| 41. | Rhenodanubian flysch : Rhythmic limestone-marl-mudrock alternation of the Piesenkopf Formation ( Late Cretaceous ) in R�thenbachtal, Ostallg�u
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| 42. | The main edifice is constructed on top of the Eocene flysch, although some Cretaceous sediments are also part of the basement.
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| 43. | The best known mountain of this flysch zone is the Riedberger Horn, which is easy to climb from the Riedberg Pass.
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| 44. | The Flysch Belt continues through Bohemia, Slovakia, and Poland, and joins the Moldavian Flysch in the Ukraine and Romania.
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| 45. | The Flysch Belt continues through Bohemia, Slovakia, and Poland, and joins the Moldavian Flysch in the Ukraine and Romania.
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| 46. | Eocene flysch forms the southwest boundary of the catchment area, towards which the catchment basin drains and where the Ombla rises.
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| 47. | These deposits are typically the non-marine alluvial and fluvial sediments of lowlands, as compared to deep-water flysch sediments.
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| 48. | The lower slopes are dominated by younger flysch rocks, which consist of thin beds of graded sandstones intercalated with softer, fissile siltstones.
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| 49. | The northern boundary with the East European craton and Bohemian Massif is well marked by the thrust of nappes of the Carpathian flysch belt.
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| 50. | The flysch basin was shortened and at the northern edge of Iberia, an orogenic wedge formed that moved slowly into the northern foreland.
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