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The Eckskopf is a mountain in dolomitic limestone (Hauptdolomite) and is highly affected by deep reaching mass movement (see tension fissures) due to tensional rebound and solution of gypsum in the subsurface.
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The Eckskopf is a mountain in dolomitic limestone (Hauptdolomite) and is highly affected by deep reaching mass movement (see tension fissures) due to tensional rebound and solution of gypsum in the subsurface.
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