Determinazione della struttura interna del rock glacier di Val Pisella (Alta Valtellina) attraverso sondaggi elettrici verticali. Risultati e problemi

Structure determination of the Val Pisella Rock Glacier (Upper Valtellina,Italy) by means of geoelectrical soundings. Results and problems

Authors

  • Cesare Resnati GEOPLAN, Monza, Italy Author
  • Claudio Smiraglia Cattedra di Geografia dell'Università di Pescara, Pescara, Italy Author

Keywords:

Rock glacier, Geoelectrical sounding, Periglacial morphology, Valtellina, Alps, Italy

Abstract

Some electrical resistivity surveys were performed on the Val Pisella Rock Glacier (Upper Valtellina, Italy) in the summer of 1989; the main objectives were to detect ice and to determine its nature. All the survey shown high values of resistivity (more than 100 000 Qm with a maximum around 1 000 000 Qm). According to these results the rock glacier contains permafrost in the form of an ice-cemented core of varying ice content; the maximum permafrost thickness is around 5 m. Therefore the rock glacier can be considered an ice-cemented one.

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Published

2024-07-10

Issue

Section

Research and review papers

How to Cite

Resnati, C., & Smiraglia, C. (2024). Determinazione della struttura interna del rock glacier di Val Pisella (Alta Valtellina) attraverso sondaggi elettrici verticali. Risultati e problemi: Structure determination of the Val Pisella Rock Glacier (Upper Valtellina,Italy) by means of geoelectrical soundings. Results and problems. Geografia Fisica E Dinamica Quaternaria, 13(2), 171-177. https://www.gfdq.glaciologia.it/index.php/GFDQ/article/view/789

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