23 results on '"Schlunegger, F."'
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2. Combining amphibious geomorphology with subsurface geophysical and geological data: A neotectonic study at the front of the Alps (Bernese Alps, Switzerland)
3. Making stratigraphy in the Anthropocene: climate change impacts and economic conditions controlling the supply of sediment to Lake Geneva
4. Bedrock sculpting under an active alpine glacier revealed from cosmic-ray muon radiography
5. The geomorphology and morphometry of the banded terrain in Hellas basin, Mars
6. Impact of an abrupt climate change on sediment distribution from source to sink, PETM, Southern Pyrenees (Spain)
7. Review of Alpine denudation rates from detrital 10Be concentrations
8. Combined Flow Abstraction and Climate Change Impacts on an Aggrading Alpine River
9. An ice-rich flow origin for the banded terrain in the Hellas basin, Mars
10. First measurement of ice‐bedrock interface of alpine glaciers by cosmic muon radiography
11. On the potential for regolith control of fluvial terrace formation in semi-arid escarpments
12. Complex geomorphologic assemblage of terrains in association with the banded terrain in Hellas basin, Mars
13. Patterns of landscape form in the upper Rhône basin, Central Swiss Alps, predominantly show lithologic controls despite multiple glaciations and variations in rock uplift rates
14. Immediate and delayed signal of slab breakoff in Oligo/Miocene Molasse deposits from the European Alps
15. On the potential for regolith control of fluvial terrace formation in semi-arid escarpments
16. Efficiency of frost-cracking processes through space and time: An example from the eastern Italian Alps
17. On the potential for regolith control of fluvial terrace formation in semi-arid escarpments.
18. Climate vs. tectonics: the competing roles of Late Oligocene warming and Alpine orogenesis in constructing alluvial megafan sequences in the North Alpine foreland basin.
19. Overdeepenings in the Swiss plateau: U-shaped geometries underlain by inner gorges.
20. Fast long-term denudation rate of steep alpine headwalls inferred from cosmogenic 36 Cl depth profiles.
21. 10 Be-inferred paleo-denudation rates imply that the mid-Miocene western central Andes eroded as slowly as today.
22. Link between concentrations of sediment flux and deep crustal processes beneath the European Alps.
23. Slab rollback orogeny in the Alps and evolution of the Swiss Molasse basin.
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