{"id":1751,"date":"2022-11-08T10:58:51","date_gmt":"2022-11-08T15:58:51","guid":{"rendered":"https:\/\/sites.williams.edu\/rcox\/files\/2022\/11\/sedimentology_505.jpg"},"modified":"2022-12-01T16:09:27","modified_gmt":"2022-12-01T21:09:27","slug":"sedimentology_505","status":"inherit","type":"attachment","link":"https:\/\/sites.williams.edu\/rcox\/cox-sedimentology\/dc2016_016_176_cox176\/attachment\/sedimentology_505\/","title":{"rendered":"DC2016_016_176_Cox176"},"author":1455,"featured_media":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_acf_changed":false},"class_list":["post-1751","attachment","type-attachment","status-inherit","hentry"],"acf":[],"description":{"rendered":"<p class=\"attachment\"><a href='https:\/\/sites.williams.edu\/rcox\/files\/2022\/11\/sedimentology_505.jpg'><img loading=\"lazy\" decoding=\"async\" width=\"300\" height=\"207\" src=\"https:\/\/sites.williams.edu\/rcox\/files\/2022\/11\/sedimentology_505-300x207.jpg\" class=\"attachment-medium size-medium\" alt=\"Upper Image: Dunes on a point Bar. Made of coarse gravel with 100m wavelength. Lower Image: Flood-transported boulder in the Grand Coulee Channel.\" srcset=\"https:\/\/sites.williams.edu\/rcox\/files\/2022\/11\/sedimentology_505-300x207.jpg 300w, https:\/\/sites.williams.edu\/rcox\/files\/2022\/11\/sedimentology_505.jpg 600w\" sizes=\"auto, (max-width: 300px) 100vw, 300px\" \/><\/a><\/p>\n<p>Upper Image: Dunes on a point Bar. Made of coarse gravel with 100m wavelength. Lower Image: Flood-transported boulder in the Grand Coulee Channel.<\/p>\n"},"caption":{"rendered":"<p>Sedimentology; Rivers &#8211; General <a href=\"https:\/\/sites.williams.edu\/rcox\/cox-sedimentology\/dc2016_016_176_cox176\/attachment\/sedimentology_505\/\">Continue reading <span class=\"meta-nav\">&rarr;<\/span><\/a><\/p>\n"},"alt_text":"Upper Image: Dunes on a point Bar. Made of coarse gravel with 100m wavelength. Lower Image: Flood-transported boulder in the Grand Coulee Channel.","media_type":"image","mime_type":"image\/jpeg","media_details":{"width":600,"height":413,"file":"2022\/11\/sedimentology_505.jpg","filesize":58180,"sizes":{"medium":{"file":"sedimentology_505-300x207.jpg","width":300,"height":207,"filesize":13027,"mime_type":"image\/jpeg","source_url":"https:\/\/sites.williams.edu\/rcox\/files\/2022\/11\/sedimentology_505-300x207.jpg"},"thumbnail":{"file":"sedimentology_505-150x150.jpg","width":150,"height":150,"filesize":5263,"mime_type":"image\/jpeg","source_url":"https:\/\/sites.williams.edu\/rcox\/files\/2022\/11\/sedimentology_505-150x150.jpg"},"full":{"file":"sedimentology_505.jpg","width":600,"height":413,"mime_type":"image\/jpeg","source_url":"https:\/\/sites.williams.edu\/rcox\/files\/2022\/11\/sedimentology_505.jpg"}},"image_meta":{"aperture":"0","credit":"","camera":"","caption":"","created_timestamp":"0","copyright":"","focal_length":"0","iso":"0","shutter_speed":"0","title":"","orientation":"0","keywords":[]}},"post":4202,"source_url":"https:\/\/sites.williams.edu\/rcox\/files\/2022\/11\/sedimentology_505.jpg","filename":"sedimentology_505.jpg","filesize":58180,"_links":{"self":[{"href":"https:\/\/sites.williams.edu\/rcox\/wp-json\/wp\/v2\/media\/1751","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/sites.williams.edu\/rcox\/wp-json\/wp\/v2\/media"}],"about":[{"href":"https:\/\/sites.williams.edu\/rcox\/wp-json\/wp\/v2\/types\/attachment"}],"author":[{"embeddable":true,"href":"https:\/\/sites.williams.edu\/rcox\/wp-json\/wp\/v2\/users\/1455"}],"replies":[{"embeddable":true,"href":"https:\/\/sites.williams.edu\/rcox\/wp-json\/wp\/v2\/comments?post=1751"}],"wp:attached-to":[{"embeddable":true,"post_type":"cox-sedimentology","id":4202,"href":"https:\/\/sites.williams.edu\/rcox\/wp-json\/wp\/v2\/cox-sedimentology\/4202"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}