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A variety of labradorite known as spectrolite is found in Finland.
The combination of dark red and black labradorite enhanced its slender, precise construction.
The uncommon anorthosite bodies are composed almost entirely of labradorite.
Some kinds of labradorite are called moonstone or sunstone.
Spectrolite is a less common variety of labradorite feldspar.
Labradorite is the principal component of the igneous rock type anorthosite.
The name spectrolite is sometimes incorrectly applied to any labradorite of similar colours.
The feldspar variety labradorite is commonly present in anorthosites.
Augite and labradorite are found in these dolerites.
The platform floors' are nevertheless riveted with labradorite.
Minerals such as turquoise, azurite, labradorite, and lapis lazuli are blue.
Labradorite is one kind of feldspar.
Feldspar phenocrysts typically are labradorite to andesine in composition.
The plagioclase ranges from oligoclase to andesine and labradorite.
The upper differentiated portions include ilmenite bearing labradorite anorthosites.
The wall is laid with gret granite and labradorite, as well as asphalt on the platform edge.
In early reports (Butler 1983, Johannesmeyer 1999) this mineral was mistakenly identified as labradorite.
The island is the geological type area of the mineral labradorite, which is a plagioclase feldspar.
The item is a bracelet of bottle labradorite, carved into the shape of a supine woman."
The basalt comprises phenocrysts of clinopyroxene and labradorite.
The basic soda-lime feldspars (labradorite to anorthite) are those that undergo this type of alteration.
Basic varieties of plagioclase, such as labradorite, are known also as phenocrysts in some Italian trachytes.
Examples include opal, labradorite, ammolite and bornite.
Gemstone varieties of labradorite exhibiting a high degree of labradorescence are called spectrolite.
These tones contrast with the dark shade of a socle, made out of polished labradorite, and has a significant jut against a plane wall.