File:Ratssteinbruch 1.jpg

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Deutsch: Ratssteinbruch im Plauenschen Grund (Weißeritztal bei/in Dresden), diskordante Überlagerung von oberkarbonischem Monzonit (historisch als Syenit klassifiziert) des Meißner Massivs (paläozoisches Grundgebirge) durch die Schichten der Dölzschen-Formation (oberes Cenoman), gelbliches Basiskonglomerat und auflagernde bläuliche siltige Ton-Mergelsteine (plenus-Pläner), der Sächsisch-Böhmischen Kreide (mesozoisches Tafeldeckgebirge).[1]
English: Quarry called “Ratssteinbruch” at Plauenscher Grund (gorge-like valley of the river Weißeritz nearby/in the city of Dresden, Saxony, Germany), Upper Carboniferous Monzonite (historically identified as Syenite) of the Meißen Massif (Paleozoic basement) unconformably overlain by Upper Cenomanian beds of the Dölzschen Formation, yellowish basal conglomerate and overlying bluish silty clay-marlstone (“plenus-Pläner”) of the Saxo-Bohemian Cretaceous Basin (Mesozoic platform).[1]
  1. a b stratigraphy and lithology according to Markus Wilmsen, Birgit Niebuhr: Stratigraphie und Ablagerungsbedingungen der Kreide in Sachsen (Elbtal-Gruppe, Cenomanium–Unterconiacium). Geologica Saxonica 60(2):347–369 (PDF 5.2 MB), see pp. 355–357 therein
Date Taken on 3 October 2014
Source Self-photographed
Author Dryhand58
Object location51° 01′ 33.47″ N, 13° 41′ 57.29″ E Kartographer map based on OpenStreetMap.View this and other nearby images on: OpenStreetMapinfo

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Attribution: Dryhand58
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Date/TimeThumbnailDimensionsUserComment
current21:06, 29 October 2014Thumbnail for version as of 21:06, 29 October 20142,496 × 1,664 (4.17 MB)Dryhand58 (talk | contribs)User created page with UploadWizard

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