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Abstract
Geomorphological indications of tectonic activity in the Danish glacial landscape were pointed out already by Milthers (1916, 1948). He described a conspicuous system of N–S-trending, narrow valleys in central Jylland and interpreted them as fault-generated features (fracture valleys). The valleys occur in the area between Ulstrup and Hammel and in a smaller area near Skjød (Fig. 1). The most significant valley system is found near Hvorslev, and it is here referred to as the Hvorslev lineaments (Fig. 1).
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Edited by Ole Bennike, Adam A. Garde and W. Stuart Watt
This Review of Survey activities presents a selection of 19 papers reflecting the wide spectrum of activities of the Geological Survey of Denmark and Greenland, including field-based, laboratory and remote sensing studies.
The Survey's activities in Denmark are illustrated by ten articles covering the [...]
