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                  <text>Campione di Pietra Verde detta “di Livinallongo”</text>
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                  <text>Estratto da “Carta Geologica d’Italia, Foglio 046 “Longarone”, la freccia rossa che punta il viola puntinato indica dove affiora la Formazione di Buchenstein</text>
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                <text>Museo di geologia, paleontologia e mineralogia delle Dolomiti agordine</text>
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              <text>L Crep Vert</text>
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              <text>&lt;p&gt;&lt;span style="font-weight: 400;"&gt;Sempre nella serie dei nomi evocativi si situa &lt;/span&gt;&lt;i&gt;&lt;span style="font-weight: 400;"&gt;L Crep Vert&lt;/span&gt;&lt;/i&gt;&lt;span style="font-weight: 400;"&gt;: il dirupo verde, parola che ha una derivazione antichissima, addirittura prelatina.&amp;nbsp;&lt;/span&gt;&lt;/p&gt;&#13;
&lt;p&gt;&lt;span style="font-weight: 400;"&gt;Deriva, infatti dall’indoeuropeo prelatino &lt;/span&gt;&lt;i&gt;&lt;span style="font-weight: 400;"&gt;*krepp&lt;/span&gt;&lt;/i&gt;&lt;span style="font-weight: 400;"&gt; ‘pietra, roccia’ e dal latino &lt;/span&gt;&lt;i&gt;&lt;span style="font-weight: 400;"&gt;viridis&lt;/span&gt;&lt;/i&gt;&lt;span style="font-weight: 400;"&gt; ‘verde’ = dirupo verde (De Nardin e Tomasi, 2011)&lt;/span&gt;&lt;/p&gt;&#13;
&lt;p&gt;&lt;i&gt;&lt;span style="font-weight: 400;"&gt;Ciamà cossita perché che ven fora crepe de la Pietra Verde da la Formazion de Buchestein: vete de tufit e cinerit verde che fazile le ven da atività volcanoclastiche de fora da l’area dolomitica d’encuoi &lt;/span&gt;&lt;/i&gt;&lt;span style="font-weight: 400;"&gt;(trad. italiana: così chiamata poiché affiorano rocce della Pietra Verde della Formazione di Buchenstein: strati di tufiti e cineriti verdi che probabilmente derivano da attività vulcanoclastiche esterne all’attuale area dolomitica)&lt;br /&gt;&lt;br /&gt;&lt;/span&gt;&lt;/p&gt;&#13;
&lt;p&gt;&lt;b&gt;Didascalie immagini&lt;/b&gt;&lt;span style="font-weight: 400;"&gt;&lt;/span&gt;&lt;/p&gt;&#13;
&lt;p&gt;&lt;span style="font-weight: 400;"&gt;Foto 1: Campione di Pietra Verde detta “di Livinallongo” Foto di&amp;nbsp;&lt;span&gt;Tiziano De Col dall'archivio di Radio Più&lt;/span&gt;&lt;/span&gt;&lt;span style="font-weight: 400;"&gt;&lt;/span&gt;&lt;/p&gt;&#13;
&lt;p&gt;&lt;span style="font-weight: 400;"&gt;Foto 2: Estratto da &lt;/span&gt;&lt;i&gt;&lt;span style="font-weight: 400;"&gt;“&lt;/span&gt;&lt;/i&gt;&lt;span style="font-weight: 400;"&gt;Carta Geologica d’Italia, Foglio 046 “Longarone&lt;/span&gt;&lt;i&gt;&lt;span style="font-weight: 400;"&gt;”,&lt;/span&gt;&lt;/i&gt;&lt;span style="font-weight: 400;"&gt; la freccia rossa che punta il viola puntinato indica dove affiora la Formazione di Buchenstein; Provenienza: ISPRA &lt;/span&gt;&lt;a href="https://www.isprambiente.gov.it/Media/carg/"&gt;&lt;span style="font-weight: 400;"&gt;https://www.isprambiente.gov.it/Media/carg/&lt;/span&gt;&lt;/a&gt;&lt;/p&gt;&#13;
&lt;p&gt;&lt;span style="font-weight: 400;"&gt;&amp;nbsp;&lt;/span&gt;&lt;/p&gt;</text>
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              <text>Davide Conedera</text>
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      <name>Agordino</name>
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      <name>Filoladin</name>
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