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Lizardite
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Lizardite
Lizardite is a mineral from the serpentine subgroup with formula Mg3(Si2O5)(OH)4, and the most common type of mineral in the subgroup. It is also a member of the kaolinite-serpentine group.
Lizardite may form a solid-solution series with the nickel-bearing népouite (pure end-member: Ni3(Si2O5)(OH)4). Intermediate compositions (Mg,Ni)3(Si2O5)(OH)4 are possible, with varying proportions of magnesium and nickel. However, the lizardite end-member is much more common than pure népouite, a relatively rare mineral most often formed by the alteration of ultramafic rocks.
Extremely fine-grained, scaly lizardite (also called orthoantigorite) comprises much of the serpentine present in "serpentine marbles". It is triclinic, has one direction of perfect cleavage, and may be white, yellow or green. Lizardite can be translucent or opaque, and have a soapy feel. It may be pseudomorphous after enstatite, olivine or pyroxene, in which case the name bastite is sometimes applied. Bastite may have a silky lustre.
Lizardite was named by Eric James William Whittaker and Jack Zussman in 1955 after the place it was first reported, the Lizard Peninsula, (from the Cornish: An Lysardh) in southern Cornwall, England, United Kingdom.
Scyelite is a synonym of lizardite.
Antigorite and lizardite commonly coexist metastably; lizardite may also be able to turn into antigorite at over 350 degrees.
Lizardite contains H2O in excess of the nominal formula, as does chrysotile. It has a high amount of Fe2O3 and a low amount of FeO.
One study found that lizardite has a high amount of SiO2 and a low amount of Al2O3.
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Lizardite
Lizardite is a mineral from the serpentine subgroup with formula Mg3(Si2O5)(OH)4, and the most common type of mineral in the subgroup. It is also a member of the kaolinite-serpentine group.
Lizardite may form a solid-solution series with the nickel-bearing népouite (pure end-member: Ni3(Si2O5)(OH)4). Intermediate compositions (Mg,Ni)3(Si2O5)(OH)4 are possible, with varying proportions of magnesium and nickel. However, the lizardite end-member is much more common than pure népouite, a relatively rare mineral most often formed by the alteration of ultramafic rocks.
Extremely fine-grained, scaly lizardite (also called orthoantigorite) comprises much of the serpentine present in "serpentine marbles". It is triclinic, has one direction of perfect cleavage, and may be white, yellow or green. Lizardite can be translucent or opaque, and have a soapy feel. It may be pseudomorphous after enstatite, olivine or pyroxene, in which case the name bastite is sometimes applied. Bastite may have a silky lustre.
Lizardite was named by Eric James William Whittaker and Jack Zussman in 1955 after the place it was first reported, the Lizard Peninsula, (from the Cornish: An Lysardh) in southern Cornwall, England, United Kingdom.
Scyelite is a synonym of lizardite.
Antigorite and lizardite commonly coexist metastably; lizardite may also be able to turn into antigorite at over 350 degrees.
Lizardite contains H2O in excess of the nominal formula, as does chrysotile. It has a high amount of Fe2O3 and a low amount of FeO.
One study found that lizardite has a high amount of SiO2 and a low amount of Al2O3.
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