F Dramis
Biographic Data
| ID | 6434151 |
|---|---|
| NAME | F Dramis |
| GIVEN NAMES | F |
| FAMILY NAME | Dramis |
| SIGNATURE | DRAMIS F |
| AFFILIATIONS | Roma Tre University |
| ORCID | 0000-0001-5931-2656 |
| VERIFIED | Yes |
| TOTAL WORKS | 9 |
| TOTAL CITATIONS | 20 |
| AUTHOR COUNT | 9 |
| EDITOR COUNT | 0 |
| FIRST PUBLICATION YEAR | 2000 |
| LATEST PUBLICATION YEAR | 2022 |
| H-INDEX | 1 |
Permafrost-based geomorphology of the Mt. Foscagno - Mt. Forcellina ridge (Adda – Inn River basins, Central Italian Alps)
The permafrost-based geomorphological map of the Mt. Foscagno–Mt Forcellina ridge (Central Italian Alps) shows the distribution of permafrost probability (high, medium, low probability, and probable absence) obtained by the application of PERMACLIM (Guglielmin et al., 2003), a GIS-based model integrating Digital Elevation Model (DEM) topographic data and the Climatic DataBase (CDB) available from Automatic Weather Stations (AWS). In addition, the…
Limestone, Karst and Tufa Dams in the Western Part of the Mekelle Outlier
Mass Movement Processes and Landforms
Mass movements may be defined as “downslope movements of rock, earth, or soil masses occurring when their resisting forces cannot resist gravitational stress.” The displacing mechanisms include: detachment by newly generated fractures or shear surfaces; fall in free air; sliding over newly generated shear surfaces whose shape is controlled by the mass structure; spreading over a softer subhorizontal material; flow over the slope surface or in a p…
Geology of the Tekeze River basin (Northern Ethiopia)
We present a geologic map of the Tekeze River basin that covers an area of ∼69,000 km2 of northern Ethiopia. The map synthesizes new data collected in two campaigns between March, 2012 and January, 2013 and compiled at a scale of 1:500,000 with published geologic surveys. The map focuses on the main geologic and tectonic features relevant to a modern interpretation of the geologic evolution of northern Ethiopia and as such, it represents an impor…
Geomorphological Map of the Ionian Area between the Trionto and Colognati River Catchments (Calabria, Italy)
Please click here to download the map associated with this article. This paper describes a geomorphological map representing a sector of the Ionian coastal belt, located in north-eastern Calabria, between the catchments of the Trionto and Colognati Rivers. The landforms have been distinguished according to their origin into: a) structural and tectonic-controlled landforms; b) gravity-induced landforms; c) landforms formed by running water; d) coa…
GIS Methodology to Assess Landslide Susceptibility
Please click here to download the map associated with this article. This paper illustrates a geographic information system (GIS) supported methodology for the assessment of landslide susceptibility. The methodology involves four operational steps: survey, site analysis, macroarea analysis and susceptibility analysis. The Survey includes the production (or acquisition) of a large-scale litho-technical map, a large-scale geomorphological map, a det…
Holocene climate phases from buried soils in Tigray (northern Ethiopia)
Holocene climate phases from buried soils in Tigray (northern Ethiopia)
Stratigraphic analysis of alluvial/colluvial sequences and 14 C dating have been used as proxies for Holocene climate changes in the highlands of Tigray (northern Ethiopia). The studied records show alternations of buried soils and peaty–clayey sediments, pointing to wet, stabilization phases, and organic-free colluvium layers resulting from the abrupt occurrence of dry-climate episodes. The 14 C dates, mostly unpublished, cluster in the 11,090–9…
The Environmental History of Tigray (Northern Ethiopia) in the Middle and Late Holocene
The Environmental History of Tigray (Northern Ethiopia) in the Middle and Late Holocene
Holocene climate phases from buried soils in Tigray (northern Ethiopia)
Holocene climate phases from buried soils in Tigray (northern Ethiopia)
Stratigraphic analysis of alluvial/colluvial sequences and 14 C dating have been used as proxies for Holocene climate changes in the highlands of Tigray (northern Ethiopia). The studied records show alternations of buried soils and peaty–clayey sediments, pointing to wet, stabilization phases, and organic-free colluvium layers resulting from the abrupt occurrence of dry-climate episodes. The 14 C dates, mostly unpublished, cluster in the 11,090–9…
Geomorphological Map of the Ionian Area between the Trionto and Colognati River Catchments (Calabria, Italy)
Please click here to download the map associated with this article. This paper describes a geomorphological map representing a sector of the Ionian coastal belt, located in north-eastern Calabria, between the catchments of the Trionto and Colognati Rivers. The landforms have been distinguished according to their origin into: a) structural and tectonic-controlled landforms; b) gravity-induced landforms; c) landforms formed by running water; d) coa…
GIS Methodology to Assess Landslide Susceptibility
Please click here to download the map associated with this article. This paper illustrates a geographic information system (GIS) supported methodology for the assessment of landslide susceptibility. The methodology involves four operational steps: survey, site analysis, macroarea analysis and susceptibility analysis. The Survey includes the production (or acquisition) of a large-scale litho-technical map, a large-scale geomorphological map, a det…
Mass Movement Processes and Landforms
Mass movements may be defined as “downslope movements of rock, earth, or soil masses occurring when their resisting forces cannot resist gravitational stress.” The displacing mechanisms include: detachment by newly generated fractures or shear surfaces; fall in free air; sliding over newly generated shear surfaces whose shape is controlled by the mass structure; spreading over a softer subhorizontal material; flow over the slope surface or in a p…
Geology of the Tekeze River basin (Northern Ethiopia)
We present a geologic map of the Tekeze River basin that covers an area of ∼69,000 km2 of northern Ethiopia. The map synthesizes new data collected in two campaigns between March, 2012 and January, 2013 and compiled at a scale of 1:500,000 with published geologic surveys. The map focuses on the main geologic and tectonic features relevant to a modern interpretation of the geologic evolution of northern Ethiopia and as such, it represents an impor…
Limestone, Karst and Tufa Dams in the Western Part of the Mekelle Outlier
Permafrost-based geomorphology of the Mt. Foscagno - Mt. Forcellina ridge (Adda – Inn River basins, Central Italian Alps)
The permafrost-based geomorphological map of the Mt. Foscagno–Mt Forcellina ridge (Central Italian Alps) shows the distribution of permafrost probability (high, medium, low probability, and probable absence) obtained by the application of PERMACLIM (Guglielmin et al., 2003), a GIS-based model integrating Digital Elevation Model (DEM) topographic data and the Climatic DataBase (CDB) available from Automatic Weather Stations (AWS). In addition, the…
Geography (8 works) · Geomorphology (7 works) · Geology (5 works) · Physical geography (5 works) · Geology (4 works) · Structural basin (4 works) · Cartography (3 works) · Geological formations and processes (3 works) · Holocene (3 works) · Landform (3 works)