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- Franconian_Line abstract "The Franconian Line (German: Fränkische Linie) is a geological fault in south-eastern Germany that forms the border between the South German Scarplands in the west and the Fichtel Mountains in the east.The Franconian Line was formed as part of the Variscan orogenesis and was most active between 100 and 50 million years ago, when the Fichtel, with its blocks of Hercynian granite, pre-Hercynian gneissess and Palaeozoic metasedimentary rocks were uplifted above its forelands that were later filled with Mesozoic-Tertiary sediments. The vertical displacement is as least 1,000 metres (3,300 ft) near Wirsberg and in some cases maybe close to 10,000 metres (33,000 ft).".
- Franconian_Line thumbnail Fränkische_Linie.jpg?width=300.
- Franconian_Line wikiPageID "27328437".
- Franconian_Line wikiPageLength "993".
- Franconian_Line wikiPageOutDegree "16".
- Franconian_Line wikiPageRevisionID "670068172".
- Franconian_Line wikiPageWikiLink Category:South_German_Scarplands.
- Franconian_Line wikiPageWikiLink Category:Tectonics.
- Franconian_Line wikiPageWikiLink Fault_(geology).
- Franconian_Line wikiPageWikiLink Fichtel_Mountains.
- Franconian_Line wikiPageWikiLink Geological_fault.
- Franconian_Line wikiPageWikiLink Gneiss.
- Franconian_Line wikiPageWikiLink Granite.
- Franconian_Line wikiPageWikiLink Hercynian.
- Franconian_Line wikiPageWikiLink Mesozoic.
- Franconian_Line wikiPageWikiLink Palaeozoic.
- Franconian_Line wikiPageWikiLink Paleozoic.
- Franconian_Line wikiPageWikiLink Sediment.
- Franconian_Line wikiPageWikiLink Sedimentary_rock.
- Franconian_Line wikiPageWikiLink Sediments.
- Franconian_Line wikiPageWikiLink South_German_Scarplands.
- Franconian_Line wikiPageWikiLink Tertiary.
- Franconian_Line wikiPageWikiLink Variscan.
- Franconian_Line wikiPageWikiLink Variscan_orogeny.
- Franconian_Line wikiPageWikiLink Wirsberg.
- Franconian_Line wikiPageWikiLink File:Fränkische_Linie.jpg.
- Franconian_Line wikiPageWikiLinkText "Franconian Line".
- Franconian_Line hasPhotoCollection Franconian_Line.
- Franconian_Line wikiPageUsesTemplate Template:Bavaria-geo-stub.
- Franconian_Line wikiPageUsesTemplate Template:Convert.
- Franconian_Line wikiPageUsesTemplate Template:Coord_missing.
- Franconian_Line wikiPageUsesTemplate Template:Lang-de.
- Franconian_Line subject Category:South_German_Scarplands.
- Franconian_Line subject Category:Tectonics.
- Franconian_Line hypernym Fault.
- Franconian_Line type Article.
- Franconian_Line type Place.
- Franconian_Line type Article.
- Franconian_Line comment "The Franconian Line (German: Fränkische Linie) is a geological fault in south-eastern Germany that forms the border between the South German Scarplands in the west and the Fichtel Mountains in the east.The Franconian Line was formed as part of the Variscan orogenesis and was most active between 100 and 50 million years ago, when the Fichtel, with its blocks of Hercynian granite, pre-Hercynian gneissess and Palaeozoic metasedimentary rocks were uplifted above its forelands that were later filled with Mesozoic-Tertiary sediments. ".
- Franconian_Line label "Franconian Line".
- Franconian_Line sameAs Fränkische_Linie.
- Franconian_Line sameAs m.0by0vg1.
- Franconian_Line sameAs Q1471197.
- Franconian_Line sameAs Q1471197.
- Franconian_Line wasDerivedFrom Franconian_Line?oldid=670068172.
- Franconian_Line depiction Fränkische_Linie.jpg.
- Franconian_Line isPrimaryTopicOf Franconian_Line.