The 1513 Monte Crenone rock avalanche: Numerical model and geomorphological analysis

4Citations
Citations of this article
6Readers
Mendeley users who have this article in their library.

Abstract

As a contribution to the knowledge of historical rockslides, this research focuses on the historical reconstruction, field mapping, and simulation of the expansion, through numerical modelling, of the 30 September 1513 Monte Crenone rock avalanche. Earth observation in 2-D and 3-D, as well as direct in situ field mapping, allowed the detachment zone and the perimeter and volume of the accumulation to be determined. Thanks to the reconstruction of the post-event digital elevation model based on historical topographic maps and the numerical modelling with the RAMMS::DEBRISFLOW software, the dynamics and runout of the rock avalanche were calibrated and reconstructed. The reconstruction of the runout model allowed confirmation of the historical data concerning this event, particularly the damming of the valley floor and the lake formation up to an elevation of 390gmga.s.l., which generated an enormous flood by dam breaching on 20 May 1515, known as the "Buzza di Biasca".

Cite

CITATION STYLE

APA

De Pedrini, A., Ambrosi, C., & Scapozza, C. (2022). The 1513 Monte Crenone rock avalanche: Numerical model and geomorphological analysis. Geographica Helvetica, 77(1), 21–37. https://doi.org/10.5194/gh-77-21-2022

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free