{"id":3143,"date":"2021-03-08T09:48:03","date_gmt":"2021-03-08T09:48:03","guid":{"rendered":"https:\/\/www.icterra.pt\/?p=3143"},"modified":"2021-03-12T10:04:25","modified_gmt":"2021-03-12T10:04:25","slug":"geologia-e-2","status":"publish","type":"post","link":"https:\/\/www.icterra.pt\/legacy\/index.php\/2021\/03\/08\/geologia-e-2\/","title":{"rendered":"Geologia e\u2026"},"content":{"rendered":"<p style=\"text-align: justify;\"><u><\/u><span style=\"font-size: 12pt; font-family: arial, helvetica, sans-serif;\">Na pr\u00f3xima 4 feira, dia 2021-03-10 das 18.00 \u00e0s 19.30, continua o Webminar &#8220;Geologia e &#8230;&#8221; com a confer\u00eancia do Prof. Carlos Ribeiro, subordinada ao tema &#8220;<b><i>Geologia e\u2026 o perigo que vem do fundo do mar<\/i><\/b>\u00a0&#8220;<u><\/u><u><\/u><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-size: 12pt; font-family: arial, helvetica, sans-serif;\"><i>Deslizamentos de terreno submarinos, gerados atrav\u00e9s de processos como abalos s\u00edsmicos ou sobrepressuriza\u00e7\u00e3o de sedimentos est\u00e3o frequentemente na origem de tsunamis. Como se detetam os deslizamentos submarinos? Como se avalia o seu potencial para gerar tsunamis? Quais os fatores que facilitam a sua ocorr\u00eancia?<u><\/u><u><\/u><\/i><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-size: 12pt; font-family: arial, helvetica, sans-serif;\">A confer\u00eancia ser\u00e1 realizada online atrav\u00e9s da Plataforma Zoom.\u00a0<a href=\"https:\/\/videoconf-colibri.zoom.us\/j\/88670733864\" target=\"_blank\" rel=\"noopener noreferrer\" data-saferedirecturl=\"https:\/\/www.google.com\/url?q=https:\/\/videoconf-colibri.zoom.us\/j\/88670733864&amp;source=gmail&amp;ust=1615279319363000&amp;usg=AFQjCNFrSoHXidsn-n_rxXQltDeGnea2UA\">https:\/\/videoconf-colibri.<wbr \/>zoom.us\/j\/88670733864<\/a><u><\/u><u><\/u><\/span><\/p>\n<p style=\"text-align: justify;\"><span style=\"font-size: 12pt; font-family: arial, helvetica, sans-serif;\">Contamos com a vossa presen\u00e7a e agradecemos a sua divulga\u00e7\u00e3o nas vossas listas de contatos.<\/span><\/p>\n<p><img loading=\"lazy\" decoding=\"async\" class=\"alignnone size-medium wp-image-3121\" src=\"https:\/\/www.icterra.pt\/wp-content\/uploads\/2021\/02\/Geologia-e-2-213x300.jpg\" alt=\"\" width=\"213\" height=\"300\" srcset=\"https:\/\/www.icterra.pt\/legacy\/wp-content\/uploads\/2021\/02\/Geologia-e-2-213x300.jpg 213w, https:\/\/www.icterra.pt\/legacy\/wp-content\/uploads\/2021\/02\/Geologia-e-2-726x1024.jpg 726w, https:\/\/www.icterra.pt\/legacy\/wp-content\/uploads\/2021\/02\/Geologia-e-2-768x1083.jpg 768w, https:\/\/www.icterra.pt\/legacy\/wp-content\/uploads\/2021\/02\/Geologia-e-2-1089x1536.jpg 1089w, https:\/\/www.icterra.pt\/legacy\/wp-content\/uploads\/2021\/02\/Geologia-e-2-820x1157.jpg 820w, https:\/\/www.icterra.pt\/legacy\/wp-content\/uploads\/2021\/02\/Geologia-e-2.jpg 1452w\" sizes=\"(max-width: 213px) 100vw, 213px\" \/><\/p>\n","protected":false},"excerpt":{"rendered":"<p>Na pr\u00f3xima 4 feira, dia 2021-03-10 das 18.00 \u00e0s 19.30, continua o Webminar &#8220;Geologia e &#8230;&#8221; com a confer\u00eancia do Prof. Carlos Ribeiro, subordinada ao tema &#8220;Geologia e\u2026 o perigo que vem do fundo do mar\u00a0&#8220; Deslizamentos de terreno submarinos, gerados atrav\u00e9s de processos como abalos s\u00edsmicos ou sobrepressuriza\u00e7\u00e3o de sedimentos est\u00e3o frequentemente na origem [&hellip;]<\/p>\n","protected":false},"author":3,"featured_media":3144,"comment_status":"closed","ping_status":"closed","sticky":false,"template":"","format":"standard","meta":{"footnotes":""},"categories":[219],"tags":[],"_links":{"self":[{"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/posts\/3143"}],"collection":[{"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/users\/3"}],"replies":[{"embeddable":true,"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/comments?post=3143"}],"version-history":[{"count":1,"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/posts\/3143\/revisions"}],"predecessor-version":[{"id":3145,"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/posts\/3143\/revisions\/3145"}],"wp:featuredmedia":[{"embeddable":true,"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/media\/3144"}],"wp:attachment":[{"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/media?parent=3143"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/categories?post=3143"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/www.icterra.pt\/legacy\/index.php\/wp-json\/wp\/v2\/tags?post=3143"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}