Description
The main fault systems in the Zürcher Weinland are the Neuhausen fault and the Wildensbucher flexure. Based on the present knowledge, no significant neo-tectonic activity is expected in the Zürcher Weinland within the next one million years, but a minor reactivation of the Neuhausen fault cannot be ruled out completely.
OPA Category
Category as used in the OPA assessment
Geological processes and events
OPA Number
Number as used in the OPA assessment
2.06
NEA V1 IFEP Reference(s)
Related IFEPs from the NEA V1 IFEP list from 1999
1.2.01, 2.2.04