Zobrazeno 1 - 10
of 213
pro vyhledávání: '"Overdeepening"'
Autor:
Sebastian Schaller, Michael E. Böttcher, Marius W. Buechi, Laura S. Epp, Stefano C. Fabbri, Natacha Gribenski, Ulrich Harms, Sebastian Krastel, Alina Liebezeit, Katja Lindhorst, Hanna Marxen, Ulli Raschke, David Schleheck, Iris Schmiedinger, Antje Schwalb, Hendrik Vogel, Martin Wessels, Flavio S. Anselmetti
Publikováno v:
Swiss Journal of Geosciences, Vol 115, Iss 1, Pp 1-25 (2022)
Abstract The modern, over 250-m-deep basin of Lake Constance represents the underfilled northern part of an over 400-m-deep, glacially overdeepened trough, which reaches well into the Alps at its southern end. The overdeepening was formed by repeated
Externí odkaz:
https://doaj.org/article/6ef84e3e05724aa791c0a15759e42ae4
Publikováno v:
Data in Brief, Vol 41, Iss , Pp 107934- (2022)
This dataset was obtained over repeated field-trips to the Sierra Nevada Massif and contains the physical parameters of its recognised water-bodies. It therefore defines the general cartography of the area, with data on individual features regarding
Externí odkaz:
https://doaj.org/article/cdd9e18a12674dd2aeac1f8dd92ac9fc
Akademický článek
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Autor:
S.C. Fabbri, C. Affentranger, S. Krastel, K. Lindhorst, M. Wessels, Herfried Madritsch, R. Allenbach, M. Herwegh, S. Heuberger, U. Wielandt-Schuster, H. Pomella, T. Schwestermann, F.S. Anselmetti
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
Probabilistic seismic hazard assessments are primarily based on instrumentally recorded and historically documented earthquakes. For the northern part of the European Alpine Arc, slow crustal deformation results in low earthquake recurrence rates and
Externí odkaz:
https://doaj.org/article/d1f4409e10a448fe8d3443a5ce2368c1
Publikováno v:
Water, Vol 13, Iss 4, p 438 (2021)
At present, there is a lack of detailed understanding on how the factors converging on water variables from mountain areas modify the quantity and quality of their watercourses, which are features determining these areas’ hydrological contribution
Externí odkaz:
https://doaj.org/article/c562ae454d2041cc94add141a7999f00
Akademický článek
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Autor:
Angela M. Gurnell, Peter W. Downs
Publikováno v:
Earth Surface Processes and Landforms. 46:3016-3025
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fc5c00889530c4ebbd1c087f27b8f5ce
https://doi.org/10.1002/esp.5268
https://doi.org/10.1002/esp.5268
Autor:
William J. Higson, Robert G. Bryant, Simon J. Cook, Darrel A. Swift, Daniel Farinotti, Guy D. Tallentire
Publikováno v:
Earth Surface Processes and Landforms, 46 (11)
Evacuation of basal sediment by subglacial drainage is an important mediator of rates of glacial erosion and glacier flow. Glacial erosion patterns can produce closed basins (i.e., overdeepenings) in glacier beds, thereby introducing adverse bed grad
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::634278ccbfdcfa33c82946df4a300619
https://hdl.handle.net/20.500.11850/489064
https://hdl.handle.net/20.500.11850/489064
Autor:
Jonathan L. Carrivick, Jenna L. Sutherland, Matthias Huss, Heather Purdie, Christopher D. Stringer, Michael Grimes, William H.M. James, Andrew M. Lorrey
Publikováno v:
Global and Planetary Change, 211
Global glacier mass loss is causing expansion of proglacial landscapes and producing meltwater that can become impounded as lakes within natural topographic depressions or ‘overdeepenings’. It is important to understand the evolution of these pro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b1a47881ee913eaf4e48cbad42f70e89
https://eprints.whiterose.ac.uk/185676/1/Carrivicketal2022_GLOBPLANCH.pdf
https://eprints.whiterose.ac.uk/185676/1/Carrivicketal2022_GLOBPLANCH.pdf
Akademický článek
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