1.0Geoparco Alpi Carnichehttps://www.geoparcoalpicarniche.org/en/Daniela De Pratohttps://www.geoparcoalpicarniche.org/en/author/daniela/Karst phenomena near the Lander Bivouac - Geoparco Alpi Carnicherich600338<blockquote class="wp-embedded-content" data-secret="tvU4tj0SxB"><a href="https://www.geoparcoalpicarniche.org/en/geostop/fenomeni-carsici/">Karst phenomena near the Lander Bivouac</a></blockquote><iframe sandbox="allow-scripts" security="restricted" src="https://www.geoparcoalpicarniche.org/en/geostop/fenomeni-carsici/embed/#?secret=tvU4tj0SxB" width="600" height="338" title="“Karst phenomena near the Lander Bivouac” — Geoparco Alpi Carniche" data-secret="tvU4tj0SxB" 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/2018/04/geostop4-bivacco-lander.jpg1100732The Lander Bivouac is located on a small plateau at about 1175 m a.s.l. Near the bivouac there are limestone rocks belonging to the Val Badia Member of the Werfen Formation. Here, pay close attention to the various surface morphologies linked to karst phenomena. One can observe both medium-sized forms …