Amakinite | |
Imasymbol: | Amk |
System: | Trigonal |
Color: | Pale green to yellow-green; rapidly turns brown when exposed to air, due to formation of Fe(OH)3 |
Cleavage: | Poor/Indistinct |
Fracture: | Irregular/Uneven |
Mohs: | 3.5-4 |
Gravity: | 2.925 - 2.98 |
Opticalprop: | Uniaxial |
Amakinite (IMA symbol: Amk[1]) is a semi transparent yellow-green hydroxide mineral belonging to the brucite group that was discovered in 1962. Its chemical formula is written as (Fe2+,Mg)(OH)2. It usually occurs in the form of splotchy, anhedral crystals forming within a group or structure in other minerals or rocks, such as kimberlite (occurring in diamond-rich eruptive pipe). Its composition is as follows:
Amakinite is slightly magnetic and was named for the Amakin Expedition,[2] which prospected the diamond deposits of Yakutia in the Russian Far East.[3]