Fasi di alluvionamento nella Piana di Santa Caterina Valfurva, Alpi Centrali, nell’ultimo millennio
Flood events in the alluvial plain of Santa Caterina Valfurva, Central Alps, during the last millennium
Keywords:
Floods, Peat, Holocene, 14CAbstract
Several peat levels inter layered between gravel and sand beds, in the alluvial plain near S. Caterina Valfurva (Sondrio, Italy), have been radiocarbon dated to the last millennium or, more exactly to the last twelve centuries. Floods events occurred before 1. 115 ± 85 years 14C. B.P.; between 1.115 ± 85 and 970 ± 100 years 14C. B.P.; between 970 ± 100 and 895 ± 105 years 14C. B.P.; between 605 ± 130 e 425 ± 105 years 14C. B.P. and after 425 ± 105 years 14C. B.P. (age 14C. not calibrated). Flood events became less frequent in recent times, when peat bog conditions were prevailing.
Downloads
Published
Issue
Section
License
Copyright (c) 2024 Manuela Pelfini (Author)
This work is licensed under a Creative Commons Attribution 4.0 International License.
You are free to copy, distribute and transmit the work, and to adapt the work. You must attribute the work in the manner specified by the author or licensor (but not in any way that suggests that they endorse you or your use of the work).