{"version":"1.0","provider_name":"Aegeus Society","provider_url":"https:\/\/www.aegeussociety.org\/en\/","author_name":"Aegeus Assistant 2","author_url":"https:\/\/www.aegeussociety.org\/en\/author\/aegeusassistant2\/","title":"Landscape evolution in the Kifissos floodplain - Aegeus Society","type":"rich","width":600,"height":338,"html":"<blockquote class=\"wp-embedded-content\" data-secret=\"srgL1ZWBIF\"><a href=\"https:\/\/www.aegeussociety.org\/en\/new_article\/landscape-evolution-in-the-kifissos-floodplain\/\">Landscape evolution in the Kifissos floodplain<\/a><\/blockquote><iframe sandbox=\"allow-scripts\" security=\"restricted\" src=\"https:\/\/www.aegeussociety.org\/en\/new_article\/landscape-evolution-in-the-kifissos-floodplain\/embed\/#?secret=srgL1ZWBIF\" width=\"600\" height=\"338\" title=\"&#8220;Landscape evolution in the Kifissos floodplain&#8221; &#8212; Aegeus Society\" data-secret=\"srgL1ZWBIF\" frameborder=\"0\" marginwidth=\"0\" marginheight=\"0\" scrolling=\"no\" class=\"wp-embedded-content\"><\/iframe><script type=\"text\/javascript\">\n\/* <![CDATA[ *\/\n\/*! This file is auto-generated *\/\n!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);\n\/\/# sourceURL=https:\/\/www.aegeussociety.org\/wp-includes\/js\/wp-embed.min.js\n\/* ]]> *\/\n<\/script>\n","description":"he effect of the mid-Holocene sea level highstand is confirmed as a contributing factor in the formation of the Piraeus early island, as narrated by Strabo, roughly in the period between 6000 and 5000 years before present. Meandering of the Kifissos River resulted in the formation of oxbow lakes which can be traced on modem topographic maps as closed depressions. A meander of the Kifissos River is delineated which flooded ancient sites in the 5th century BC near Plato\u2019s Academy and he indicates that the statesman of Athens Cimon \u201cconverted the Academy from a waterless and arid spot into a well-watered grove\u201d by digging channels for watering from this meander."}