{"id":482,"date":"2009-01-22T21:56:00","date_gmt":"2009-01-22T21:56:00","guid":{"rendered":"http:\/\/blogs.agu.org\/landslideblog\/2009\/01\/22\/whitby-the-old-and-the-new\/"},"modified":"2010-10-21T13:37:42","modified_gmt":"2010-10-21T17:37:42","slug":"whitby-the-old-and-the-new","status":"publish","type":"post","link":"https:\/\/blogs.agu.org\/landslideblog\/2009\/01\/22\/whitby-the-old-and-the-new\/","title":{"rendered":"Whitby &#8211; the old and the new"},"content":{"rendered":"<p>As someone interested in earth processes, one of the great powers of the <span class=\"blsp-spelling-error\">internet<\/span> is the ability to access quickly images of places in which I am interested.  Over the last few years my colleagues and I have been studying rockfall processes at the town of Whitby in N. Yorkshire, which is in NE. England.  I thought as a bit of fun I would compare two images of the cliffs in the town.  The first, assessed from <a href=\"http:\/\/www.oldukphotos.com\/yorkshire-whitby.htm\">here<\/a>, was taken in the 1900&#8217;s &#8211; i.e. a century ago:<\/p>\n<p><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/09_01-whitby-1.jpg\"><img decoding=\"async\" style=\"margin: 0px auto 10px;text-align: center;cursor: pointer;width: 415px;height: 307px\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/09_01-whitby-1.jpg\" alt=\"\" border=\"0\" \/><\/a><br \/>The second, accessed from <a href=\"http:\/\/milliondollarlake.com\/images\/Whitby%20Harbour.jpg\">here<\/a>, was taken in the last few years:<\/p>\n<p><a href=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/09_01-whitby-3.jpg\"><img decoding=\"async\" style=\"margin: 0px auto 10px;text-align: center;cursor: pointer;width: 400px;height: 300px\" src=\"https:\/\/blogs.agu.org\/landslideblog\/files\/2010\/10\/09_01-whitby-3.jpg\" alt=\"\" border=\"0\" \/><\/a><\/p>\n<p>There are several things of interest here.  It is important to note that the two images were not taken from quite the same angle -the 2000&#8217;s image was taken further from the sea than was the 1900&#8217;s one, though there is not much difference.  However, there is quite a lot of interest here.  First, note the very different beaches between the two images &#8211; in the 1900&#8217;s image there is very little beach visible, and indeed boats are <span class=\"blsp-spelling-corrected\">moored<\/span> by the small pier.  Now the beach has encroached into this area, presumably through natural accretion though I guess it could have been <span class=\"blsp-spelling-corrected\">artificially<\/span> stocked.<\/p>\n<p>More interesting, the profile of the cliff has changed dramatically.  The cliff a century ago was far less steep, with a large, protruding toe.  In the recent image most of this toe has been eroded away, leaving a far steeper profile.  Interestingly though the profile of the top of the slope is little changed, except being a little steeper.  Presumably as the toe continues to <span class=\"blsp-spelling-corrected\">erode<\/span>, and thus the slope to steepen, the rate of erosion at the top will increase, or a large <span class=\"blsp-spelling-corrected\">failure<\/span> will occur that will cause the cliff top to erode back a few metres.  Fortunately, it is a long way to the abbey and church, and there is little else at the cliff top to worry about unduly.<\/p>\n<!-- AddThis Advanced Settings generic via filter on the_content --><!-- AddThis Share Buttons generic via filter on the_content -->","protected":false},"excerpt":{"rendered":"<p>As someone interested in earth processes, one of the great powers of the internet is the ability to access quickly images of places in which I am interested. Over the last few years my colleagues and I have been studying rockfall processes at the town of Whitby in N. Yorkshire, which is in NE. England. I thought as a bit of fun I would compare two images of the cliffs &hellip;<!-- AddThis Advanced Settings generic via filter on wp_trim_excerpt --><!-- AddThis Share Buttons generic via filter on wp_trim_excerpt --><\/p>\n","protected":false},"author":22,"featured_media":0,"comment_status":"open","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[1],"tags":[134,182,21],"class_list":["post-482","post","type-post","status-publish","format-standard","hentry","category-uncategorized","tag-coastal-erosion","tag-england","tag-images"],"_links":{"self":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/482","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/users\/22"}],"replies":[{"embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/comments?post=482"}],"version-history":[{"count":0,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/posts\/482\/revisions"}],"wp:attachment":[{"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/media?parent=482"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/categories?post=482"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/blogs.agu.org\/landslideblog\/wp-json\/wp\/v2\/tags?post=482"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}