A LARGE, SLOW-MOVING EARTH FLOW IN THE NORTHERN APENNINES: THE SIGNATICO LANDSLIDE (ITALY)

被引:0
|
作者
Mandrone, Giuseppe [1 ]
Buratti, Lorenzo [2 ]
Chelli, Alessandro [2 ]
Lopardo, Luigi [3 ]
Tellini, Claudio [2 ]
机构
[1] Univ Turin, Dipartimento Sci Terra, I-10125 Turin, Italy
[2] Univ Parma, Dipartimento Sci Terra, I-43100 Parma, Italy
[3] Reg Emilia Romagna, Serv Tecn Bacini Affluenti Po, Rome, Italy
来源
关键词
Landslide; Reactivation; Monitoring System; Parma; Italy Valley; ROCK MASSES;
D O I
暂无
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The Signatico landslide is located in Northern Italy, on the Po plain side of the Apennines, along the river Parma. It is a complex landslide with a total length of about 3 kill (the accumulation zone only Occupies over I kill of the river bed). It involves rotational slides and falls from the crown, but the displaced material is very quickly weathered and dismembered, moving downstream as a long, slow flow. This landslide has undergone many reactivations, historically dating back to the Middle Ages. Now, many human facilities are directly at risk: an important road, some villages and some other scattered houses, A comparison of aerial photos taken over the last 30 years was made, in order to identify signals of the landslide evolution while engineering-geological surveys investigated the landslide and the surrounding, areas. A monitoring system is also in progress. The aim of this study is to forecast a possible new reactivation. In this case, it is important to give, as soon as technically possible, the information to civil protection so that loss reduction measures can be adequately planned.
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页码:247 / 253
页数:7
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