Lusatian Fault

This article includes a list of references, related reading, or external links, but its sources remain unclear because it lacks inline citations. Please help improve this article by introducing more precise citations. (April 2012) (Learn how and when to remove this message)

The Lusatian Fault (German: Lausitzer Verwerfung), formerly Lusatian Overthrust (Lausitzer Überschiebung), is the most important geological disturbance zone between the Elbe valley and the Giant Mountains. It is a fault that separates the granite of Lusatia from the Cretaceous sandstones of North Bohemia to the south. It is assumed that there was a fault throw of several hundred metres whereby the northern block was uplifted or upthrust relative to the southern block.