Hydrated normal carbonate
Specific gravity: 1.77 to 1.8
Colour: Chalky white
Ikaite is a very rare carbonate that forms in sea water and lake water in anaerobic (oxygen deficient), organic-rich
periglacial (subject to repeated freezing and thawing) and glaciomarine (containing both glacial ice and marine water)
environments near 0oC, readily converting to calcite at higher temperatures
of about 8oC
(HOM, Mindat, Webmin).
At White Cliffs, New South Wales, Australia, opal pseudomorphs after ikaite have been found (KL p259).
At the type locality, Ikka Bund, Ikka Fjord, Sermersooq, Greenland, Denmark, chalklike underwater pillars occur in the inner part of the fjord, 8 km south of Ivigtut. The pillars reach to within half a metre of the water surface. The temperature at the base of the pillars was 3oC and 7o at the top. Samples were collected by a frogman and shipped in a refrigerator at about 4oC (AM 49.439).
At the Olitsna river, White Sea coast, Karelia Republic, Russia, calcite pseudomorphs after ikaite have been found (KL p154). These pseudomorphs are sometimes called "glendonite" (Mindat).
At Bielo More, Kola Peninsula, Murmansk Oblast, Russia, pseudomorphs of calcite after ikaite to 10 cm have been found (Extra Lapis English-4 p23).
Back to Minerals