Geophysical signature of a World War i tunnel-like anomaly in the Forni Glacier (Punta Linke, Italian Alps)

Global warming and the associated glacier retreat recently revealed the entrance to an ice–rock tunnel, at an altitude of ∼3600 m a.s.l., in the uppermost portion of the Forni Glacier in the Central Italian Alps. The tunnel served as an entrance to an Austro-Hungarian cableway station excavated in t...

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Published in:Journal of Glaciology
Main Authors: Francese R. G., Bondesan A., Giorgi M., Picotti S., Carcione J., Salvatore M. C., Nicolis F., Baroni C.
Other Authors: Francese, R. G., Bondesan, A., Giorgi, M., Picotti, S., Carcione, J., Salvatore, M. C., Nicolis, F., Baroni, C.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2019
Subjects:
GPR
Online Access:http://hdl.handle.net/11577/3316467
https://doi.org/10.1017/jog.2019.59
https://www.cambridge.org/core/journals/journal-of-glaciology/all-issues
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spelling ftunivpadovairis:oai:www.research.unipd.it:11577/3316467 2024-04-21T08:06:18+00:00 Geophysical signature of a World War i tunnel-like anomaly in the Forni Glacier (Punta Linke, Italian Alps) Francese R. G. Bondesan A. Giorgi M. Picotti S. Carcione J. Salvatore M. C. Nicolis F. Baroni C. Francese, R. G. Bondesan, A. Giorgi, M. Picotti, S. Carcione, J. Salvatore, M. C. Nicolis, F. Baroni, C. 2019 ELETTRONICO http://hdl.handle.net/11577/3316467 https://doi.org/10.1017/jog.2019.59 https://www.cambridge.org/core/journals/journal-of-glaciology/all-issues eng eng Cambridge University Press info:eu-repo/semantics/altIdentifier/wos/WOS:000487667400008 volume:65 issue:253 firstpage:798 lastpage:812 numberofpages:15 journal:JOURNAL OF GLACIOLOGY http://hdl.handle.net/11577/3316467 doi:10.1017/jog.2019.59 info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85072067801 https://www.cambridge.org/core/journals/journal-of-glaciology/all-issues info:eu-repo/semantics/openAccess Glacier decay GPR Italian Alp military geoscience numerical modeling seismic white war World War I info:eu-repo/semantics/article 2019 ftunivpadovairis https://doi.org/10.1017/jog.2019.59 2024-03-28T02:04:55Z Global warming and the associated glacier retreat recently revealed the entrance to an ice–rock tunnel, at an altitude of ∼3600 m a.s.l., in the uppermost portion of the Forni Glacier in the Central Italian Alps. The tunnel served as an entrance to an Austro-Hungarian cableway station excavated in the rocks during the Great War just behind the frontline. A comprehensive geophysical survey, based on seismic and ground-penetrating radar profiling, was then undertaken to map other possibleWorldWar I (WWI) remains still embedded in the ice. The ice–rock interface was reconstructed over the entire saddle and in the uppermost portion of the glacier. A prominent linear reflector was surprisingly similar to the common response of buried pipes. The reflector orientation, almost longitudinal to the slope, does not seem to be compatible with a glacial conduit or with other natural features. Numerical simulations of a series of possible targets constrained interpretation to a partly water-filled rounded shape cavity. The presence of a preserved WWI tunnel connecting Mount Vioz and Punta Linke could be considered a realistic hypothesis. The Forni glacier could be still considered polythermal and comprised of cold ice without basal sliding in its top portion. Article in Journal/Newspaper Journal of Glaciology Padua Research Archive (IRIS - Università degli Studi di Padova) Journal of Glaciology 65 253 798 812
institution Open Polar
collection Padua Research Archive (IRIS - Università degli Studi di Padova)
op_collection_id ftunivpadovairis
language English
topic Glacier decay
GPR
Italian Alp
military geoscience
numerical modeling
seismic
white war
World War I
spellingShingle Glacier decay
GPR
Italian Alp
military geoscience
numerical modeling
seismic
white war
World War I
Francese R. G.
Bondesan A.
Giorgi M.
Picotti S.
Carcione J.
Salvatore M. C.
Nicolis F.
Baroni C.
Geophysical signature of a World War i tunnel-like anomaly in the Forni Glacier (Punta Linke, Italian Alps)
topic_facet Glacier decay
GPR
Italian Alp
military geoscience
numerical modeling
seismic
white war
World War I
description Global warming and the associated glacier retreat recently revealed the entrance to an ice–rock tunnel, at an altitude of ∼3600 m a.s.l., in the uppermost portion of the Forni Glacier in the Central Italian Alps. The tunnel served as an entrance to an Austro-Hungarian cableway station excavated in the rocks during the Great War just behind the frontline. A comprehensive geophysical survey, based on seismic and ground-penetrating radar profiling, was then undertaken to map other possibleWorldWar I (WWI) remains still embedded in the ice. The ice–rock interface was reconstructed over the entire saddle and in the uppermost portion of the glacier. A prominent linear reflector was surprisingly similar to the common response of buried pipes. The reflector orientation, almost longitudinal to the slope, does not seem to be compatible with a glacial conduit or with other natural features. Numerical simulations of a series of possible targets constrained interpretation to a partly water-filled rounded shape cavity. The presence of a preserved WWI tunnel connecting Mount Vioz and Punta Linke could be considered a realistic hypothesis. The Forni glacier could be still considered polythermal and comprised of cold ice without basal sliding in its top portion.
author2 Francese, R. G.
Bondesan, A.
Giorgi, M.
Picotti, S.
Carcione, J.
Salvatore, M. C.
Nicolis, F.
Baroni, C.
format Article in Journal/Newspaper
author Francese R. G.
Bondesan A.
Giorgi M.
Picotti S.
Carcione J.
Salvatore M. C.
Nicolis F.
Baroni C.
author_facet Francese R. G.
Bondesan A.
Giorgi M.
Picotti S.
Carcione J.
Salvatore M. C.
Nicolis F.
Baroni C.
author_sort Francese R. G.
title Geophysical signature of a World War i tunnel-like anomaly in the Forni Glacier (Punta Linke, Italian Alps)
title_short Geophysical signature of a World War i tunnel-like anomaly in the Forni Glacier (Punta Linke, Italian Alps)
title_full Geophysical signature of a World War i tunnel-like anomaly in the Forni Glacier (Punta Linke, Italian Alps)
title_fullStr Geophysical signature of a World War i tunnel-like anomaly in the Forni Glacier (Punta Linke, Italian Alps)
title_full_unstemmed Geophysical signature of a World War i tunnel-like anomaly in the Forni Glacier (Punta Linke, Italian Alps)
title_sort geophysical signature of a world war i tunnel-like anomaly in the forni glacier (punta linke, italian alps)
publisher Cambridge University Press
publishDate 2019
url http://hdl.handle.net/11577/3316467
https://doi.org/10.1017/jog.2019.59
https://www.cambridge.org/core/journals/journal-of-glaciology/all-issues
genre Journal of Glaciology
genre_facet Journal of Glaciology
op_relation info:eu-repo/semantics/altIdentifier/wos/WOS:000487667400008
volume:65
issue:253
firstpage:798
lastpage:812
numberofpages:15
journal:JOURNAL OF GLACIOLOGY
http://hdl.handle.net/11577/3316467
doi:10.1017/jog.2019.59
info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-85072067801
https://www.cambridge.org/core/journals/journal-of-glaciology/all-issues
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