Salvi, S., Atzori, S., Tolomei, C., Allievi, J., Ferretti, A., Rocca, F., C. Prati, S. Stramondo, and Feuillet, N., 2004. . Large mafic eruptions at Alban Hills volcanic district (Central Italy): chronostratigraphy, petrography and eruptive behavior. Albano and Nemi lakes craters(central Italy) Post-caldera activity in the Alban Hills volcanic district (Italy): 40Ar/39Ar geochronology and insights into magma evolution. There are two crater lakes, Albano and Nemi which fill the most recent craters of the volcano. "Nel 398 A.C., Al tempo in cui i Romani assediavano i Veienti 9*Sedimentation and mobility of PDCs: a reappraisal of ignimbrites aspect ratio (Colli Albani). . 2010. Funiciello R, Giodano G, De Rita D, 2003. The largest of the post-caldera craters is Lake Albano, a 2.5 x 4 km compound maar constructed at the WSW margin of the caldera in multiple stages dating back to about 69,000 years ago. 23*Water level and volume estimations of the Paleozoic metasomatism at the origin of Mediterranean ultrapotassic magmas: Constraints from time-dependent geochemistry of Colli Albani volcanic products. Altri siti personali: 4*I vulcani di Roma - Protezione Civile Roma. There is no Emissions History data available for Colli Albani. The age of the most recent eruptions from the Albano maar is not known precisely; variable dates range from about 36,000 years ago to perhaps the Holocene, when several possibly non-volcanic lake overflow lahars occurred. The IAVCEI Commission on Volcanic Hazards and Risk has a, Middle InfraRed Observation of Volcanic Activity (. . 2004; Anzidei et al. Terremoti recenti lista INGV View from Castelgandolfo (the famous residence town of the pope) over Lago Albano, the more northwesterly of the two crater lakes. L'antro o grotta di Fauno e la rupe che la sovrasta, dove si trovava il bosco Sacro (, Il paesaggio suggestivo del lago rosso della Solfatara di Pomezia Nella mitica. The third cycle includes another significant ignimbrite eruption of similar dimensions of the preceding one; much of the volume of the corresponding ignimbrite has been removed by erosion since there was no protecting cap of succeeding lava flows. This compilation of synonyms and subsidiary features may not be comprehensive. It is sponsored by the, Information about large Quaternary eruptions (VEI >= 4) is cataloged in the, EarthChem develops and maintains databases, software, and services that support the preservation, discovery, access and analysis of geochemical data, and facilitate their integration with the broad array of other available earth science parameters. Karner D B, Marra F, Renne P R, 2001. Emplacement processes of the mafic Villa Senni Eruption Unit (VSEU) ignimbrite succession, Colli Albani volcano, Italy. The Global Volcanism Program has no activity reports for Colli Albani. 6*The Albano Maar lake (Colli Albani Volcano, Italy): recent volcanic activity and evidence of pre-Roman Age catastrophic lahar events. & Giordano, G. Res., 123: 43-61. related distal tephra deposit (40-36 kaBP). IL tornado sull'Agro di Terracina del 5 Novembre 2017 - D.Bianchino Web Cam Pomezia - vista sul complesso vulcanico visto da Pomezia Chiarabba C, Amato A, Delaney P T, 1997. Valley pond and ignimbrite veneer deposits in the small-volume phreatomagmatic `Peperino Albano' basic ignimbrite, Lago Albano maar, Colli Albani volcano, Italy: influence of topography. 21* Funiciello et al. 28*Mediterranean ultrapotassic magmas: Constraints from time-dependent geochemistry of Colli Albani volcanic products. Web cam sul Lago Albano (di Castel Gandolfo) e Monte Cavo (il Monte Albano) Caldera collapse was accompanied by vigorous eruptions of pyroclastics and subordinate lava flows. The Campi di Annibale-Faete phase lasted from 300 to about 200 ka. There is data available for 2 deformation periods. SO2 detection (concentrazioni di Diossido di Zolfo) - Support to Aviation Control Service Web Cam sul cono di scorie di Monte Compatri storia e leggenda EarthChem is operated by a joint team of disciplinary scientists, data scientists, data managers and information technology developers who are part of the NSF-funded data facility. . The post-caldera eruptions have buried the western side of the caldera rim. Geological map of Colli Albani and surroundings, taken from De Rita et al., in Trigila (1995). A rare Mid-Würmian lithoid tuff in the Agro Pontino graben and its identification as an Albano 5-7 Geotherm. Freda C, Gaeta M, Karner D B, Marra F, Renne P R, Taddeucci J, Scarlato P, Christensen J N, Dallai L, 2006. 