The internal structure of rock glaciers and recently deglaciated slopes as revealed by geoelectrical tomography

insights on permafrost and recent glacial evolution in the Central and Western Alps (Italy-France)

A. Ribolini, M. Guglielmin, D. Fabre, X. Bodin, M. Marchisio, S. Sartini, Matteo Spagnolo, P. Schoeneich

Research output: Contribution to journalArticle

44 Citations (Scopus)

Abstract

Ground ice of permafrost origin and sedimentary ice of glacial origin can coexist in locations where rock glaciers and glaciers interacted, as well as in glacigenic sediments abandoned by a retreating glacier and subsequently exposed again to atmospheric cooling. Some of these geomorphological settings in the Central (Foscagno rock glacier) and Western Alps (Marinet and Schiantala rock glaciers, Schiantala debris-covered glacier, Maledia glacier) were explored by means of geoelectrical tomographies. The aim was that of inferring the presence of ice and cryologically interpreting electrical stratigraphies in order to test whether or not the internal structure of these landforms can be used for the reconstruction of recent permafrost and glacier evolution. Geomorphological data assisted these reconstructions and available borehole stratigraphies were used to calibrate the resistivities.

Along with the ice-debris mixture, massive ice has also been found as lenses both at the apex and the front of the studied rock glaciers. These lenses of sedimentary origin are thought to be transferred from a glacier snout to sectors of rock glacier and eventually embedded into the permafrost creep. The scarcity of frozen debris in the mid-upper part of the rock glaciers - as revealed by low resistivity values - can be due to the disruptive effect of the over-riding glacier over the permafrost.

The near-surface sedimentary ice masses detected along the slopes of the studied glacial cirques are interpreted as or debris-covered terminations of the glaciers still visible upward, or as fragments of it detached by the main bodies. These ice masses are locally associated to medium-high resistive sediments, consistent with permafrost occurrence. This indicates that the non-glacial environment established during the deglaciation allowed the onset of frozen sediments formation.

Overall, the results indicate that internal structure of rock glaciers and recent-deglaciated slopes can store the different climate-related episodes occurred in a specific area, such as those linked to the shifting between glacial to criotic condition and vice-versa. (C) 2009 Elsevier Ltd. All rights reserved.

Original languageEnglish
Pages (from-to)507-521
Number of pages15
JournalQuaternary Science Reviews
Volume29
Issue number3-4
Early online date13 Nov 2009
DOIs
Publication statusPublished - Feb 2010

Keywords

  • mountain permafrost
  • Upper Valtellina
  • Resistivity tomography
  • Maritime Alps
  • Swiss Alps
  • Ice core
  • dynamics
  • environment
  • forefields
  • massif

Cite this

The internal structure of rock glaciers and recently deglaciated slopes as revealed by geoelectrical tomography : insights on permafrost and recent glacial evolution in the Central and Western Alps (Italy-France). / Ribolini, A.; Guglielmin, M.; Fabre, D.; Bodin, X.; Marchisio, M.; Sartini, S.; Spagnolo, Matteo; Schoeneich, P.

In: Quaternary Science Reviews, Vol. 29, No. 3-4, 02.2010, p. 507-521.

Research output: Contribution to journalArticle

@article{5426dd5a25004800b348d9886fdf43c1,
title = "The internal structure of rock glaciers and recently deglaciated slopes as revealed by geoelectrical tomography: insights on permafrost and recent glacial evolution in the Central and Western Alps (Italy-France)",
abstract = "Ground ice of permafrost origin and sedimentary ice of glacial origin can coexist in locations where rock glaciers and glaciers interacted, as well as in glacigenic sediments abandoned by a retreating glacier and subsequently exposed again to atmospheric cooling. Some of these geomorphological settings in the Central (Foscagno rock glacier) and Western Alps (Marinet and Schiantala rock glaciers, Schiantala debris-covered glacier, Maledia glacier) were explored by means of geoelectrical tomographies. The aim was that of inferring the presence of ice and cryologically interpreting electrical stratigraphies in order to test whether or not the internal structure of these landforms can be used for the reconstruction of recent permafrost and glacier evolution. Geomorphological data assisted these reconstructions and available borehole stratigraphies were used to calibrate the resistivities.Along with the ice-debris mixture, massive ice has also been found as lenses both at the apex and the front of the studied rock glaciers. These lenses of sedimentary origin are thought to be transferred from a glacier snout to sectors of rock glacier and eventually embedded into the permafrost creep. The scarcity of frozen debris in the mid-upper part of the rock glaciers - as revealed by low resistivity values - can be due to the disruptive effect of the over-riding glacier over the permafrost.The near-surface sedimentary ice masses detected along the slopes of the studied glacial cirques are interpreted as or debris-covered terminations of the glaciers still visible upward, or as fragments of it detached by the main bodies. These ice masses are locally associated to medium-high resistive sediments, consistent with permafrost occurrence. This indicates that the non-glacial environment established during the deglaciation allowed the onset of frozen sediments formation.Overall, the results indicate that internal structure of rock glaciers and recent-deglaciated slopes can store the different climate-related episodes occurred in a specific area, such as those linked to the shifting between glacial to criotic condition and vice-versa. (C) 2009 Elsevier Ltd. All rights reserved.",
keywords = "mountain permafrost, Upper Valtellina, Resistivity tomography, Maritime Alps, Swiss Alps, Ice core, dynamics, environment, forefields, massif",
author = "A. Ribolini and M. Guglielmin and D. Fabre and X. Bodin and M. Marchisio and S. Sartini and Matteo Spagnolo and P. Schoeneich",
year = "2010",
month = "2",
doi = "10.1016/j.quascirev.2009.10.008",
language = "English",
volume = "29",
pages = "507--521",
journal = "Quaternary Science Reviews",
issn = "0277-3791",
publisher = "Elsevier",
number = "3-4",

