Labradorite

_Composition_: NaAlSi₃O₈, 50% to 30%; CaAl₂Si₂O₈, 50% to 70%. _Crystal

system_: triclinic. _Hardness_: 6.0 to 6.5. _Specific gravity_: about

2.60. _Luster_: vitreous to sometimes pearly. _Color_: straw yellow,

white, greenish, gray, reddish, bluish, and green. Sometimes shows a

play of colors on particular cleavage surfaces. _Streak_: uncolored.

_Cleavage_: three directions. _Fracture_: uneven to conchoidal.

_Tenacity_: brittle. _Diaphaneity_: transparent to translucent.

_Refractive index_: about 1.56. _Dispersion_: low.

Very fine facet-quality labradorite has been found about 20 miles south

of Alpine, Brewster County. The labradorite occurs loose in the soil as

slightly weathered or frosted cleavage fragments, commonly showing one

or more crystal faces (Pl. II, B). The pale-yellow or straw-yellow color

of these fragments, as well as their lack of internal imperfections,

makes these stones excellent gem material. Individual pieces that exceed

three-fourths inch in their longest dimensions are rare. Cut stones of

more than 5 or 6 carats from this locality are scarce. The source of

this material is uncertain, but it is probably weathering out of an

underlying igneous rock.

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