Si esaminano gli aspetti geologici e geomorfologici del quartiere di Prati e delle pendici di Monte Mario, con particolare riferimento ai rapporti con il Fiume Tevere e con le disastrose alluvioni che hanno interessato storicamente l'area; inoltre si ricostruiscono le principali modificazioni antropiche ed urbanistiche che ha subito questo settore della piana tiberina dall'epoca romana ai nostri giorni.
The study described in the paper was focused on the geology and geomorphology of the Prati district (17th sub-municipality) and of the area lying at the foot of the Monte Mario hill of Rome, namely on their relations with the Tiber river and the catastrophic floods which have historically hit the area. The study also reconstructed the main changes (in terms of human settlements and urbanisation) that this sector of the Tiber river plain has experienced from Roman times to date.
Lanzini, M., Mazza, R., Capelli, G. (2008). Le antiche alluvioni del Tevere ed i dissesti storici (Prati – Balduina XVII Municipio). MEMORIE DESCRITTIVE DELLA CARTA GEOLOGICA D'ITALIA, 80 parte seconda, 185-194.
Le antiche alluvioni del Tevere ed i dissesti storici (Prati – Balduina XVII Municipio)
MAZZA, Roberto;
2008-01-01
Abstract
The study described in the paper was focused on the geology and geomorphology of the Prati district (17th sub-municipality) and of the area lying at the foot of the Monte Mario hill of Rome, namely on their relations with the Tiber river and the catastrophic floods which have historically hit the area. The study also reconstructed the main changes (in terms of human settlements and urbanisation) that this sector of the Tiber river plain has experienced from Roman times to date.I documenti in IRIS sono protetti da copyright e tutti i diritti sono riservati, salvo diversa indicazione.
