Gemology Books Bibliography

Gemology Books Bibliography

Explore books on gems, gemology, jewelry and mineralogy in Four Treasures, the Lotus Gemology reference database. This bibliography brings together matching book records from the collection, with publication details, abstracts and cover images where available.

Gemology Book References

The list below matches books concerning gemology and related subjects in the database's searchable fields. Some works cover several branches of gems, jewelry or mineralogy.

2,801–2,820 of 3,630 matching references

“Reconstructed rubies” found to be synthetic corundum

Journal Article
Benson, L.B. (1953) “Reconstructed rubies” found to be synthetic corundum. Journal of Gemmology, Vol. 4, No. 1, January, pp. 1–10.
Record No. 456  |  ISBN/ISSN: 221252  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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Recently a number of stones have appeared on the market that were thought to be reconstructed ruby. Although the exact process used for the commercial production of synthetic corundum has been known for many years, the degree to which synthetic material may overlap in appearance the reconstructed stone is given little attention in present text books. In fact, little information has been published concerning the exact method used to produce reconstructed ruby.

Mandeville’s Travels

Book
Letts, M. (1953) Mandeville’s Travels. London, Hakluyt Society, 2 Vols., 554 pp.
Record No. 37  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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A scholarly edition of the medieval travel narrative attributed to Sir John Mandeville, bringing together several textual versions for comparison. Volume I presents the Egerton text in modernized English, preceded by Letts’s introduction and an essay by E.G.R.Taylor on medieval cosmographical ideas. Volume II contains the French Paris text with an English translation, the shorter Bodleian version, and supplementary passages from German and Latin versions and related sources. The narrative moves from pilgrimage routes and sacred sites in the Holy Land to accounts of distant Asian kingdoms, combining geographical information, descriptions of customs and religions, and fabulous peoples and natural wonders. For gemological history, it preserves influential traditions concerning precious stones, notably diamonds said to grow, reproduce, and derive nourishment from heavenly dew, together with beliefs in their protective powers. Such passages document medieval lapidary lore and European perceptions of Asian wealth. The edition’s comparative texts and historical apparatus make it useful for studying how geographical knowledge, borrowed accounts, religious traditions, and marvels were assembled and transmitted.

Augustine to Galileo | The History of Science | A.D. 400–1650

Book
Crombie, A.C. (1952) Augustine to Galileo | The History of Science | A.D. 400–1650. London, Heinemann, 2 Vols. (373 pp.).
Record No. 27337  |  ISBN/ISSN: 435541943  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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On its first publication in 1952, Augustine to Galileo was widely welcomed as having ‘removed for ever any excuse there may have been for ignorance of medieval scientific thought’. The book has since become a standard work, and the second (revised and enlarged) edition is now reissued with further corrections. Medieval scientific thought is deceptive both in its similarities to and in its differences from modern science. It was a series of actions in the great adventure of philosophical reformation that separates the classical world from our own. In the course of that adventure, as at all times in the history of science, one system of scientific thought gave place to another not merely because new facts were discovered, but more significantly because men began to ask new questions, to look at long-familiar evidence in a new way. Not only the origins but the nature of modern science can scarcely be understood without a knowledge of the period covered by this book. Dr. Crombie begins with an account of the remains of those Greek scientific conceptions found in the West after the fall of Rome, and of the new ideas about the natural world introduced with Christianity. He then traces the process of the recovery of Greek science from Byzantium and Islam, the assimilation of the new knowledge in the Latin West, the parallel development of technology, and the new conception of experimental science that was formed in the thirteenth and fourteenth centuries. The shifts in scientific thinking in the later Middle Ages emerge as a product of the empiricism of technology married to the methods of rational abstraction of mathematics and philosophy. These shifts prepared the ground for the final revolution brought about by Galileo and his contemporaries. A consideration of their work brings the author to his conclusion. Dr. Crombie is one of the most outstanding historians of science, and is University Lecturer in the History of Science at Oxford.

Jade in Mexico

Journal Article
Barber, R.J. (1952) Jade in Mexico. Gems & Gemology, Vol. 7, No. 5, Spring, pp. 147–150.
Record No. 3637  |  ISBN/ISSN: 0016626X  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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Barber examines the evidence for indigenous jade supplies in Mexico and argues that renewed commercial demand could encourage the rediscovery of their sources. He describes a trade in which rural inhabitants sell ancient carvings unearthed during cultivation to intermediaries who supply urban dealers and tourist shops. The limited availability of authentic objects, combined with visitors’ interest in ornamental stones rather than archaeological authenticity, has encouraged the sale of substitutes, including green glass marketed as Mexican jade. Barber suggests that a dependable market for newly collected material could stimulate prospecting and support a revived carving industry, particularly if country people were assured of payment for suitable stones found in streams and elsewhere. Distinguishing nephrite from fei cui, he identifies the latter as the principal material of ancient Mexican jade carvings, while reporting that some objects are nephrite. He challenges theories that American jade was imported from Asia or that similarities between carvings demonstrate an Asian origin for indigenous American cultures. His argument rests on reported chemical and optical differences between the jadeite mineral in Burmese and American materials, especially the greater calcium and magnesium components attributed to the latter, which he interprets as evidence for an American source. The archaeological distribution of jade extends from Sonora to Panama, with particularly abundant finds in Guerrero, Oaxaca, Chiapas, Veracruz, and Tabasco; however, Barber cautions that this distribution need not indicate numerous deposits, since exchange and the widespread esteem accorded jade could explain its dispersal. For Maya communities in the limestone country of Yucatán, he proposes supplies from the mountains of Oaxaca or Guatemala, obtained through southern and western neighbours. He illustrates jade’s importance through protective and medicinal amulets, funerary practices involving stones placed in the mouth and images deposited with the dead, traditions surrounding Quetzalcoatl, and Aztec tribute records specifying jade objects and their places of origin. Ancient exploitation, he argues, need not have involved recognizable bedrock quarries: river pebbles and boulders may have furnished much of the material, an interpretation supported by carvings whose outlines accommodate the original stone’s shape. Rough boulders reportedly recovered from Maya temple ruins, including one weighing approximately 200 pounds, and a reported river find from the eastern Oaxaca highlands provide further indications of raw material procurement. Throughout, Barber connects the archaeological question of jade supply with the practical economics of collecting, emphasizing that local knowledge and financial incentives would be central to locating workable material.

