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Sounds reasonable; basically a methane boil as all these pockets start coalescing into ever bigger pockets in a runaway reaction?

Still, since it's always above freezing under the permafrost (according to Wikipedia, a max thickness of 4m, and that crater looks far deeper), perhaps these pockets are common, and there are many places where the permafrost serves as a cap over columns of foamy earth. Maybe the freeze-thaw cycle isn't so important in the formation of these foamy regions, but more so in the degradation of the caps over them?