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Willekeurige foto 's
News
Tuesday, Oct 01, 2013
A second (and much more violent) geyser-like fumarole or mudvolcano recently appeared off shore near Fumiciono, approx. 100 meters out from the beach in the area where the new port of Rome is being built. It is an underwater vent that produces fountains of upwelling sediment-rich water driven by strong degassing from the sea floor: ... [meer...]
Monday, Aug 26, 2013
What appears to be a new fumarole appeared near Rome's International Fiumicino airport Saturday morning. A vent producing small geyser-like fountains of steam, water and mud suddenly opened in the ground near a road crossing near Fiumicino. ... [meer...]
 

Monte Albano vulkaan

stratovulkaan, caldera 950 m
Italy, 41.75°N / 12.71°E
Current status: normal or dormant (1 out of 5) | Reports
Monte Albano vulkaan boeken
Last update: 1 Oct 2013
Typical eruption style: Explosieve
Monte Albano vulkaanuitbarstingen: unknown
TijdMag. / DiepteAfstandLocatie
Mon, 25 Mar 2019
Mon, 25 Mar 00:09 UTCM 1.7 / 11.1 km10 km3 km W Colonna (RM) (Italy)
Sun, 24 Mar 2019
Sun, 24 Mar 03:21 UTCM 1.3 / 4.8 km12 km2 km N Colonna (RM) (Italy)
Mon, 11 Mar 2019
Mon, 11 Mar 05:19 UTCM 1.2 / 4.3 km12 km2 km N Colonna (RM) (Italy)
Thu, 7 Feb 2019
Thu, 7 Feb 21:08 UTCM 1.4 / 10.4 km16 km7 km NW Colonna (RM)
Wed, 6 Feb 2019
Wed, 6 Feb 22:06 UTCM 2.0 / 9 km13 kmSOUTHERN ITALY
Bekijk alle recente aardbevingen
The Monte Albano (Alban Hills) complex immediately SE of Rome contains a large Pleistocene stratovolcano with a 10 x 12 km wide caldera.

Background:

The caldera was formed during an eruptive period with six major explosive eruptions producing at least 280 cu km of ejecta between about 560,000 and 350,000 years ago. Subsequent eruptions occurred from a new 5-km-wide central cone and from many phreatomagmatic craters and cones within the Artemisio-Tuscolana caldera and on its outer flanks. The post-caldera eruptions have buried the western side of the caldera rim. The largest of the post-caldera craters is Lake Albano, a 4 x 2.5 km wide maar constructed at the WSW margin of the caldera in 5 stages dating back to about 45,000 years ago. Eruptive products of the 3rd stage were dated at 26,000 yrs Before Present (BP). The 4th and 5th stages were not dated directly, but sediment-core gaps at 16,000 and 7500 yrs BP may correspond to these eruptions (Villa et al., 1999). Reported historical eruptions during the Roman period are uncertain, but seismic swarms of up to two years duration have been recorded since Roman times.
Source: Smithsonian GVP


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