P. Gangloff et al., PERMAFROST STRUCTURES OF WURMIAN AGE ON T HE NORTHERN PIEDMONT OF THEPYRENEES, Geographie physique et quaternaire, 48(2), 1994, pp. 169-178
Permafrost structures of Wurmian age on the northern piedmont of the P
yrenees. Cryoturbations developed on top of old terraces of the northe
rn piedmont of the Pyrenees. They deformed the contact between a Wurmi
an loess and weathered gravels underneath. Two fossil ice wedge casts
observed under the cryoturbated layer are indicative of a permafrost o
f Wurmian age, extending more than 15 km north of the external moraine
s of Lourdes.