permafrost

 PER-mah-frost

 Ground that remains frozen continuously for two or more years — soil, rock, and sediment held together by ice. Permafrost underlies roughly a quarter of the Northern Hemisphere's land surface and can extend to depths of over a thousand feet. It is not permanent despite its name. As the Arctic warms, permafrost is thawing — releasing stored carbon, destabilizing infrastructure, and reshaping landscapes into the pitted, slumping terrain called thermokarst.
Etymology
 English compound, coined in 1943 by Siemon William Muller — permanent + frost. The name was aspirational; the ground is proving less permanent than the word suggests.
 ice/snow geology
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