Contemporary pingos: a discussion

Authors

  • John Ross Mackay University of British Columbia, Vancouver, Canada

DOI:

https://doi.org/10.26485/BP/1978/27/8

Keywords:

open system, closed system, type of ice, capillary model

Abstract

The principal difference between open and closed system pingos is believed to be in the water source and growth site, rather than in the type of ice. There appears to be a continuum from tabular sheets of injection ice, which are, of course, not pingos, through pingos of intrusive to segregated ice, to flat areas underlain by segregated ice. Thus it is the mound form, rather than ice type, which characterizes a pingo. The growth of open and closed system pingos can be explained by the capillary model which accounts for both the growth of ice and also for pore water expulsion which is associated with closed system pingos. When the capillary model of ice lensing is applied to pingos, the bending resistance of the superincumbent material must be taken into consideration in computing the total uplift resistance.

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