Margarite
Appearance
Margarite | ||
---|---|---|
Mohs scale hardness 4 | | |
References | [2][3][4] |
Margarite is a calcium rich member of the
Mohs hardness of 4. It is translucent with perfect 010 cleavage and exhibits crystal twinning
.
It occurs commonly as an alteration product of corundum, andalusite and other aluminous minerals. It has been reported as forming alteration pseudomorphs of chiastolite along with muscovite and paragonite. The margarite in this occurrence forms preferentially along the dark graphite rich inclusions with the chiastolite crystals.
Margarite is found in the emery deposits of
Aegean islands
, and with corundum
at several localities in the United States.[5]
References
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- Deer, W.A., R.A. Howie, and J. Zussman (1963) Rock-forming minerals, v. 3, Sheet Silicates, p. 95-98.
- public domain: Spencer, Leonard James (1911). "Clintonite". In Chisholm, Hugh (ed.). Encyclopædia Britannica. Vol. 6 (11th ed.). Cambridge University Press. p. 530. This article incorporates text from a publication now in the
- Mineral Data Publishing PDF