-45-nr-dowles-brook","status":"publish","type":"post","link":"http:\/\/geopark.org.uk\/pub\/2015\/12\/route-45-nr-dowles-brook\/","title":{"rendered":"Route 45 nr Dowles Brook"},"content":{"rendered":"<div class=\"post-bodycopy clearfix\">\n<div class=\"post-bodycopy clearfix\">\n<div class=\"post-bodycopy clearfix\">\n<div id=\"attachment_4716\" style=\"width: 310px\" class=\"wp-caption alignright\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-4716\" class=\"size-medium wp-image-4716\" src=\"http:\/\/geopark.org.uk\/pub\/wp-content\/uploads\/2015\/12\/section-4b.7-exp-G.R-747-764.-GW-site-location-no.-14-5-300x225.jpg\" alt=\"Variety of lithologies in Carboniferous Etruria Formation \" width=\"300\" height=\"225\" srcset=\"http:\/\/geopark.org.uk\/pub\/wp-content\/uploads\/2015\/12\/section-4b.7-exp-G.R-747-764.-GW-site-location-no.-14-5-300x225.jpg 300w, http:\/\/geopark.org.uk\/pub\/wp-content\/uploads\/2015\/12\/section-4b.7-exp-G.R-747-764.-GW-site-location-no.-14-5-150x113.jpg 150w, http:\/\/geopark.org.uk\/pub\/wp-content\/uploads\/2015\/12\/section-4b.7-exp-G.R-747-764.-GW-site-location-no.-14-5-400x300.jpg 400w, http:\/\/geopark.org.uk\/pub\/wp-content\/uploads\/2015\/12\/section-4b.7-exp-G.R-747-764.-GW-site-location-no.-14-5.jpg 640w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><p id=\"caption-attachment-4716\" class=\"wp-caption-text\">Variety of lithologies in Carboniferous Etruria Formation<\/p><\/div>\n<p style=\"text-align: justify;\"><b>Geological overview<br \/>\n<\/b>This exposure of Carboniferous-aged, Etruria Formation rocks consist of multi-coloured red, purple, yellow and green-grey, commonly mottled mudstone. These sediments were deposited on a well-drained alluvial plain and were extensively affected by soil-forming processes. Layers of sandstone within the layers of finner-grained mudstones and siltstones represent the deposits of shallow river channels and sheet flooding.<\/p>\n<p><b>Location<br \/>\n<\/b>Kinlet, Wyre Forest, Shropshire; Grid Reference: SO 7462 7644<\/p>\n<p><b>Access<br \/>\n<\/b>Open along a public right of way<\/p>\n<p><b>Geologi<\/b><b>cal Age<br \/>\n<\/b>Carboniferou<b>s <\/b>&#8211; Etruria Formation<\/p>\n<p><strong>Rock Types <\/strong><br \/>\nSedimentary &#8211; sandstone, siltstone, mudstone, clay<\/p>\n<p><strong>Features<\/strong><br \/>\nSedimentary structures<\/p>\n<p><b>Interpretation<br \/>\n<\/b>Section 4 of the <a href=\"http:\/\/geopark.org.uk\/pub\/category\/explore-geology-landscape\/walking-trails\/the-geopark-way\/\" target=\"_blank\" rel=\"noopener\">Geopark Way<\/a> trail<\/p>\n<\/div>\n<\/div>\n<\/div>\n","protected":false},"excerpt":{"rendered":"\n<p id=\"caption-attachment-4716\" class=\"wp-caption-text\">Variety of lithologies in Carboniferous Etruria Formation<\/p>\n<p style=\"text-align: justify;\">Geological overview This exposure of Carboniferous-aged, Etruria Formation rocks consist of multi-coloured red, purple, yellow and green-grey, commonly mottled mudstone. These sediments were deposited on a well-drained alluvial plain and were extensively affected by soil-forming processes. Layers of sandstone within the layers of [&#8230;]<\/p>\n","protected":false},"author":2,"featured_media":0,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"om_disable_all_campaigns":false,"_monsterinsights_skip_tracking":false,"_monsterinsights_sitenote_active":false,"_monsterinsights_sitenote_note":"","_monsterinsights_sitenote_category":0,"footnotes":""},"categories":[4],"tags":[],"aioseo_notices":[],"_links":{"self":[{"href":"http:\/\/geopark.org.uk\/pub\/wp-json\/wp\/v2\/posts\/4422"}],"collection":[{"href":"http:\/\/geopark.org.uk\/pub\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"http:\/\/geopark.org.uk\/pub\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"http:\/\/geopark.org.uk\/pub\/wp-json\/wp\/v2\/users\/2"}],"replies":[{"embeddable":true,"href":"http:\/\/geopark.org.uk\/pub\/wp-json\/wp\/v2\/comments?post=4422"}],"version-history":[{"count":5,"href":"http:\/\/geopark.org.uk\/pub\/wp-json\/wp\/v2\/posts\/4422\/revisions"}],"predecessor-version":[{"id":6513,"href":"http:\/\/geopark.org.uk\/pub\/wp-json\/wp\/v2\/posts\/4422\/revisions\/6513"}],"wp:attachment":[{"href":"http:\/\/geopark.org.uk\/pub\/wp-json\/wp\/v2\/media?parent=4422"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/geopark.org.uk\/pub\/wp-json\/wp\/v2\/categories?post=4422"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/geopark.org.uk\/pub\/wp-json\/wp\/v2\/tags?post=4422"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}