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Needle ice; ice structures formed when the air temperature is below 0℃ and the soil is not.
1979, E. Derbyshire, Geomorphological Processes, Routledge, →ISBN, page 208:
The most widespread and familiar example of this process is that associated with the growth of needle ice or pipkrake (Figure 5.15), needles of clear ice commonly exceeding 5 cm in length. Growth of pipkrake is favoured by supercooling of the soil in conditions of marked radiative heat loss from the surface […]