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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: ... [more]
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. ... [more]
 

Monte Albano volcano

stratovolcano, caldera 950 m
Italy, 41.75°N / 12.71°E
Current status: dormant (1 out of 5)
Monte Albano volcano books
Last update: 1 Oct 2013
Typical eruption style: Explosive
Monte Albano volcano eruptions: unknown
TimeMag. / DepthDistanceLocation
Fri, 15 Sep
Fri, 15 Sep 18:12 UTCM 2.3 / 10 km38 kmSOUTHERN ITALY
Thu, 17 Aug
Thu, 17 Aug 20:45 UTCM 1.6 / 10 km30 km6 km N Latina (LT)
Tue, 15 Aug
Tue, 15 Aug 04:57 UTCM 1.9 / 6.4 km36 km3 km SW Bassiano (LT)
Sun, 13 Aug
Sun, 13 Aug 17:07 UTCM 1.4 / 9.7 km21 km1 km SE Poli (RM)
View all recent quakes
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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