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PN Torres del Paine | Turbidite rocks

WI_ch205k.jpg

Two layers of sedimentary rocks originating from the consolidation of mainly fine-grained deposits that were transported from a continental shelf down into the deep sea by so-called turbidity flows. Later on, these rocks were uplifted and tilted.

Location
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Created
on Wednesday 21 February 2018 by Martin Mergili
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3364 visits, CC BY-NC-SA 4.0 DEED license