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The results of a combined geophysical and geomorphological investigation of thermal-contraction-crack polygons near Gondwana station (Germany) in northern Victoria Land (Antarctica) are reported. An area of about 20,000 m(2) characterized by random orthogonal polygons was investigated using integrated ground penetrating radar, electrical resistivity tomography, geomorphological surveys, and two trench excavations. The polygons are well developed only at elevations higher than 6-7 m above current sea level on Holocene-age raised beaches. It is concluded that the polygons are composite in nature because the shallow linear depressions that outline the polygons are underlain by fissures that can contain both sandy gravel and foliated ice (i.e., ice wedges) even in the same polygon network and at distances of just a few meters. Unexpectedly, most of the polygons follow the border of the raised beaches and develop in correspondence with stratigraphic layers dipping toward the sea, imaged by ground penetrating radar (GPR) profiles and interpreted as prograding layers toward the present-day shoreline.

We exploit the attribute analysis of GPR data to analyze the different EM responses of the ice of two alpine glaciers. We focus on frequency-related attributes to identify zones with higher attenuation of EM signal, which could be further related to higher water content and higher electrical conductivity. We succeeded in associating the scattering facies to warm ice zones of the Marmolada glacier, further linked to the thickness of the snow cover, and to a layer of mixed debris and ice of the Eastern Gran Zebrù glacier. Moreover, we conducted automated diffraction hyperbolas analyses to gain insight into the basal thermal conditions and glaciological facies.