In the western portion of Latium (CentraI ltaly) a series of ancient, generally evident volcanic edifices and numerous lakes hosted in depressions is present. They are directly or indirectly tied to severe volcanism which occurred between 2 and 0.08 Ma ago. From a geomorphological point of view, it is possible to identify different volcanic landscapes, whose appearance mainIy depends on the magma chemistry. The landscape of the Tuscan-Latium Magmatic Province, which was fed by silicic magmas, is typified by numerous lava domes, rising up from a generally fiat ignimbritic plateaux. The landscape of the alkaline potassic volcanism shows strong differences that are tied to the existence or not of well-identified centraI volcanic edifices. In the first case the Iandscape is dominated by the presence of outstanding volcanic relief; in the second one many di fferen t minor emission centres are scattered over Iarge fiat areas, mainly built up by pyroclastic flows.
A route of fire in Central Italy. The Lazio ancient volcanoes / Fredi, Paola; Ciccacci, Sirio. - STAMPA. - (2017), pp. 303-316. [10.1007/978-3-319-26194-2].
A route of fire in Central Italy. The Lazio ancient volcanoes
FREDI, Paola;CICCACCI, Sirio
2017
Abstract
In the western portion of Latium (CentraI ltaly) a series of ancient, generally evident volcanic edifices and numerous lakes hosted in depressions is present. They are directly or indirectly tied to severe volcanism which occurred between 2 and 0.08 Ma ago. From a geomorphological point of view, it is possible to identify different volcanic landscapes, whose appearance mainIy depends on the magma chemistry. The landscape of the Tuscan-Latium Magmatic Province, which was fed by silicic magmas, is typified by numerous lava domes, rising up from a generally fiat ignimbritic plateaux. The landscape of the alkaline potassic volcanism shows strong differences that are tied to the existence or not of well-identified centraI volcanic edifices. In the first case the Iandscape is dominated by the presence of outstanding volcanic relief; in the second one many di fferen t minor emission centres are scattered over Iarge fiat areas, mainly built up by pyroclastic flows.File | Dimensione | Formato | |
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