Processi paraglaciali su alcuni versanti alpini: i casi di studio della Valle di Slingia (Bz), del Ghiacciaio di Cima Uomo (Tn) e del Bacino del Vauz (Bl).
This PhD thesis has been carried out in the context of a Strategic Project of the University of Padua ("Georisk"), which aim was the study of the geological and hydrological hazards in the north-east of Italy. The project was divided into 5 workpackages (WP) and the PhD study was mainly co...
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Format: | Doctoral or Postdoctoral Thesis |
Language: | Italian |
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Università degli studi di Padova
2014
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Online Access: | http://hdl.handle.net/11577/3423561 |
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ftunivpadovairis:oai:www.research.unipd.it:11577/3423561 2024-04-14T08:18:20+00:00 Processi paraglaciali su alcuni versanti alpini: i casi di studio della Valle di Slingia (Bz), del Ghiacciaio di Cima Uomo (Tn) e del Bacino del Vauz (Bl). Zanoner, Thomas Zanoner, Thomas Carton, Alberto La Rocca, Maria Cristina 2014-01-31 http://hdl.handle.net/11577/3423561 ita ita Università degli studi di Padova http://hdl.handle.net/11577/3423561 info:eu-repo/semantics/openAccess Paraglaciale/Paraglacial DGPV/DSGSDs Rock glacier/Rock glacier Periglaciale/Periglacial Alpi Orientali/Eastern Alps Settore GEO/04 - Geografia Fisica e Geomorfologia info:eu-repo/semantics/doctoralThesis 2014 ftunivpadovairis 2024-03-21T19:56:36Z This PhD thesis has been carried out in the context of a Strategic Project of the University of Padua ("Georisk"), which aim was the study of the geological and hydrological hazards in the north-east of Italy. The project was divided into 5 workpackages (WP) and the PhD study was mainly conducted in the framework of WP1 ("slope processes"). The study focused on the geomorphological evolution of three mountain areas affected by the presence of glaciers at different times. According to the literature, after the glacial mass withdrawal the evolution of these territories is defined "paraglacial evolution". In particular, the study areas are: the Schlinig Valley (Eastern Alps - South Tyrol), the area of Cima Uomo Glacier (Dolomites - Trentino) and the Vauz Basin (Dolomites - Belluno). In the Schlinig Valley the aim was to assess the state of the slopes which are affected by various DSGSDS (Deep Seated Gravitational Slope Deformations). At Cima Uomo the purpose was to understand how the permafrost presence can drive the evolution of the area during and after the deglaciation. Finally, in the Vauz Basin, the aim was to understand the present evolution of this area, which in the past underwent paraglacial modeling processes and modification, as documented by some relict landforms. The detailed study of the three investigated areas allowed to: 1) characterize the current geomorphological processes, 2) understand the past morphological evolution and 3) better understand the developmental status achieved in each area with respect to the paraglacial period. The three study areas highlight the importance of the local topo-climatic factors on the characteristics of paraglacial evolution processes, deposits and landforms respect to the wider scale climatic factors. La presente tesi di Dottorato è stata realizzata nell’ambito di un Progetto Strategico dell’Università degli Studi di Padova (“Georisk”), il quale aveva come obiettivo lo studio dei rischi geologici e idrologici nell’Italia nord orientale. Il Progetto strategico ... Doctoral or Postdoctoral Thesis permafrost Padua Research Archive (IRIS - Università degli Studi di Padova) |
institution |
Open Polar |
collection |
Padua Research Archive (IRIS - Università degli Studi di Padova) |
op_collection_id |
ftunivpadovairis |
language |
Italian |
topic |
Paraglaciale/Paraglacial DGPV/DSGSDs Rock glacier/Rock glacier Periglaciale/Periglacial Alpi Orientali/Eastern Alps Settore GEO/04 - Geografia Fisica e Geomorfologia |
spellingShingle |
