File:Röthenbach Flysch.JPG

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Deutsch: Aufschluss mit steilgestellter, rhythmisch geschichteter Kalk-Mergel-Tonstein-Wechselfolge der Piesenkopf-Formation (Oberkreide) im Röthenbachtal, Ammergauer Alpen, Bayern. Die Abfolge gehört zum Rhenodanubischen Flysch und damit zum Penninikum. Der Aufschluss ist ein geschütztes Geotop und eines von „Bayerns 100 schönsten Geotopen“.
English: Exposure with steeply tilted, rhythmically bedded limestone-marl-claystone alternation of the Piesenkopf Formation (Upper Cretaceous) in the valley of the Röthenbach creek, Ammergau Alps, Bavaria, Germany. The succession is part of the Rhenodanubian Flysch and thus part of the Penninic domain. The exposure is a protected geotope and is selected one of the „100 most beautiful geotopes of Bavaria“.
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Source Own work
Author Jensibua
Camera location47° 34′ 50″ N, 10° 53′ 28″ E Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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current23:33, 17 March 2014Thumbnail for version as of 23:33, 17 March 20142,848 × 4,272 (8.55 MB)Jensibua (talk | contribs){{Information |Description ={{de|1=Flysch im Röthenbachtal, Ammergauer Alpen, Geotop in Bayern}} |Source ={{own}} |Author =Jensibua |Date =2014-03-09 |Permission = |other_versions = }} {{Location|47|3...

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