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Sesia Lanzo Zone
Eclogitic micaschists complex made through genetic process: regional metamorphism in eclogitic facies
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Chenaillet unit
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Zermatt-Saas Unit
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Casletto bridge
Outerop of "Cenerigneiss", rocks that derive from the metamorphism of a sedimentary rock, probably from a conglomerate, originating from a submarine landslide along an active continental margin.
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Orthogneiss of Jiezera Massif
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White granite of Montorfano
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Megabreccia (Volcanites and volcanoclastites)
Among the fragments forming it, it is even possible to find pieces of the ancient continental crust, also shattered by the explosion, such as the so-called Lake Shale, rocks recognisable by their silvery glow and characteristic foliation.
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Ivrea Verbano Zone, Basal Complex
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Low Susa Valley Serpentinite and Peridotites
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Mica schists lens in Borgone Metagranite
lenticular bodies of silvery micaschists** (1) embedded in metagranite (2) and strongly deformed, with thicknesses varying from a few decimeters to a few metres.
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Dora Maira Unit
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Gravelly sands
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sand
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Sands
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sand
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silts and organic substances
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Rezerwat Meteoryt Morasko
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sand and clay
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Bobrowe Skały, Piastów
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Skałka Teściowej
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natural geological exposure
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Granite rocks
Group of rocks made out of granite
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Miedzyzdroje's aeolian sands
A series of aeolian sands (2-15 m)
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Miedzyzdroje's fluvioglacial level
Series of fluvioglacial (fluvioglacial) sandy and gravel formations of varying thickness
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Vistula glaciation clay till level
yellow-brown in color, up to 3 m thick, associated with the youngest thrust of the ice sheet on this area (Vistula glaciation, North Polish, Pomeranian phase of the glaciation Baltic, 14-12 thousand years ago)