- Author
- Year
- 2012
- host editors
-
K. Brandt
- Title
- Das Absinken der Oberfläche im Treenetal während des Spätholozäns
- Book title
- Hollingstedt an der Treene: ein Flusshafen der Wikingerzeit und des Mittelalters für den Transitverkehr zwischen Nord- und Ostsee
- Pages (from-to)
- 401-413
- Publisher
- Neumunster: Wacholtz Verlag
- ISBN
- 9783529018114
- Series
- Schriften der Archäeologischen Landesmuseum, 10
- Document type
- Chapter
- Faculty
- Faculty of Science (FNWI)
- Institute
- Institute for Biodiversity and Ecosystem Dynamics (IBED)
- Abstract
-
The stated lowering of the surface in the valley of the Treene is substantial. According to the height
of the peat located on slopes, a decline of at least 150 cm is computed. A considerable part of the total
drop took place before the drainage operation carried out around the year 1924. It cannot be ruled out
that the damming-up of the Treene in the year 1570 played a major role in the lowering of the surface
(Borger 1998; cf. the contribution by G. J. Borger in this volume). However, even prior to this, drainage
of the bogs had on all accounts been undertaken by man to a limited extent. - Language
- German
- Persistent Identifier
- https://hdl.handle.net/11245/1.375645
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