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Случайные фотографии
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: ... [подробнее]
Monday, Aug 26, 2013
Как представляется, что новые фумарольные появился возле аэропорта Рим Фьюмичино Международный субботу утром. Производство небольших фонтанчиков Гейзер как пара, воды и грязи вентиляционные внезапно был открыт в земле вблизи перекрестка вблизи Fiumicino. ... [подробнее]

Monte Albano вулкан

stratovolcano, caldera 950 m
Италия, 41.75°N / 12.71°E
Текущее состояние: normal or dormant (1 из 5) | Reports
Monte Albano volcano books
Last update: 26 Mar 2019
Типичный извержения стиль: ВЗРЫВООПАСНЫЕ
Monte Albano Вулкан-извержения: unknown
ВремяМагнитный / ГлубинаРасстояниеМестоположение
Wed, 13 May 2020
Wed, 13 May 00:07 UTCM 1.5 / 9.8 km26 km6 km SW Fonte Nuova (RM) (Italy)
Tue, 12 May 2020
Tue, 12 May 00:06 UTCM 1.8 / 9.2 km27 km5 km SW Fonte Nuova (RM) (Italy)
Mon, 11 May 2020
Mon, 11 May 22:51 UTCM 1.7 / 8.5 km14 km6 km NW Colonna (RM) (Italy)
Mon, 11 May 03:03 UTCM 3.3 / 10.5 km26 km5 km SW Fonte Nuova (RM) (Italy)
Просмотреть все последние землетрясения
The Monte Albano (Alban Hills) complex immediately SE of Rome contains a large Pleistocene stratovolcano with a 10 x 12 km wide caldera.

Справочная информация:

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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