Late Quaternary geology of a potential wind-farm area in the Kattegat, southern Scandinavia
Following the proposal of the offshore Anholt wind-farm project with an energy capacity of 400 megawatt in the Kattegat, southern Scandinavia, an evaluation of the geotechnical properties of the subsurface of the area is required. As a first step to map the seabed geology the Geological Survey of De...
Published in: | Geological Survey of Denmark and Greenland (GEUS) Bulletin |
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Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Geological Survey of Denmark and Greenland (GEUS)
2010
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Subjects: | |
Online Access: | https://geusbulletin.org/index.php/geusb/article/view/4893 https://doi.org/10.34194/geusb.v20.4893 |
Summary: | Following the proposal of the offshore Anholt wind-farm project with an energy capacity of 400 megawatt in the Kattegat, southern Scandinavia, an evaluation of the geotechnical properties of the subsurface of the area is required. As a first step to map the seabed geology the Geological Survey of Denmark and Greenland (GEUS) conducted a geophysical survey (Leth et al. 2009) which, together with cone penetration tests and data from boreholes, lead to a greater understanding of the geological architecture and development of the 144 km2 survey area (Figs 1, 2). |
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