Neues zur pleistozänen Harzvergletscherung

Jürgen Hövermann
Based on an exploratory excavation in the gravels of the Böhrweg at the South-West margin of the Harz (380 m over sea level), surprising results on the structure of the debris at that place were obtained. Structures of solifluc-tion and cryoturbation in the upmost meters of a about 20 m high debris have probably displaced and compressed two marked wet soil formations. Underneath intensive foldings as well as vertical and nearly horizental shear planes can...