Articles | Volume 74, issue 2
https://doi.org/10.5194/egqsj-74-301-2025
https://doi.org/10.5194/egqsj-74-301-2025
Research article
 | 
24 Nov 2025
Research article |  | 24 Nov 2025

Sediment storage quantification in the Black Forest highlights tectonic influence on typically wide and shallow valleys

Annette Sophie Bösmeier and Jan Henrik Blöthe

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Cited articles

Akaike, H.: Information theory and an extension of the maximum likelihood principle, in: 2nd Int. Symp. Inf. Theory, edited by: Petrov, B. N. and Csaki, F., Akademiai Kiado, Budapest, 267–281, 1973. 
Ardies, G. W., Dalrymple, R. W., and Zaitlin, B. A.: Controls on the Geometry of Incised Valleys in the Basal Quartz Unit (Lower Cretaceous), Western Canada Sedimentary Basin, J. Sediment. Res., 72, 602–618, https://doi.org/10.1306/032101720602, 2002. 
Behnia, P. and Blais-Stevens, A.: Landslide susceptibility modelling using the quantitative random forest method along the northern portion of the Yukon Alaska Highway Corridor, Canada, Nat. Hazards, 90, 1407–1426, https://doi.org/10.1007/s11069-017-3104-z, 2018. 
Behrmann, J. H., Hermann, O., Horstmann, M., Tanner, D. C., and Bertrand, G.: Anatomy and kinematics of oblique continental rifting revealed: A three-dimensional case study of the southeast Upper Rhine graben (Germany), AAPG Bull., 87, 1105–1121, https://doi.org/10.1306/02180300153, 2003. 
Blachowski, J.: Application of GIS spatial regression methods in assessment of land subsidence in complicated mining conditions: case study of the Walbrzych coal mine (SW Poland), Nat. Hazards, 84, 997–1014, https://doi.org/10.1007/s11069-016-2470-2, 2016. 
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We estimated the thickness, spatial distribution, and volumes of alluvial valley fills in the southwestern Black Forest utilizing an extensive borehole database to compile local valley cross sections and model sediment depth above bedrock. Our results reveal considerable spatial heterogeneity and underscore the importance of tectonic boundary conditions on the valley infill in addition to further geologic, hydrologic, and climatologic conditions and processes interacting with fluvial dynamics.
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