Fig. 5From: On the pre-history of the turbidite concept: an Alpine perspective on occasion of the 70th anniversary of Kuenen’s 1948 landmark talkIdeal sections (both with and without vertical exaggeration) of an island arc and the corresponding foredeep (Horn 1914, 433). Note that Horn explicitly interpreted flysch (“Grauer Schlick (= Flysch)”) as a deepwater sediment formed by means of subaquatic slide and slump movementsBack to article page