Feeding the hungry river: Fluvial morphodynamics and the entrainment of artificially inserted sediment at the dammed river Isar, Eastern Alps, Germany

Geomorphology ◽  
2017 ◽  
Vol 291 ◽  
pp. 128-142 ◽  
Author(s):  
Tobias Heckmann ◽  
Florian Haas ◽  
Judith Abel ◽  
Andreas Rimböck ◽  
Michael Becht
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2000 ◽  
Vol 151 (9) ◽  
pp. 325-335 ◽  
Author(s):  
Giovanni Bovio

Important forest fire prevention developments of the Lombardy, Piedmont and Aosta Valley regions are highlighted in this study and a certain number of activities considered able to improve the situation are proposed.


Author(s):  
Andrei Grachev ◽  
H. A. Kollmann ◽  
O. A. Korchagin ◽  
D. M. Pechersky ◽  
V. A. Tsel'movich
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2021 ◽  
Author(s):  
Qingbin Guan ◽  
Yongjiang Liu ◽  
Franz Neubauer ◽  
Sanzhong Li ◽  
Johann Genser ◽  
...  

Geosciences ◽  
2021 ◽  
Vol 11 (8) ◽  
pp. 331
Author(s):  
Selçuk Aksay ◽  
Susan Ivy-Ochs ◽  
Kristina Hippe ◽  
Lorenz Grämiger ◽  
Christof Vockenhuber

The Säntis nappe is a complex fold-and-thrust structure in eastern Switzerland, consisting of numerous tectonic discontinuities and a range of hillslopes prone to landsliding and large slope failures that modify the topography irreversibly. A slope failure, namely the Sennwald rock avalanche, occurred in the southeast wall of this fold-and-thrust structure due to the rock failure of Lower Cretaceous Helvetic limestones along the Rhine River valley. In this research, this palaeolandslide is examined in a multidisciplinary approach for the first time with detection and mapping of avalanche deposits, dynamic run-out modelling and cosmogenic nuclide dating. During the rock failure, the avalanche deposits were transported down the hillslope in a spreading-deck fashion, roughly preserving the original stratigraphic sequence. The distribution of landslide deposits and surface exposure age of the rock failure support the hypothesis that the landslide was a single catastrophic event. The 36Cl surface exposure age of avalanche deposits indicates an age of 4.3 ± 0.5 ka. This time coincides with a notably wet climate period, noted as a conditioning factor for landslides across the Alps in the mid-Holocene. The contemporaneity of our event at its location in the Eastern Alps provide additional support for the contention of increased regional seismic activity in mid-Holocene.


2006 ◽  
Vol 414 (1-4) ◽  
pp. 259-282 ◽  
Author(s):  
Alberto Castellarin ◽  
Rinaldo Nicolich ◽  
Roberto Fantoni ◽  
Luigi Cantelli ◽  
Mattia Sella ◽  
...  
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2010 ◽  
Vol 106 (6) ◽  
pp. 967-977 ◽  
Author(s):  
Michaela Sonnleitner ◽  
Ruth Flatscher ◽  
Pedro Escobar García ◽  
Jana Rauchová ◽  
Jan Suda ◽  
...  

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