Nuove ipotesi sulla massima espansione olocenica del Ghiacciaio della Ventina (Valtellina, Alpi Retiche)
New hypothesis about the maximum advance of the Ventina Glacier (Valtellina, Alpi Retiche)
Keywords:
Glacier, Dendrogeomorphology, HoloceneAbstract
A stump found between the outermost frontal moraine and the second one deposited by the Ventina Glacier, allows to discuss new hypothesis about the holocenic history of the glacier. This work discuss the firsts 14C results obtained.
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Published
2024-07-05
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Short communication
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Copyright (c) 2024 Manuela Pelfini, Claudio Smiraglia (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).
How to Cite
Pelfini, M., & Smiraglia, C. (2024). Nuove ipotesi sulla massima espansione olocenica del Ghiacciaio della Ventina (Valtellina, Alpi Retiche) : New hypothesis about the maximum advance of the Ventina Glacier (Valtellina, Alpi Retiche). Geografia Fisica E Dinamica Quaternaria, 17(1), 103-105. https://www.gfdq.glaciologia.it/index.php/GFDQ/article/view/687
