Fabio Florindo
Biographic Data
| ID | 5647092 |
|---|---|
| NAME | Fabio Florindo |
| GIVEN NAMES | Fabio |
| FAMILY NAME | Florindo |
| SIGNATURE | FLORINDO F |
| AFFILIATIONS | Istituto Nazionale di Geofisica e Vulcanologia |
| ORCID | 0000-0002-6058-9748 |
| VERIFIED | Yes |
| TOTAL WORKS | 6 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 6 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2015 |
| LATEST PUBLICATION YEAR | 2026 |
| H-INDEX | 0 |
Archaeomagnetic reconstruction on the firing orientation of Italian Terra Sigillata ware
Archaeomagnetism, the application of paleomagnetic methods to archaeological materials, can be used not only for chronological dating but also to address unresolved questions in cultural heritage research and archaeology by investigating ancient technologies. In this study, we focus on a longstanding unresolved question in Roman ceramic production: the loading configuration and stacking patterns of vessels inside kilns. We apply archaeomagnetic m…
On the Trail of the “Trembling” Pompeii (Italy)
Ancient Pompeii is known worldwide for having been destroyed by the Plinian eruption of Vesuvius in 79 CE. However, the city experienced a prolonged period of seismicity preceding the catastrophe, beginning with a major earthquake in 62 CE, the effects of which are identifiable in the archaeological structures. This study examines multiple lines of evidence for superimposed, ancient seismic damage in four contexts excavated between 2018 and 2025,…
Late Holocene Abrupt Changes in the Fluvial Dynamics of the Tiber Valley Catchment (Rome, Italy)
In the present work, we investigate the post-glacial aggradation of three tributary valleys draining the left hydrographic basin of the Tiber River in central Rome: the Murcia, Caffarella, and Grottaperfetta valleys. We describe the Upper Pleistocene–Holocene stratigraphic record of the alluvial successions occurring in the Caffarella Valley through the core data collected in a dedicatedly performed 35 m deep borehole. We provide seven 14C age co…
The Bucobello 322 ka-fossil-bearing volcaniclastic-flow deposit in the eastern Vulsini Volcanic District (central Italy)
A review of the stratigraphy of Rome (Italy) according to geochronologically and paleomagnetically constrained aggradational successions, glacio-eustatic forcing and volcano-tectonic processes
A potential global boundary stratotype section and point (GSSP) for the Tarentian Stage, Upper Pleistocene, from the Taranto area (Italy)
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A potential global boundary stratotype section and point (GSSP) for the Tarentian Stage, Upper Pleistocene, from the Taranto area (Italy)
A review of the stratigraphy of Rome (Italy) according to geochronologically and paleomagnetically constrained aggradational successions, glacio-eustatic forcing and volcano-tectonic processes
The Bucobello 322 ka-fossil-bearing volcaniclastic-flow deposit in the eastern Vulsini Volcanic District (central Italy)
Late Holocene Abrupt Changes in the Fluvial Dynamics of the Tiber Valley Catchment (Rome, Italy)
In the present work, we investigate the post-glacial aggradation of three tributary valleys draining the left hydrographic basin of the Tiber River in central Rome: the Murcia, Caffarella, and Grottaperfetta valleys. We describe the Upper Pleistocene–Holocene stratigraphic record of the alluvial successions occurring in the Caffarella Valley through the core data collected in a dedicatedly performed 35 m deep borehole. We provide seven 14C age co…
Archaeomagnetic reconstruction on the firing orientation of Italian Terra Sigillata ware
Archaeomagnetism, the application of paleomagnetic methods to archaeological materials, can be used not only for chronological dating but also to address unresolved questions in cultural heritage research and archaeology by investigating ancient technologies. In this study, we focus on a longstanding unresolved question in Roman ceramic production: the loading configuration and stacking patterns of vessels inside kilns. We apply archaeomagnetic m…
On the Trail of the “Trembling” Pompeii (Italy)
Ancient Pompeii is known worldwide for having been destroyed by the Plinian eruption of Vesuvius in 79 CE. However, the city experienced a prolonged period of seismicity preceding the catastrophe, beginning with a major earthquake in 62 CE, the effects of which are identifiable in the archaeological structures. This study examines multiple lines of evidence for superimposed, ancient seismic damage in four contexts excavated between 2018 and 2025,…
Sedimentary rock (4 works) · Geology (3 works) · Geology and Paleoclimatology Research (3 works) · Paleontology (3 works) · Aggradation (2 works) · Archaeology (2 works) · Fluvial (2 works) · Maritime and Coastal Archaeology (2 works) · Structural basin (2 works) · Tectonics (2 works)