Francesco Troiani
Biographic Data
| ID | 8536504 |
|---|---|
| NAME | Francesco Troiani |
| GIVEN NAMES | Francesco |
| FAMILY NAME | Troiani |
| SIGNATURE | TROIANI F |
| AFFILIATIONS | Sapienza University of Rome |
| ORCID | 0000-0002-4554-1332 |
| VERIFIED | Yes |
| TOTAL WORKS | 6 |
| TOTAL CITATIONS | 0 |
| AUTHOR COUNT | 6 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2012 |
| LATEST PUBLICATION YEAR | 2026 |
| H-INDEX | 0 |
Spatio-temporal variability of landslides as indicator of climate change impact
Ground instabilities such as landslides, subsidence, sinkholes, and soil liquefaction are highly sensitive to climate change. In Italy, these phenomena represent a major component of hydrogeological risk, particularly in mountainous and hilly regions where recent extreme events have highlighted the growing influence of climatic stressors on slope instability. Intense and prolonged rainfall acts both as a preparatory factor, gradually weakening sl…
Deep-Seated Gravitational Slope Deformations in Molise region (Italy)
This paper focuses on Deep-Seated Gravitational Slope Deformations (DSGSDs) identified in the Molise region (Italy), along the central-southern sector of the Apennines chain. These phenomena were detected and mapped through a combination of aerial-photo interpretation, morphological analyses, and field surveys, integrated through satellite SAR interferometry (InSAR). The obtained general map is organized in different sections: inventory map with …
Geomorphology of the lower Mesopotamian plain at Tell Zurghul archaeological site
The landscape of the Lower Mesopotamia Plain (LMP) has been moulded by water-related processes, consequently, its Holocene geomorphic evolution has been strictly connected to the fluvial process and the anthropogenic water management since 8000 BC. About 6000 years ago, during the maximum marine ingression, the modern cities of Nasiriyah and Al-Amara were close to the Persian Gulf shoreline. Successively, the Tigris and Euphrates developed two wi…
SLiX
The stream length-gradient (SL) index is widely used in geomorphological studies aimed at detecting knickzones, which are extensive along-stream deviations from the typical concave-up shape assumed for stream longitudinal profiles at steady-state conditions. In particular, SL was practical for identifying anomalous gradients along bedrock stream channels in mountainous catchments. This work presents the GIS toolbox SLiX designed to extract values…
Rockfall runout, Mount Cimone area, Emilia-Romagna Region, Italy
Numerous mass movements of different typology characterize both mountainous and piedmont sectors of the Emilia-Romagna Region (Apennine chain, North Italy). Although a less spatially frequent landslide typology within the region, rock falls represent severe threats to buildings, roads and persons due to their high propagation velocity. This paper presents an extract of the Emilia-Romagna regional map of the rock fall runout areas at a scale of 1:…
Geomorphological map of the Montelago area (North Marche Apennines, central Italy)
The hamlet of Montelago (‘Mountain of the Lake’) lies within the northern Marche Apennines close to the watershed of Fosso del Lago (‘Stream of the Lake’): both Italian toponyms clearly suggest the presence of a paleolake. Official geological maps reported lacustrine sediments within the upper basin of the Fosso del Lago stream, where outcrops of lacustrine sediments have also been noted for about five decades. The nineteenth-century Gregorian ca…
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Geomorphological map of the Montelago area (North Marche Apennines, central Italy)
The hamlet of Montelago (‘Mountain of the Lake’) lies within the northern Marche Apennines close to the watershed of Fosso del Lago (‘Stream of the Lake’): both Italian toponyms clearly suggest the presence of a paleolake. Official geological maps reported lacustrine sediments within the upper basin of the Fosso del Lago stream, where outcrops of lacustrine sediments have also been noted for about five decades. The nineteenth-century Gregorian ca…
Rockfall runout, Mount Cimone area, Emilia-Romagna Region, Italy
Numerous mass movements of different typology characterize both mountainous and piedmont sectors of the Emilia-Romagna Region (Apennine chain, North Italy). Although a less spatially frequent landslide typology within the region, rock falls represent severe threats to buildings, roads and persons due to their high propagation velocity. This paper presents an extract of the Emilia-Romagna regional map of the rock fall runout areas at a scale of 1:…
SLiX
The stream length-gradient (SL) index is widely used in geomorphological studies aimed at detecting knickzones, which are extensive along-stream deviations from the typical concave-up shape assumed for stream longitudinal profiles at steady-state conditions. In particular, SL was practical for identifying anomalous gradients along bedrock stream channels in mountainous catchments. This work presents the GIS toolbox SLiX designed to extract values…
Deep-Seated Gravitational Slope Deformations in Molise region (Italy)
This paper focuses on Deep-Seated Gravitational Slope Deformations (DSGSDs) identified in the Molise region (Italy), along the central-southern sector of the Apennines chain. These phenomena were detected and mapped through a combination of aerial-photo interpretation, morphological analyses, and field surveys, integrated through satellite SAR interferometry (InSAR). The obtained general map is organized in different sections: inventory map with …
Geomorphology of the lower Mesopotamian plain at Tell Zurghul archaeological site
The landscape of the Lower Mesopotamia Plain (LMP) has been moulded by water-related processes, consequently, its Holocene geomorphic evolution has been strictly connected to the fluvial process and the anthropogenic water management since 8000 BC. About 6000 years ago, during the maximum marine ingression, the modern cities of Nasiriyah and Al-Amara were close to the Persian Gulf shoreline. Successively, the Tigris and Euphrates developed two wi…
Spatio-temporal variability of landslides as indicator of climate change impact
Ground instabilities such as landslides, subsidence, sinkholes, and soil liquefaction are highly sensitive to climate change. In Italy, these phenomena represent a major component of hydrogeological risk, particularly in mountainous and hilly regions where recent extreme events have highlighted the growing influence of climatic stressors on slope instability. Intense and prolonged rainfall acts both as a preparatory factor, gradually weakening sl…
Geography (5 works) · Geology (5 works) · Geomorphology (5 works) · Landslide (5 works) · Landslides and related hazards (5 works) · Cartography (4 works) · Archaeology (3 works) · Paleontology (3 works) · Physical geography (3 works) · Drainage basin (2 works)