 
<?xml version="1.0" encoding="UTF-8"?>
<rss version="2.0"
	xmlns:content="http://purl.org/rss/1.0/modules/content/"
	xmlns:wfw="http://wellformedweb.org/CommentAPI/"
	xmlns:dc="http://purl.org/dc/elements/1.1/"
	xmlns:atom="http://www.w3.org/2005/Atom"
	xmlns:sy="http://purl.org/rss/1.0/modules/syndication/"
	xmlns:slash="http://purl.org/rss/1.0/modules/slash/"
	>

<channel>
	<title>Corrado Venturini &#187; morene</title>
	<atom:link href="https://www.corradoventurini.it/cor/tag/morene/feed/" rel="self" type="application/rss+xml" />
	<link>https://www.corradoventurini.it/cor</link>
	<description>anche le pietre sono parole</description>
	<lastBuildDate>Tue, 22 Sep 2026 08:48:03 +0000</lastBuildDate>
	<language>it-IT</language>
		<sy:updatePeriod>hourly</sy:updatePeriod>
		<sy:updateFrequency>1</sy:updateFrequency>
	<generator>https://wordpress.org/?v=3.9.35</generator>
	<item>
		<title>Scarpata fluviale di Aonedis</title>
		<link>https://www.corradoventurini.it/cor/scarpata-fluviale-di-aonedis/</link>
		<comments>https://www.corradoventurini.it/cor/scarpata-fluviale-di-aonedis/#comments</comments>
		<pubDate>Tue, 28 May 2013 19:26:57 +0000</pubDate>
		<dc:creator><![CDATA[Conradus]]></dc:creator>
				<category><![CDATA[DIVULGAZIONE]]></category>
		<category><![CDATA[Geositi del FVG]]></category>
		<category><![CDATA[morene]]></category>
		<category><![CDATA[paleo-laghi]]></category>
		<category><![CDATA[Würm]]></category>

		<guid isPermaLink="false">http://www.corradoventurini.it/cvw/?p=1422</guid>
		<description><![CDATA[<p>Il sito si affaccia sull’ampio alveo ghiaioso del Fiume Tagliamento, in sinistra idrografica. è situato tra Aonedis e il ponte di Pinzano (v. geosito Stretta di Pinzano e conglomerati miocenici). È rappresentato da una ripida parete, alta 55 m ed estesa 300 m. La incide il Tagliamento che ha messo allo scoperto, dal basso verso [&#8230;]</p>
<p>The post <a rel="nofollow" href="https://www.corradoventurini.it/cor/scarpata-fluviale-di-aonedis/">Scarpata fluviale di Aonedis</a> appeared first on <a rel="nofollow" href="https://www.corradoventurini.it/cor">Corrado Venturini</a>.</p>
]]></description>
		<wfw:commentRss>https://www.corradoventurini.it/cor/scarpata-fluviale-di-aonedis/feed/</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>Cordoni morenici presso Valbertad (Lanza)</title>
		<link>https://www.corradoventurini.it/cor/cordoni-morenici-presso-valbertad-lanza/</link>
		<comments>https://www.corradoventurini.it/cor/cordoni-morenici-presso-valbertad-lanza/#comments</comments>
		<pubDate>Mon, 27 May 2013 17:04:10 +0000</pubDate>
		<dc:creator><![CDATA[Conradus]]></dc:creator>
				<category><![CDATA[DIVULGAZIONE]]></category>
		<category><![CDATA[Geositi del FVG]]></category>
		<category><![CDATA[morene]]></category>
		<category><![CDATA[Würm]]></category>