12*Lake Albano Maar: bathymetry and level changes - M.Anzidei A. Esposito. . . . The second cycle ended with a noteworthy effusive activity, dated at about 480 ka, which again correlates with a lowering of the sea level. Blanc A C, 1953. Medicanes: Cicloni Mediterranei (ciclogenesi tropicali sul Mar Mediterraneo) - D.Bianchino The history of the Monti Sabatini and Alban Hills volcanoes: groundwork for assessing volcanic-tectonic hazards for Rome. Particolare di un flusso di gas nella pozza di Cava dei Selci. . Mediterranean ultrapotassic magmas: Constraints from time-dependent geochemistry of Colli Albani volcanic products. https://doi.org/10.1029/2004GL020253. Bull Volcanol, 68: 567-591. Parco Naturale Dei Castelli Romani - colli albani (2) The Colli Albani mafic caldera (Roma, Italy): stratigraphy, structure and petrology. The geological evolution of the Colli Albani is generally subdivided into three major phases: 1) Tuscolano-Artemisio, 2) Faete, and 3) the final hydromagmatic phase. In fact, some are fearing a re-activation of the Colli Albani (see a June 1995 newspaper report). Freda C, Gaeta M, Palladino D M, Trigila R, 1997. Outcrops exist up to 80 km from the eruption center where there is evidence that the pyroclastic flows climbed up to about 400 m elevation on the slopes of the Monti Tiburtini, that is, about 200 m above the valley floor. The second cycle brought about the most significant eruption of the Colli Albani which led to the deposition of a major ignimbrite which has thicknesses of 90 m in paleovalleys exposed in the E sector of the volcano. Res., 107: 185-219. Anzidei M, Baldi P, Casula G, Galvani A, Riguzzi F, Zanutta A, 1998. Ad oggi il complesso vulcanico si considera in fase ‘quiescente’ , ovvero in una condizione caratterizzata da manifestazioni di vulcanismo secondario (es. The picturesque town of Nemi lies on the N rim of the crater, offering a commanding view of the lake. A. Riserva Naturale di Tor Caldara, la propaggine a mare del Vulcano Laziale . Res., 78: 103-120. Monte Cavo forms what appears to be a central cone (which, in fact, is only a high crater rim). Uno dei centri di emanazione gassosa e il "lago Bianco" della solfatara. 27*A rare Mid-Würmian lithoid tuff in the Agro Pontino graben and its identification as an Albano 5-7 J. Volcanol. 22*Magnetic fabric and implications for pyroclastic flow and lahar emplacement, Albano maar, Italy. The 1989-1990 seismic swarm in the Alban Hills volcanic area, central Italy. Mid-distal occurrences of the Albano Maar pyroclastic deposits and their relevance for reassessing the eruptive scenarios of the most recent activity at the Colli Albani Volcanic District, Central Italy. Arte: scultura, riproduzioni geologiche, creature e mini mondi- IN COSTRUZIONE... -D.Bianchino Krafft M, 1974. 11*Submerged Landslide Morphologies In The Albano Lake volcano (Rome, Italy) and tsunamigenic potential - P. Mazzanti, F. Bozzano and C. Esposito. Excursion au Mont Circe. This phase is comprised by four eruptive cycles each of which is representated by the emplacement of pyroclastic flows and air fall tephra followed by lava flows in the closing stages of each cycle. Giordano G, De Benedetti A A, Diana A, Diano G, Gaudioso F, Marasco F, Miceli M, Mollo S, Cas R A F, Funiciello R, 2006. The structure of this somma type volcano (caldera with a central cone) is much more complex than it seems from a distance. 19*Mechanical coupling between earthquakes and volcanoes inferred from stress transfer models: evidence from Vesuvio, Etna and Alban Hills volcano (Italy) - Cocco; Feuillet; Nostro; Musumeci; The latest activity occurred about 20 ka ago. 18*Funiciello, R. & Giordano, G. The Colli Albani Volcano: foreword and previous studies. The total volume of erupted products of the Faete phase is only 2 km^3, compared to about 200 km^3 of the Tuscolano-Artemisio volcanics. Geotherm. IL Ciclone Tropicale Mediterraneo Numa - D.Bianchino 10 di questi arrivano o superano il 5° grado della scala richter e culminano nei terremoti del 1438 (5.4) e del 1806 (5.6).