Paraglaciale/Paraglacial DGPV/DSGSDs Rock glacier/Rock glacier Periglaciale/Periglacial Alpi Orientali/Eastern Alps Settore GEO/04 - Geografia Fisica e Geomorfologia Zanoner, Thomas Processi paraglaciali su alcuni versanti alpini: i casi di studio della Valle di Slingia (Bz), del Ghiacciaio di Cima Uomo (Tn) e del Bacino del Vauz (Bl). |
topic_facet |
Paraglaciale/Paraglacial DGPV/DSGSDs Rock glacier/Rock glacier Periglaciale/Periglacial Alpi Orientali/Eastern Alps Settore GEO/04 - Geografia Fisica e Geomorfologia |
description |
This PhD thesis has been carried out in the context of a Strategic Project of the University of Padua ("Georisk"), which aim was the study of the geological and hydrological hazards in the north-east of Italy. The project was divided into 5 workpackages (WP) and the PhD study was mainly conducted in the framework of WP1 ("slope processes"). The study focused on the geomorphological evolution of three mountain areas affected by the presence of glaciers at different times. According to the literature, after the glacial mass withdrawal the evolution of these territories is defined "paraglacial evolution". In particular, the study areas are: the Schlinig Valley (Eastern Alps - South Tyrol), the area of Cima Uomo Glacier (Dolomites - Trentino) and the Vauz Basin (Dolomites - Belluno). In the Schlinig Valley the aim was to assess the state of the slopes which are affected by various DSGSDS (Deep Seated Gravitational Slope Deformations). At Cima Uomo the purpose was to understand how the permafrost presence can drive the evolution of the area during and after the deglaciation. Finally, in the Vauz Basin, the aim was to understand the present evolution of this area, which in the past underwent paraglacial modeling processes and modification, as documented by some relict landforms. The detailed study of the three investigated areas allowed to: 1) characterize the current geomorphological processes, 2) understand the past morphological evolution and 3) better understand the developmental status achieved in each area with respect to the paraglacial period. The three study areas highlight the importance of the local topo-climatic factors on the characteristics of paraglacial evolution processes, deposits and landforms respect to the wider scale climatic factors. La presente tesi di Dottorato è stata realizzata nell’ambito di un Progetto Strategico dell’Università degli Studi di Padova (“Georisk”), il quale aveva come obiettivo lo studio dei rischi geologici e idrologici nell’Italia nord orientale. Il Progetto strategico ... |
author2 |
Zanoner, Thomas Carton, Alberto La Rocca, Maria Cristina |
format |
Doctoral or Postdoctoral Thesis |
author |
Zanoner, Thomas |
author_facet |
Zanoner, Thomas |
author_sort |
Zanoner, Thomas |
title |
Processi paraglaciali su alcuni versanti alpini: i casi di studio della Valle di Slingia (Bz), del Ghiacciaio di Cima Uomo (Tn) e del Bacino del Vauz (Bl). |
title_short |
Processi paraglaciali su alcuni versanti alpini: i casi di studio della Valle di Slingia (Bz), del Ghiacciaio di Cima Uomo (Tn) e del Bacino del Vauz (Bl). |
title_full |
Processi paraglaciali su alcuni versanti alpini: i casi di studio della Valle di Slingia (Bz), del Ghiacciaio di Cima Uomo (Tn) e del Bacino del Vauz (Bl). |
title_fullStr |
Processi paraglaciali su alcuni versanti alpini: i casi di studio della Valle di Slingia (Bz), del Ghiacciaio di Cima Uomo (Tn) e del Bacino del Vauz (Bl). |
title_full_unstemmed |
Processi paraglaciali su alcuni versanti alpini: i casi di studio della Valle di Slingia (Bz), del Ghiacciaio di Cima Uomo (Tn) e del Bacino del Vauz (Bl). |
title_sort |
processi paraglaciali su alcuni versanti alpini: i casi di studio della valle di slingia (bz), del ghiacciaio di cima uomo (tn) e del bacino del vauz (bl). |
publisher |
Università degli studi di Padova |
publishDate |
2014 |
url |
http://hdl.handle.net/11577/3423561 |
genre |
permafrost |
genre_facet |
permafrost |
op_relation |
http://hdl.handle.net/11577/3423561 |
op_rights |
info:eu-repo/semantics/openAccess |
_version_ |
1796317794558541824 |