		<guid isPermaLink="false">http://www.corradoventurini.it/cvw/?p=1235</guid>
		<description><![CDATA[<p>La storia geologica del Monte Zermula, la cui successione rocciosa raggiunge e supera i 400 milioni di anni, si è arricchita di interessanti testimonianze tardo-glaciali würmiane in tempi che possiamo considerare recenti (circa 16.000 anni fa). Il versante settentrionale del massiccio carbonatico, le cui propaggini si estendono fino ai 1000-1500 m del fondovalle, conserva ben [&#8230;]</p>
<p>The post <a rel="nofollow" href="https://www.corradoventurini.it/cor/cordoni-morenici-presso-valbertad-lanza/">Cordoni morenici presso Valbertad (Lanza)</a> appeared first on <a rel="nofollow" href="https://www.corradoventurini.it/cor">Corrado Venturini</a>.</p>
]]></description>
		<wfw:commentRss>https://www.corradoventurini.it/cor/cordoni-morenici-presso-valbertad-lanza/feed/</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>The Late Quaternary evolution of the Friuli upper plain</title>
		<link>https://www.corradoventurini.it/cor/the-late-quaternary-evolution-of-the-friuli-upper-plain/</link>
		<comments>https://www.corradoventurini.it/cor/the-late-quaternary-evolution-of-the-friuli-upper-plain/#comments</comments>
		<pubDate>Fri, 24 May 2013 15:00:46 +0000</pubDate>
		<dc:creator><![CDATA[Conradus]]></dc:creator>
				<category><![CDATA[Pubblicazioni]]></category>
		<category><![CDATA[RICERCA]]></category>
		<category><![CDATA[depositi glaciofluviali]]></category>
		<category><![CDATA[morene]]></category>
		<category><![CDATA[Olocene]]></category>
		<category><![CDATA[Tagliamento]]></category>

		<guid isPermaLink="false">http://www.corradoventurini.it/cvw/?p=1087</guid>
		<description><![CDATA[<p>The central Friuli upper plain and the Tagliamento Moraine Amphitheatre (NE Italy) provide good evidence of how the joint analysis of field survey data and surface digital representations (DEM derived maps) can enable more careful geological mapping and a more accurate analysis of landforms and the related forming processes. During the Late Pleistocene and the [&#8230;]</p>
<p>The post <a rel="nofollow" href="https://www.corradoventurini.it/cor/the-late-quaternary-evolution-of-the-friuli-upper-plain/">The Late Quaternary evolution of the Friuli upper plain</a> appeared first on <a rel="nofollow" href="https://www.corradoventurini.it/cor">Corrado Venturini</a>.</p>
]]></description>
		<wfw:commentRss>https://www.corradoventurini.it/cor/the-late-quaternary-evolution-of-the-friuli-upper-plain/feed/</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
		<item>
		<title>Evoluzione quaternaria della media Val di Vizze &#8211; Pfitschtal (Vipiteno, BZ &#8211; Alpi Aurine)</title>
		<link>https://www.corradoventurini.it/cor/evoluzione-quaternaria-della-media-val-di-vizze-pfitschtal-vipiteno-bz-alpi-aurine/</link>
		<comments>https://www.corradoventurini.it/cor/evoluzione-quaternaria-della-media-val-di-vizze-pfitschtal-vipiteno-bz-alpi-aurine/#comments</comments>
		<pubDate>Wed, 24 Oct 2012 14:37:25 +0000</pubDate>
		<dc:creator><![CDATA[Conradus]]></dc:creator>
				<category><![CDATA[Pubblicazioni]]></category>
		<category><![CDATA[RICERCA]]></category>
		<category><![CDATA[conoidi]]></category>
		<category><![CDATA[DEM]]></category>
		<category><![CDATA[geomorfologia]]></category>
		<category><![CDATA[microrilievo]]></category>
		<category><![CDATA[morene]]></category>
		<category><![CDATA[tardoglaciale]]></category>

		<guid isPermaLink="false">http://www.corradoventurini.it/cvw/?p=1075</guid>
		<description><![CDATA[<p>Con questo lavoro viene affrontata per la prima volta l’evoluzione quaternaria del segmento mediano della Val di Vizze (Pfitschtal) &#8211; situata in provincia di Bolzano (Alpi Aurine) &#8211; il più ricco di evidenze geomorfologiche, distribuite lungo 12 km di fondovalle piatto e sovralluvionato. L’obiettivo è stato perseguito attraverso il confronto tra numerosi dati geomorfologici e [&#8230;]</p>
<p>The post <a rel="nofollow" href="https://www.corradoventurini.it/cor/evoluzione-quaternaria-della-media-val-di-vizze-pfitschtal-vipiteno-bz-alpi-aurine/">Evoluzione quaternaria della media Val di Vizze &#8211; Pfitschtal (Vipiteno, BZ &#8211; Alpi Aurine)</a> appeared first on <a rel="nofollow" href="https://www.corradoventurini.it/cor">Corrado Venturini</a>.</p>
]]></description>
		<wfw:commentRss>https://www.corradoventurini.it/cor/evoluzione-quaternaria-della-media-val-di-vizze-pfitschtal-vipiteno-bz-alpi-aurine/feed/</wfw:commentRss>
		<slash:comments>0</slash:comments>
		</item>
	</channel>
</rss>
