1 The refolding of two nappes differing in age so that parts of the younger nappe lie below older rocks.
2 The convolution of layers of ground under periglacial conditions. To form thermokarst involutions, ice-rich permafrost must thaw, drainage conditions must be poor, and sediments must vary in texture or composition. In addition, the sediments should be susceptible to fluidization, liquefaction, or hydroplastic deformation (Murton and French (1993) Perm. & Periglac. 4, 3). The repetition of differential heave and soft-loam settlement promotes decimetre-scale involutions in near-saturated soils subject to deep seasonal frost penetration (Ogino and Matsuoka (2007) Perm. & Periglac. 18, 4).