1.0Geoparco Alpi Carnichehttps://www.geoparcoalpicarniche.org/en/omniahttps://www.geoparcoalpicarniche.org/en/author/omnia/The limestone of the Findenig Formation - Geoparco Alpi Carnicherich600338<blockquote class="wp-embedded-content" data-secret="xuYEdHcmjC"><a href="https://www.geoparcoalpicarniche.org/en/geostop/i-calcari-della-formazione-del-findenig/">The limestone of the Findenig Formation</a></blockquote><iframe sandbox="allow-scripts" security="restricted" src="https://www.geoparcoalpicarniche.org/en/geostop/i-calcari-della-formazione-del-findenig/embed/#?secret=xuYEdHcmjC" width="600" height="338" title="“The limestone of the Findenig Formation” — Geoparco Alpi Carniche" data-secret="xuYEdHcmjC" frameborder="0" marginwidth="0" marginheight="0" scrolling="no" class="wp-embedded-content"></iframe><script>
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https://www.geoparcoalpicarniche.org/wp-content/uploads/2018/02/HP17_DSC03474_2-1280.jpg1280960The limestone of the Findenig Formation was formed from a calcareous mud rich in clay, which was deposited in deep seas during the Devonian, about 390 million years ago. It contains mainly shells and skeletons of microorganisms (plankton). In the rock, dark red clayey layers alternate with lighter layers in …