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1 results

  • 16 - Glacially Induced Faults in Germany

  • from Part IV - Glacially Triggered Faulting at the Edge and in the Periphery of the Fennoscandian Shield
  • Edited by Holger Steffen, Odleiv Olesen, Raimo Sutinen
  • Book:
    Glacially-Triggered Faulting
    Published online:
    02 December 2021
    Print publication:
    16 December 2021, pp 283-303

  • Summary

    Recent studies have shown that the low seismicity of northern Germany is characterized by fault activity caused by the decay of the Late Pleistocene (Weichselian) ice sheet. Several faults and fault systems show evidence of neotectonic activity, all of which are oriented parallel to the margin of the Pleistocene ice sheets. The timing of fault movements implies that the seismicity in northern Germany is likely induced by varying lithospheric stress conditions related to glacial isostatic adjustment, and the faults thus can be classified as glacially induced faults. For the Osning, Harz Boundary and Schaabe faults, this is supported by numerical simulation of glacial isostatic adjustment-related stress field changes. Glacial isostatic adjustment is also a likely driver for the historical and parts of the recent fault activity. Glacial isostatic adjustment is also described for the Alps, but it is difficult to clearly distinguish between reactivation of faults in the foreland of the Alps due to the Alpine collision and glacial isostatic adjustment.