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- Q1734417 subject Q7288240.
- Q1734417 subject Q8393277.
- Q1734417 subject Q8409749.
- Q1734417 subject Q8487713.
- Q1734417 abstract "The Karsdorf Fault (German: Karsdorfer Störung or Karsdorfer Verwerfung) is a striking tectonic fracture line, which is part of the Central Saxon Fault, and is located in the eastern Ore Mountains and the Elbe Valley Slate Mountains. It forms the northern geological boundary of the Eastern Ore Mountains in the district of Sächsische Schweiz-Osterzgebirge with the Elbe zone, where it is adjoined by the Döhlen Basin and the Kreischa Basin.It derives its name from the town of Karsdorf near Rabenau, formerly also known as Wendisch-Carsdorf. As a result the fault line is also called the Wendisch-Carsdorf Fault Line (Wendisch-Carsdorfer Verwerfungslinie) in historical literature.Near Karsdorf the fault line runs in a southeasterly direction where it is geomorphologically outlined by the following clearly visible features: Windberg near Freital, 352 m above NN. Lerchenberg near Possendorf, 425 m Quohrener Kipse, 452 m Hermsdorfer Berg, 447 m Wilisch, 476 m Finckenfang near Maxen, 394 m Lerchenhügel near Hausdorf, 413 m Lederberg near Schlottwitz, 446 mSouth of the fracture line is an almost level wooded area with remnants of sandstone - the Dippoldiswald and Hirschbach Heaths - which are drained by the Oelsabach, Hirschbach and Lockwitzbach. These woodland areas are part of the Cretaceous Elbe Sandstone and are regionally important for their water supply. The oldest sections of these relicts belong to the earliest Cretaceous deposits (Niederschöna Formation) in the Dresden region. They are separated from the main Elbe Valley chalk region by the Karsdorf Fault.".
- Q1734417 thumbnail Wilisch.jpg?width=300.
- Q1734417 wikiPageWikiLink Q13085.
- Q1734417 wikiPageWikiLink Q1325424.
- Q1734417 wikiPageWikiLink Q1564654.
- Q1734417 wikiPageWikiLink Q20306.
- Q1734417 wikiPageWikiLink Q2035448.
- Q1734417 wikiPageWikiLink Q211396.
- Q1734417 wikiPageWikiLink Q2307625.
- Q1734417 wikiPageWikiLink Q4198.
- Q1734417 wikiPageWikiLink Q44626.
- Q1734417 wikiPageWikiLink Q6323.
- Q1734417 wikiPageWikiLink Q6696.
- Q1734417 wikiPageWikiLink Q6787.
- Q1734417 wikiPageWikiLink Q6807.
- Q1734417 wikiPageWikiLink Q6811.
- Q1734417 wikiPageWikiLink Q7288240.
- Q1734417 wikiPageWikiLink Q8218.
- Q1734417 wikiPageWikiLink Q8393277.
- Q1734417 wikiPageWikiLink Q8409749.
- Q1734417 wikiPageWikiLink Q8487713.
- Q1734417 comment "The Karsdorf Fault (German: Karsdorfer Störung or Karsdorfer Verwerfung) is a striking tectonic fracture line, which is part of the Central Saxon Fault, and is located in the eastern Ore Mountains and the Elbe Valley Slate Mountains.".
- Q1734417 label "Karsdorf Fault".
- Q1734417 depiction Wilisch.jpg.