The Piuro 1618 landslide is renowned as one of the most catastrophic historical events of the Central Alps. The landscape of the Bregaglia Valley has been successively modified to such an extent to make it difficult to ascertain the source of the landslide, the extent of its deposits and the setting of the ancient village. This study focuses on the identification of the source area of the landslide, its dynamics, the extent of its deposits and the estimation of the involved volumes. The geological map here proposed permitted to reconstruct the relationships between the pre-1618 setting, the 1618 restructuration of the landscape and the post-event changes that occurred owing to erosion by the trunk river, deposition of debris flow fans and slope dynamics. The paper shows how geological mapping may help to unravel landscape evolution of an Alpine valley even at the high-resolution required by historical and archaeological studies.

Geology of the area of the Piuro 1618 event (Val Bregaglia, Italian Central Alps) : the setting of a catastrophic historical landslide / E. Pigazzi, R. Bersezio, A. Morcioni, D. Tantardini, T. Apuani. - In: JOURNAL OF MAPS. - ISSN 1744-5647. - 18:2(2022), pp. 342-351. [10.1080/17445647.2022.2057878]

Geology of the area of the Piuro 1618 event (Val Bregaglia, Italian Central Alps) : the setting of a catastrophic historical landslide

E. Pigazzi
Primo
;
R. Bersezio
Secondo
;
A. Morcioni;D. Tantardini
Penultimo
;
T. Apuani
Ultimo
2022

Abstract

The Piuro 1618 landslide is renowned as one of the most catastrophic historical events of the Central Alps. The landscape of the Bregaglia Valley has been successively modified to such an extent to make it difficult to ascertain the source of the landslide, the extent of its deposits and the setting of the ancient village. This study focuses on the identification of the source area of the landslide, its dynamics, the extent of its deposits and the estimation of the involved volumes. The geological map here proposed permitted to reconstruct the relationships between the pre-1618 setting, the 1618 restructuration of the landscape and the post-event changes that occurred owing to erosion by the trunk river, deposition of debris flow fans and slope dynamics. The paper shows how geological mapping may help to unravel landscape evolution of an Alpine valley even at the high-resolution required by historical and archaeological studies.
geological map; Central Alps; Bregaglia Valley; landslides; Palimpsest landscape; Piuro 1618
Settore GEO/05 - Geologia Applicata
Settore GEO/02 - Geologia Stratigrafica e Sedimentologica
   Alpi in Movimento, Movimento nelle Alpi. Piuro 1618-2018 (A.M.AL.PI.18)
   A.M.AL.PI.18
   EUROPEAN COMMISSION
   ID 594274
2022
4-apr-2022
https://www.tandfonline.com/doi/full/10.1080/17445647.2022.2057878
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/2434/932107
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