Zobrazeno 1 - 10
of 23
pro vyhledávání: '"Marc Ostermann"'
Autor:
Matthias Themessl, Katharina Enigl, Stefan Reisenhofer, Judith Köberl, Dominik Kortschak, Steffen Reichel, Marc Ostermann, Stefan Kienberger, Dirk Tiede, David N. Bresch, Thomas Röösli, Dagmar Lehner, Chris Schubert, Andreas Pichler, Markus Leitner, Maria Balas
Publikováno v:
Geosciences, Vol 12, Iss 8, p 283 (2022)
Loss and damage databases are essential tools within the disaster risk management cycle for making informed decisions. However, even in data-rich countries such as Austria, no consistent and curated multi-hazard database is available. Based on the re
Externí odkaz:
https://doaj.org/article/53d7905bc41c45a3b852437a78de3945
Autor:
Filippo Vecchiotti, Anna Sara Amabile, Salvatore Clemente, Marc Ostermann, Gianfranco Nicodemo, Dario Peduto
Publikováno v:
Geosciences, Vol 12, Iss 7, p 256 (2022)
This paper focuses on the study of the Vögelsberg landslide located in the municipality of Wattens (Tyrol, Austria), which reactivated in 2016, causing damages to nearby buildings and infrastructures. Since the date of reactivation, a modern monitor
Externí odkaz:
https://doaj.org/article/2097564d19bc411797d349aed4023254
Landslide dams are counted as one of the most destructive mountain hazards. They pose flood hazards downstream and damming effects upstream. Assessing their stability requires either a detailed case study or relying on geomorphic indices. A case-stud
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::08cf8214ffbb05183a35e0dab132b66e
https://doi.org/10.5194/egusphere-egu23-7131
https://doi.org/10.5194/egusphere-egu23-7131
Autor:
Franz Blauensteiner, Anne Hormes, Louise Mary Vick, Christina Rechberger, Thomas Sausgruber, Marc S. Adams, Christian Zangerl, Marc Ostermann, Christine Fey, Anna Sara Amabile, Christian Demmler, Filippo Vecchiotti
Publikováno v:
Geomechanics and Tunnelling. 13:88-102
Displacement rates of mountain slope deformations that can affect entire valley mountain flanks are often measured spatially distributed in‐situ without spatial significance. The spatially explicit measurement and recording of time series of slope
Publikováno v:
Geomorphology. 415:108403
Autor:
Filippo Vecchiotti, Erik Kuschel, Christian Zangerl, Wolfgang Straka, Anna Sara Amabile, Arben Kociu, Gerald Valentin, Marc Ostermann
In the year 2019, at Kartais (Hüttschlag, Austria) parts of an approximately 100 m high and fractured rock wall mainly composed of calcareous-mica-schists became unstable and collapsed two times. The first failure event was a wedge failure and occur
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5db28ecbe49a9452d037afe0579428f6
https://doi.org/10.5194/egusphere-egu2020-20693
https://doi.org/10.5194/egusphere-egu2020-20693
Autor:
Carlotta Guardiani, Amrit Dhakal, Marc Ostermann, A. Schiller, Filippo Vecchiotti, Robert Supper, Megh Raj Dhital, Anna Sara Amabile, Bharat Raij Pant
Continuous INSAR-monitoring of slow mass movements in the surrounding of fast (m/year) or acute processes can deliver important data complementing geomorphologic information in order to understand the broader dynamic context in which a landslide is s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f290a3be145cb7d6649aaac488e6e868
https://doi.org/10.5194/egusphere-egu2020-21875
https://doi.org/10.5194/egusphere-egu2020-21875
Autor:
Diethard Sanders, Marc Ostermann, Jürgen Konzett, Bastian Joachim-Mrosko, Peter Tropper, Julian Lanthaler
The P-T conditions in extremely-rapid gravity-driven rockslides are difficult to constrain from the descended rock mass itself. Here, we report mineralogical observations from the Koefels rockslide and their interpretation. The Koefels event – happ
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cc630b1c9df2c7855e6111a077dd3a0f
https://doi.org/10.5194/egusphere-egu2020-4831
https://doi.org/10.5194/egusphere-egu2020-4831
Publikováno v:
Landslides. 15:2243-2254
The steep, south facing slopes of the central Vinschgau (Val Venosta, South Tyrol, northern Italy) are characterized by deep-seated compound rockslides affecting 51 km2 and reaching beneath the Quaternary valley fill. Morphological features include d