作者: S.-E. Lauritzen , R.Ø. Skoglund
DOI: 10.1016/B978-0-12-374739-6.00111-1
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摘要: Relict phreatic caves, in hanging positions within a glacial topography, pose an enigma with respect to the speleogenetic interpretation. A glacier ice mass may provide liquid water and create caves anywhere adjacent rock, making ice-contact as well interglacial, meteoric speleogenesis feasible. The problem is reviewed relevant rheology, hydrology, chemistry. environment was certainly able overprint widen already existing ( sensu lato speleogenesis), while full evolution of from tight fractures stricto speleogenesis) slow inefficient (about 1/40) compared nonglacial conditions.