1.0Geoparco Alpi Carnichehttps://www.geoparcoalpicarniche.org/en/omniahttps://www.geoparcoalpicarniche.org/en/author/omnia/The Hochwipfel formation - Geoparco Alpi Carnicherich600338<blockquote class="wp-embedded-content" data-secret="Gdv1SSs1Cn"><a href="https://www.geoparcoalpicarniche.org/en/geostop/formazione-dellhochwipfel/">The Hochwipfel formation</a></blockquote><iframe sandbox="allow-scripts" security="restricted" src="https://www.geoparcoalpicarniche.org/en/geostop/formazione-dellhochwipfel/embed/#?secret=Gdv1SSs1Cn" width="600" height="338" title="“The Hochwipfel formation” — Geoparco Alpi Carniche" data-secret="Gdv1SSs1Cn" frameborder="0" marginwidth="0" marginheight="0" scrolling="no" class="wp-embedded-content"></iframe><script type="text/javascript">
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https://www.geoparcoalpicarniche.org/wp-content/uploads/2018/01/las-calas-06.jpg525300During the Hercynian (the Upper Carboniferous) orogeny, the Carnic basin was characterized by strong tectonic movements that led to the deepening of some areas and the lifting of others. Submarine landslides thus led to the accumulation of sediments with variable granulometry including breccias, conglomerates, sandstones and pelites with characteristics that …