File:Geotop Gomaringen gtk 4658 P1190140.jpg

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Deutsch: Der aufgelassene Steinbruch zwischen Gomaringen und Hinterweiler ist der Rest eines größeren Steinbruchgeländes in den unteren Schichten der Numismalismergel-Formation (pb1, früher Schwarzjura gamma). Das Profil zeigt einen insgesamt etwa 40 m langen und 7 m hohen Ausschnitt aus dieser Formation im mittleren Unterjura: Kalkmergel und Mergelsteine mit der abschließenden Devoei-Bank, die hier eine Verebnungsfläche verursacht.
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current21:07, 6 May 2020Thumbnail for version as of 21:07, 6 May 20204,000 × 2,248 (3.92 MB)Vux (talk | contribs)Uploaded own work with UploadWizard

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