{"id":1670,"date":"2025-06-06T16:36:49","date_gmt":"2025-06-06T16:36:49","guid":{"rendered":"https:\/\/sites.warnercnr.colostate.edu\/fluvial-geomorphology\/?p=1670"},"modified":"2025-06-06T16:36:50","modified_gmt":"2025-06-06T16:36:50","slug":"dr-david-sear-seminar","status":"publish","type":"post","link":"https:\/\/sites.warnercnr.colostate.edu\/fluvial-geomorphology\/2025\/06\/06\/dr-david-sear-seminar\/","title":{"rendered":"Dr. David Sear seminar"},"content":{"rendered":"\n<p>David Sear visited from the University of Southampton, UK, and gave a seminar: What does process-based restoration mean in groundwater-dominated low-energy river systems with 6000 years of human history?<\/p>\n\n\n\n<figure class=\"wp-block-image size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"1545\" height=\"2000\" src=\"https:\/\/sites.warnercnr.colostate.edu\/fluvial-geomorphology\/wp-content\/uploads\/sites\/53\/2025\/06\/David-Sear-Seminar.jpg\" alt=\"\" class=\"wp-image-1672\" style=\"width:253px;height:auto\" srcset=\"https:\/\/sites.warnercnr.colostate.edu\/fluvial-geomorphology\/wp-content\/uploads\/sites\/53\/2025\/06\/David-Sear-Seminar.jpg 1545w, https:\/\/sites.warnercnr.colostate.edu\/fluvial-geomorphology\/wp-content\/uploads\/sites\/53\/2025\/06\/David-Sear-Seminar-768x994.jpg 768w, https:\/\/sites.warnercnr.colostate.edu\/fluvial-geomorphology\/wp-content\/uploads\/sites\/53\/2025\/06\/David-Sear-Seminar-1187x1536.jpg 1187w\" sizes=\"auto, (max-width: 1545px) 100vw, 1545px\" \/><\/figure>\n\n\n\n<p>David encouraged members of our lab to see as many different rivers as possible, so in the spirit of his advice we took him for a tour of a mountain river in the Southern Rockies.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full is-resized\"><img loading=\"lazy\" decoding=\"async\" width=\"2560\" height=\"1920\" src=\"https:\/\/sites.warnercnr.colostate.edu\/fluvial-geomorphology\/wp-content\/uploads\/sites\/53\/2025\/06\/LBC_SFP_April282025-6-scaled.jpg\" alt=\"\" class=\"wp-image-1671\" style=\"width:500px;height:auto\" srcset=\"https:\/\/sites.warnercnr.colostate.edu\/fluvial-geomorphology\/wp-content\/uploads\/sites\/53\/2025\/06\/LBC_SFP_April282025-6-scaled.jpg 2560w, https:\/\/sites.warnercnr.colostate.edu\/fluvial-geomorphology\/wp-content\/uploads\/sites\/53\/2025\/06\/LBC_SFP_April282025-6-768x576.jpg 768w, https:\/\/sites.warnercnr.colostate.edu\/fluvial-geomorphology\/wp-content\/uploads\/sites\/53\/2025\/06\/LBC_SFP_April282025-6-1536x1152.jpg 1536w, https:\/\/sites.warnercnr.colostate.edu\/fluvial-geomorphology\/wp-content\/uploads\/sites\/53\/2025\/06\/LBC_SFP_April282025-6-2048x1536.jpg 2048w\" sizes=\"auto, (max-width: 2560px) 100vw, 2560px\" \/><\/figure>\n","protected":false},"excerpt":{"rendered":"<p>David Sear visited from the University of Southampton, UK, and gave a seminar: What does process-based restoration mean in groundwater-dominated low-energy river systems with 6000 years of human history? David encouraged members of our lab to see as many different &hellip; <a href=\"https:\/\/sites.warnercnr.colostate.edu\/fluvial-geomorphology\/2025\/06\/06\/dr-david-sear-seminar\/\">Continue reading <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n","protected":false},"author":235,"featured_media":0,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[],"class_list":["post-1670","post","type-post","status-publish","format-standard","hentry","category-uncategorized"],"_links":{"self":[{"href":"https:\/\/sites.warnercnr.colostate.edu\/fluvial-geomorphology\/wp-json\/wp\/v2\/posts\/1670","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/sites.warnercnr.colostate.edu\/fluvial-geomorphology\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/sites.warnercnr.colostate.edu\/fluvial-geomorphology\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/sites.warnercnr.colostate.edu\/fluvial-geomorphology\/wp-json\/wp\/v2\/users\/235"}],"replies":[{"embeddable":true,"href":"https:\/\/sites.warnercnr.colostate.edu\/fluvial-geomorphology\/wp-json\/wp\/v2\/comments?post=1670"}],"version-history":[{"count":1,"href":"https:\/\/sites.warnercnr.colostate.edu\/fluvial-geomorphology\/wp-json\/wp\/v2\/posts\/1670\/revisions"}],"predecessor-version":[{"id":1673,"href":"https:\/\/sites.warnercnr.colostate.edu\/fluvial-geomorphology\/wp-json\/wp\/v2\/posts\/1670\/revisions\/1673"}],"wp:attachment":[{"href":"https:\/\/sites.warnercnr.colostate.edu\/fluvial-geomorphology\/wp-json\/wp\/v2\/media?parent=1670"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/sites.warnercnr.colostate.edu\/fluvial-geomorphology\/wp-json\/wp\/v2\/categories?post=1670"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/sites.warnercnr.colostate.edu\/fluvial-geomorphology\/wp-json\/wp\/v2\/tags?post=1670"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}