1.0EcoShape - ENhttps://www.ecoshape.org/enLithosphere - salt marshesrich600338<blockquote class="wp-embedded-content" data-secret="cCciHKjOic"><a href="https://www.ecoshape.org/en/concepts/growing-salt-marshes/lithosphere/">Lithosphere – salt marshes</a></blockquote><iframe sandbox="allow-scripts" security="restricted" src="https://www.ecoshape.org/en/concepts/growing-salt-marshes/lithosphere/embed/#?secret=cCciHKjOic" width="600" height="338" title="“Lithosphere – salt marshes” — EcoShape - EN" data-secret="cCciHKjOic" frameborder="0" marginwidth="0" marginheight="0" scrolling="no" class="wp-embedded-content"></iframe><script>
/*! This file is auto-generated */
!function(d,l){"use strict";l.querySelector&&d.addEventListener&&"undefined"!=typeof URL&&(d.wp=d.wp||{},d.wp.receiveEmbedMessage||(d.wp.receiveEmbedMessage=function(e){var t=e.data;if((t||t.secret||t.message||t.value)&&!/[^a-zA-Z0-9]/.test(t.secret)){for(var s,r,n,a=l.querySelectorAll('iframe[data-secret="'+t.secret+'"]'),o=l.querySelectorAll('blockquote[data-secret="'+t.secret+'"]'),c=new RegExp("^https?:$","i"),i=0;i<o.length;i++)o[i].style.display="none";for(i=0;i<a.length;i++)s=a[i],e.source===s.contentWindow&&(s.removeAttribute("style"),"height"===t.message?(1e3<(r=parseInt(t.value,10))?r=1e3:~~r<200&&(r=200),s.height=r):"link"===t.message&&(r=new URL(s.getAttribute("src")),n=new URL(t.value),c.test(n.protocol))&&n.host===r.host&&l.activeElement===s&&(d.top.location.href=t.value))}},d.addEventListener("message",d.wp.receiveEmbedMessage,!1),l.addEventListener("DOMContentLoaded",function(){for(var e,t,s=l.querySelectorAll("iframe.wp-embedded-content"),r=0;r<s.length;r++)(t=(e=s[r]).getAttribute("data-secret"))||(t=Math.random().toString(36).substring(2,12),e.src+="#?secret="+t,e.setAttribute("data-secret",t)),e.contentWindow.postMessage({message:"ready",secret:t},"*")},!1)))}(window,document);
//# sourceURL=https://www.ecoshape.org/en/wp-includes/js/wp-embed.min.js
</script>
Soil subsidence: Marshes increase in elevation and thereby counteract soil subsidence. Typical marsh accretion rates are in the order of 10 mm per year. Very strong rates of soil subsidence (higher than the local marsh accretion rate) will most likely cause marshes to drown in the future. Especially as soil subsidence and sea-level rise together […]