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                <text>La selce è una roccia sedimentaria composta perlopiù da silice. La silice proviene dai resti scheletrici o gusci di piccoli organismi (es. diatomee, spugne, radiolari). Si tratta quindi di quarzo microcristallino che tende solitamente a concentrarsi in forma di lenti o noduli all’interno di strati calcarei; è estremamente compatta e, per la sua tendenza a rompersi generando margini translucidi e taglienti, è stata utilizzata molto dall’uomo preistorico. Il suo colore dipende da elementi accessori quali ossidi presenti nella roccia: se c’è ferro la pietra ha un colore rossiccio, se ha delle tracce di piombo diventa bluastra e se c’è del rame assume un colore verdastro; infine invece se c’è materia organica ha un colore nero. La disponibilità di questo tipo di materiale fu fondamentale per i nostri antenati, poiché la selce oltre a essere un ottimo strumento di taglio, quindi impiegato per la realizzazione di utensili per la caccia, è utilizzabile anche come pietra focaia per l’accensione del fuoco. Anche recentemente (1600-1890) la selce è stata usata come pietra focaia negli accendini e nei fucili antichi.</text>
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&#13;
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        <name> A passion for rocks</name>
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                <text>Audio di due arenarie che si scontrano</text>
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                <text>Luca De Monaco</text>
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            <name>Publisher</name>
            <description>An entity responsible for making the resource available</description>
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                <text>Museo virtuale "Dolom,it"</text>
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                <text>Audio Calcari</text>
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                <text>Audio di due calcari che si scontrano</text>
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        <name>Sassi del Piave</name>
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