{"id":4461,"date":"2015-12-11T20:41:58","date_gmt":"2015-12-11T20:41:58","guid":{"rendered":"http:\/\/geopark.org.uk\/pub\/?p=4461"},"modified":"2023-06-19T09:23:26","modified_gmt":"2023-06-19T09:23:26","slug":"teme-valley","status":"publish","type":"post","link":"http:\/\/geopark.org.uk\/pub\/2015\/12\/teme-valley\/","title":{"rendered":"Teme Valley"},"content":{"rendered":"<div class=\"post-bodycopy clearfix\">\n<div class=\"post-bodycopy clearfix\">\n<div id=\"attachment_4727\" style=\"width: 310px\" class=\"wp-caption alignright\"><img loading=\"lazy\" decoding=\"async\" aria-describedby=\"caption-attachment-4727\" class=\"wp-image-4727 size-medium\" src=\"http:\/\/geopark.org.uk\/pub\/wp-content\/uploads\/2015\/12\/River-Teme-Martley-300x225.jpg\" alt=\"River Teme, Martley\" width=\"300\" height=\"225\" srcset=\"http:\/\/geopark.org.uk\/pub\/wp-content\/uploads\/2015\/12\/River-Teme-Martley-300x225.jpg 300w, http:\/\/geopark.org.uk\/pub\/wp-content\/uploads\/2015\/12\/River-Teme-Martley-150x113.jpg 150w, http:\/\/geopark.org.uk\/pub\/wp-content\/uploads\/2015\/12\/River-Teme-Martley-400x300.jpg 400w, http:\/\/geopark.org.uk\/pub\/wp-content\/uploads\/2015\/12\/River-Teme-Martley.jpg 640w\" sizes=\"(max-width: 300px) 100vw, 300px\" \/><p id=\"caption-attachment-4727\" class=\"wp-caption-text\">River Teme, Martley<\/p><\/div>\n<p style=\"text-align: justify;\"><strong>Geological Overview<b><br \/>\n<\/b><\/strong>The River Teme is remarkable for its near natural form and as such is a Site of Special Scientific Interest (SSSI) throughout its length. Known as the &#8216;Wild Daughter of the River Severn&#8217; due to its sinuous nature, it twists its way for 81 miles from its source on Cilfaesty Hill, Powys, Wales, through its often steep-sided valley to its confluence with the River Severn near Worcester.<\/p>\n<p style=\"text-align: justify;\">The history of the River Teme is complicated and encompasses glacial diversions, river captures, glacial lakes, melt-water torrents and bygone river systems.<\/p>\n<p style=\"text-align: justify;\">Today the Lower Teme has a deep channel cut in a wide alluvial plain. Channel plan-form is one dominated by free menders across the floodplain. Since the Teme is a \u2018flashy\u2019 river, which responds rapidly to rain fall inputs to the basin, large and rapid changes in stage, velocity and discharge occur. Thus form-process relationships at the channel margins are readily observable and often spectacular in nature. Channel change can be rapid. Cut-offs and near cut-off are numerous along the river\u2019s course and floodplain features such as backchannels and old oxbows can be seen clearly.<\/p>\n<p><b>Location<br \/>\n<\/b>Teme Valley, Martley, Worcestershire; Grid Reference: SO 7450 6030<\/p>\n<p><b>Access<br \/>\n<\/b>Open along public right of way<\/p>\n<p><b>Geologi<\/b><b>cal Age<br \/>\n<\/b>Quaternary<\/p>\n<\/div>\n<div class=\"post-bodycopy clearfix\">\n<p><strong>Features<br \/>\n<\/strong>Geomorphology<br \/>\nIce Age interpretation of the changing course of the River Teme<\/p>\n<p><b>Interpretation<br \/>\n<\/b>Interpretation board on site<br \/>\nMartley geology trails <a href=\"http:\/\/geopark.org.uk\/pub\/2015\/12\/3c-martley-a-geopark-way-circular-trail\/\" target=\"_blank\" rel=\"noopener\">1<\/a> and <a href=\"http:\/\/www.geo-village.eu\/?page_id=1644\" target=\"_blank\" rel=\"noopener\">3<\/a><br \/>\nSection 7 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><\/p>\n<\/div>\n<\/div>\n","protected":false},"excerpt":{"rendered":"\n<p id=\"caption-attachment-4727\" class=\"wp-caption-text\">River Teme, Martley<\/p>\n<p style=\"text-align: justify;\">Geological Overview The River Teme is remarkable for its near natural form and as such is a Site of Special Scientific Interest (SSSI) throughout its length. Known as the &#8216;Wild Daughter of the River Severn&#8217; due to its sinuous nature, it twists its way for 81 miles [&#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\/4461"}],"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=4461"}],"version-history":[{"count":4,"href":"http:\/\/geopark.org.uk\/pub\/wp-json\/wp\/v2\/posts\/4461\/revisions"}],"predecessor-version":[{"id":6517,"href":"http:\/\/geopark.org.uk\/pub\/wp-json\/wp\/v2\/posts\/4461\/revisions\/6517"}],"wp:attachment":[{"href":"http:\/\/geopark.org.uk\/pub\/wp-json\/wp\/v2\/media?parent=4461"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"http:\/\/geopark.org.uk\/pub\/wp-json\/wp\/v2\/categories?post=4461"},{"taxonomy":"post_tag","embeddable":true,"href":"http:\/\/geopark.org.uk\/pub\/wp-json\/wp\/v2\/tags?post=4461"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}