GLOSSARY

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Amorphous—without definite molecular structure; not crystalline.
Baroque stone—an irregularly shaped, polished stone; usually applied to tumbled stones.
Baroque pearl—an irregularly shaped pearl.
Brilliancy—reflecting much light; having brightness.
Brilliant cut—a mode of arrangement of facets commonly used on round or oval stones. The standard American brilliant cut has 57 or 58 facets. Most diamonds of 5 or less carats are cut in this manner.
Cabochon—a stone cut with a flat or convex upper surface; sometimes faceted in part. Opal, star sapphire, and agate are stones that are frequently cut in this style (fig. 2).
Cambrian—a division of geologic time, estimated to be the time from 550 to 440 million years ago; the oldest time division of the Paleozoic era.
Carat—a unit of weight equal to ? of a gram or 0.2 gram. One ounce avoirdupois is equal to 141.75 carats.
Cleavage—the tendency of certain minerals to split in particular directions yielding relatively smooth plane surfaces.
Conchiolin—an organic albuminoid substance found in pearls.
Conchoidal—a type of fracture having curved concavities or the approximate shape of one-half of a bivalve shell. Glass has excellent conchoidal fracture.
Cretaceous—a division of geologic time, estimated to be the time from 135 to 60 million years ago; youngest division of the Mesozoic era.
Crown—that portion of a faceted gem above the girdle; the upper portion of a facet-cut gem (fig. 6).
Cryptocrystalline—composed of very fine or microscopic crystals.
Crystal—the regular polyhedral form, bounded by plane surfaces, that is assumed by a mineral under suitable conditions. Crystals have definite external symmetry and internal molecular order.
Crystalline—possessing definite internal molecular order; not amorphous.
Cubic—in the general shape of a cube. The isometric crystal system is often called the cubic system.
Culet—the very bottom portion of a faceted gem; the point or line formed by the intersection of the lowest pavilion facets (fig. 6).
Dendritic—branching or tree-like in form.
Diaphaneity—relative transparency. The diaphaneity of a mineral is described as transparent, translucent, opaque, etc.
Dike—a tabular rock body, usually igneous in origin, which cuts across the surrounding rock strata.
Dispersion—a measure of the ability of gemstones to separate complex or white light into its component colors; often illustrated with a prism. Gemstones that are capable of separating colors of light widely are said to have high dispersion; gemstones not so capable of separating white light into colors are said to have low dispersion.
Dopping—the act of cementing a gemstone, either rough or partly finished, to a dop-stick.
Dop-stick—the wooden stick or cylindrical piece of metal to which a gemstone is cemented to facilitate handling during cutting and polishing.
Dop-wax—the agent or cement used to secure a gemstone to a dop-stick.
Emerald cut—a rectangular or square faceted stone with beveled corners whose surfaces are covered with several series of rectangular facets.
Eocene—a division of geologic time, estimated to be the time from 50 to 40 million years ago; one of the older divisions of the Cenozoic era.
Extrusive rock—igneous rock that has been extruded or forced out onto the earth’s surface.
Facet—a single plane polished surface on a faceted gem.
Facet head—a device used in the cutting and polishing of faceted gems; used to control the placement of facets and their relative angles (fig. 7).
Facet table—the equipment used in the cutting and polishing of faceted gems and the table on which most of the equipment is mounted (fig. 7).
Feldspar—a group of closely related silicate minerals including orthoclase, microcline, sanidine, plagioclase, labradorite, and others.
Fire—the reflections of variously colored light from a precious opal; also the different colors of light reflected from a faceted gem owing to the dispersion of the mineral.
Fracture—the texture of a freshly broken surface other than a cleavage surface, described as conchoidal, even, splintery, etc.
Gem—a cut and polished gemstone.
Gemology—the science dealing with the study of gemstones.
Gemstone—a mineral suitable for cutting into a gem; the term gemstones is frequently used collectively to include both cut and polished stones and rough stones.
Geode—a rounded or spherical rock cavity; commonly lined with crystals.
Girdle—the portion of a faceted gem separating the crown from the pavilion; the girdle may or may not be polished and usually contains about 2 percent of the total depth of the gem (fig. 6).
Gneiss—a coarse-grained metamorphic rock having segregations of granular and platy minerals that give it a more or less banded appearance without well-developed schistosity.
Grain (pearl grain)—a unit of weight equal to 0.05 gram or 0.25 carat; not the same as the Troy grain.
Granite—a granular igneous rock composed mostly of quartz, feldspar, and commonly mica and/or hornblende.
Hexagonal—having six angles and six sides; a crystal system in which the crystal faces are referred to four intersecting axes; three of these axes are equal, lie in the same plane, and intersect at angles of 60 degrees; the fourth axis is perpendicular to the other three.
Igneous rock—rock formed by solidification from a hot melt.
Index of refraction—a measure of the relative ability of a gemstone to “bend” incident light rays; sine of the angle of incidence of a light ray divided by the sine of the angle of refraction.
Intrusive rock—rock that has been pushed (usually in a molten state) among pre-existing rock strata, commonly along faults or fissures. Intrusive rocks do not reach the earth’s surface but are commonly exposed at the surface by later erosion.
Isometric—a crystal system in which the crystal faces are referred to three equal intersecting axes at right angles to each other.
Lap—a disc-shaped piece of metal or other material which is impregnated with diamond dust, or some other cutting or polishing agent, that is revolved while the gemstone is worked against it.
Lap plate—a metal plate to which a cutting or polishing lap is attached, usually by means of a threaded bolt and wing nut. The lap plate is attached to the shaft which is turned by the motor under the facet table.
Lapidary—one who practices the lapidary arts; a gem cutter.
Limestone—a sedimentary rock composed mostly of calcium carbonate.
Luster—the appearance of the freshly broken or unweathered surface of a mineral in reflected light (p. 5).
Main facet—as applied to the standard American brilliant cut, one of the first eight facets cut on either the crown or pavilion of a gem (fig. 6).
Matrix—the material in which a specific mineral is embedded; also the rock to which one end of a crystal is attached.
Metamorphic rock—rock that has been changed from i
                                                                                                                                                                                                                                                                                                           

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