}

TY - JOUR

T1 - The internal structure of rock glaciers and recently deglaciated slopes as revealed by geoelectrical tomography

T2 - insights on permafrost and recent glacial evolution in the Central and Western Alps (Italy-France)

AU - Ribolini, A.

AU - Guglielmin, M.

AU - Fabre, D.

AU - Bodin, X.

AU - Marchisio, M.

AU - Sartini, S.

AU - Spagnolo, Matteo

AU - Schoeneich, P.

PY - 2010/2

Y1 - 2010/2

N2 - Ground ice of permafrost origin and sedimentary ice of glacial origin can coexist in locations where rock glaciers and glaciers interacted, as well as in glacigenic sediments abandoned by a retreating glacier and subsequently exposed again to atmospheric cooling. Some of these geomorphological settings in the Central (Foscagno rock glacier) and Western Alps (Marinet and Schiantala rock glaciers, Schiantala debris-covered glacier, Maledia glacier) were explored by means of geoelectrical tomographies. The aim was that of inferring the presence of ice and cryologically interpreting electrical stratigraphies in order to test whether or not the internal structure of these landforms can be used for the reconstruction of recent permafrost and glacier evolution. Geomorphological data assisted these reconstructions and available borehole stratigraphies were used to calibrate the resistivities.Along with the ice-debris mixture, massive ice has also been found as lenses both at the apex and the front of the studied rock glaciers. These lenses of sedimentary origin are thought to be transferred from a glacier snout to sectors of rock glacier and eventually embedded into the permafrost creep. The scarcity of frozen debris in the mid-upper part of the rock glaciers - as revealed by low resistivity values - can be due to the disruptive effect of the over-riding glacier over the permafrost.The near-surface sedimentary ice masses detected along the slopes of the studied glacial cirques are interpreted as or debris-covered terminations of the glaciers still visible upward, or as fragments of it detached by the main bodies. These ice masses are locally associated to medium-high resistive sediments, consistent with permafrost occurrence. This indicates that the non-glacial environment established during the deglaciation allowed the onset of frozen sediments formation.Overall, the results indicate that internal structure of rock glaciers and recent-deglaciated slopes can store the different climate-related episodes occurred in a specific area, such as those linked to the shifting between glacial to criotic condition and vice-versa. (C) 2009 Elsevier Ltd. All rights reserved.

AB - Ground ice of permafrost origin and sedimentary ice of glacial origin can coexist in locations where rock glaciers and glaciers interacted, as well as in glacigenic sediments abandoned by a retreating glacier and subsequently exposed again to atmospheric cooling. Some of these geomorphological settings in the Central (Foscagno rock glacier) and Western Alps (Marinet and Schiantala rock glaciers, Schiantala debris-covered glacier, Maledia glacier) were explored by means of geoelectrical tomographies. The aim was that of inferring the presence of ice and cryologically interpreting electrical stratigraphies in order to test whether or not the internal structure of these landforms can be used for the reconstruction of recent permafrost and glacier evolution. Geomorphological data assisted these reconstructions and available borehole stratigraphies were used to calibrate the resistivities.Along with the ice-debris mixture, massive ice has also been found as lenses both at the apex and the front of the studied rock glaciers. These lenses of sedimentary origin are thought to be transferred from a glacier snout to sectors of rock glacier and eventually embedded into the permafrost creep. The scarcity of frozen debris in the mid-upper part of the rock glaciers - as revealed by low resistivity values - can be due to the disruptive effect of the over-riding glacier over the permafrost.The near-surface sedimentary ice masses detected along the slopes of the studied glacial cirques are interpreted as or debris-covered terminations of the glaciers still visible upward, or as fragments of it detached by the main bodies. These ice masses are locally associated to medium-high resistive sediments, consistent with permafrost occurrence. This indicates that the non-glacial environment established during the deglaciation allowed the onset of frozen sediments formation.Overall, the results indicate that internal structure of rock glaciers and recent-deglaciated slopes can store the different climate-related episodes occurred in a specific area, such as those linked to the shifting between glacial to criotic condition and vice-versa. (C) 2009 Elsevier Ltd. All rights reserved.

KW - mountain permafrost

KW - Upper Valtellina

KW - Resistivity tomography

KW - Maritime Alps

KW - Swiss Alps

KW - Ice core

KW - dynamics

KW - environment

KW - forefields

KW - massif

U2 - 10.1016/j.quascirev.2009.10.008

DO - 10.1016/j.quascirev.2009.10.008

M3 - Article

VL - 29

SP - 507

EP - 521

JO - Quaternary Science Reviews

JF - Quaternary Science Reviews

SN - 0277-3791

IS - 3-4

ER -