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![Plan of the initial landslide area on the <span class="search-highlight">Stože</span> <span class="search-highlight">slope</span> with Mangart Creek va...]()
![Initial debris flow was triggered on the <span class="search-highlight">Stože</span> <span class="search-highlight">slope</span>. Main scarp ( a ), eas...]()
![Toe of the landslide at <span class="search-highlight">Stože</span> <span class="search-highlight">slope</span> (i.e. zone of accumulation) with the in...]()
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![Geological map of the <span class="search-highlight">Stože</span> landslide ( Špacapan &amp; Petrica 2002 ). 1, R...]()
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Image
Plan of the initial landslide area on the Stože slope with Mangart Creek va...
in Debris-flow events at Mt Mangart, Slovenia
> Quarterly Journal of Engineering Geology and Hydrogeology
Published: 29 April 2016
Fig. 4. Plan of the initial landslide area on the Stože slope with Mangart Creek valley, where the first debris-flow mass (from Event 1) accumulated. Subsequent wetting-up through continuing rainfall and stream inflow resulted in the triggering of a catastrophic wet debris flow (Event 2).
Image
Initial debris flow was triggered on the Stože slope. Main scarp ( a ), eas...
in Debris-flow events at Mt Mangart, Slovenia
> Quarterly Journal of Engineering Geology and Hydrogeology
Published: 29 April 2016
Fig. 6. Initial debris flow was triggered on the Stože slope. Main scarp ( a ), east flank ( b ) and west flank ( c ) of the landslide.
Image
Toe of the landslide at Stože slope (i.e. zone of accumulation) with the in...
in Debris-flow events at Mt Mangart, Slovenia
> Quarterly Journal of Engineering Geology and Hydrogeology
Published: 29 April 2016
Fig. 8. Toe of the landslide at Stože slope (i.e. zone of accumulation) with the inflow of Mangart Creek.
Journal Article
Debris-flow events at Mt Mangart, Slovenia
Publisher: Geological Society of London
Published: 29 April 2016
Quarterly Journal of Engineering Geology and Hydrogeology (2016) 49 (2): 117–124.
...Fig. 4. Plan of the initial landslide area on the Stože slope with Mangart Creek valley, where the first debris-flow mass (from Event 1) accumulated. Subsequent wetting-up through continuing rainfall and stream inflow resulted in the triggering of a catastrophic wet debris flow (Event 2). ...
FIGURES
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Image
Geological map of the Stože landslide ( Špacapan & Petrica 2002 ). 1, R...
in Debris-flow events at Mt Mangart, Slovenia
> Quarterly Journal of Engineering Geology and Hydrogeology
Published: 29 April 2016
Fig. 3. Geological map of the Stože landslide ( Špacapan & Petrica 2002 ). 1, Rockfall; 2, slope gravel; 3, moraine with clay; 4, moraine with 5, dolomite; 6, Julian–Tuvalian calcareous marl; 7, Julian–Tuvalian dolomite limestone and marlstone; 8, Julian–Tuvalian dolomite and limestone; 9
Journal Article
Hydrogeochemistry in landslide research: a review
Publisher: Société Géologique de France
Published: 01 March 2007
Bulletin de la Société Géologique de France (2007) 178 (2): 113–126.
... the hydrological processes in landslide triggering. Landslides are well known for their data shortage; especially in case the hydrogeology is heterogeneous and difficult to measure. In this article we analyse the impact hydrogeochemical processes has on physical properties of the soil material and rock slopes, i.e...
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