More news of synthetic red spinel

Journal Article
Gübelin, E.J. (1952–53) More news of synthetic red spinel. Gems & Gemology, Vol. 7, No. 8, Winter, pp. 236–247.
Record No. 2041  |  ISBN/ISSN: 0016626X  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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E.J. Gübelin reports successful production of ruby-red synthetic spinel by an adapted Verneuil process, revising his earlier conclusion that satisfactory cutting material was practically unobtainable. The investigation examines six faceted specimens ranging from 0.37 to 2.00 carats, with colors varying from metallic purple-red to an attractive ruby red. Gübelin attributes the advance to precise control of highly purified starting materials, an equimolar mixture of magnesia and alumina, chromium oxide as the coloring agent, and closely regulated temperature and material supply. Although the boules remained partly cracked and yielded relatively few flawless portions, they represented single crystals rather than aggregates. X-ray powder diffraction patterns of natural and synthetic red spinel corresponded closely in line positions and intensities. Measured lattice constants of approximately 8.084 Å for the synthetic material and 8.086 Å for the natural comparison confirmed their structural similarity but offered no practical means of distinguishing origin. Specific gravities ranged from 3.579 to 3.598, and refractive indices from 1.7191 to 1.7198, closely matching natural red spinel. The absorption spectrum likewise resembled that of natural material, with broad absorption extending approximately from 490 to 595 nanometers. Fluorescence provided a more useful distinction: the synthetic specimens showed dull red fluorescence under short-wave ultraviolet radiation and a brilliant red response under long-wave radiation. Their fluorescence spectrum contained a strong broad red band at approximately 685–690 nanometers and a faint satellite line near 678 nanometers, contrasting with the multiple lines described for natural red spinel. Microscopic examination supplied the clearest evidence of synthesis. Gas inclusions included spherical, distorted, elongated, and tadpole-shaped cavities, with minute bubbles concentrated into dense clouds or broad parallel bands. Distinct curved striae and growth bands occurred throughout the series, including in specimens lacking conspicuous bubbles. These features resembled those of synthetic corundum more closely than those commonly observed in conventional alumina-rich synthetic spinel. Gübelin relates their conspicuous development to difficulties in maintaining steady growth. Extinction between crossed polarizers varied with internal perfection: heavily included specimens displayed strong anomalous birefringence with feathery or banded textures, whereas cleaner stones showed complete or nearly complete extinction. He cautions that the combination of bubbles and curved bands could initially suggest synthetic ruby, making the absence of dichroism and examination of optical behavior important. The article establishes synthetic red spinel as a new identification problem while emphasizing that routine physical properties alone may closely reproduce those of natural material. Gübelin concludes by urging manufacturers to develop distinctive decorative materials whose appeal does not depend on resemblance to natural gems.

Unusual two and three phase inclusions in Ceylon sapphire

Journal Article
Hoagland, L.P. (1952) Unusual two and three phase inclusions in Ceylon sapphire. Journal of Gemmology, Vol. 3, No. 8, Oct., pp. 330–336.
Record No. 995  |  ISBN/ISSN: 221252  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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At a meeting of the Mineralogical Society held on 24ᵗʰ January, 1952, for the second time within a year a new gem mineral was described. On the former occasion only two small cut specimens of the mineral (taaffeite) were on view, these representing the whole of the world’s known supply; whereas in describing sinhalite Dr. G. F. Claringbull was able to produce a score of cut examples, some of them of considerable size. There was also one small pebble of rough, recovered by Dr. E. H. Rutland from samples of illam held by the lapidaries, Charles Mathews & Son.

Many reconstructed rubies found to be synthetic corundum

Journal Article
Benson, L.B. (1952) Many reconstructed rubies found to be synthetic corundum. Gems & Gemology, Vol. 7, No. 5, Spring, pp. 139–145.
Record No. 455  |  ISBN/ISSN: 0016626X  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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L.B. Benson reassesses the identification of reconstructed ruby, showing that many stones assigned to this category are synthetic corundum whose unusual features reflect growth conditions rather than the fusion of natural ruby fragments. He distinguishes reconstruction, defined as sintering natural fragments together under intense heat with or without pressure, from complete melting and subsequent crystal growth. A genuinely reconstructed stone should retain evidence of its fragmentary origin, potentially including natural inclusions, discontinuities in crystallographic orientation, and variations in hardness associated with bonding material. Benson questions historical accounts of substantial commercial production because securely documented specimens are scarce and early manufacturing methods remain uncertain. He suggests that some nineteenth-century “Geneva rubies” may have been early synthetic crystals rather than reconstructed aggregates. Intersecting curved striae, often cited as evidence of reconstruction, do not necessarily indicate separately oriented fragments. They can develop within a single crystal when the direction of deposition changes or growth is interrupted and resumed. The principal laboratory examples are heavily included rubies averaging approximately half to three-quarters of a carat, with abundant gas cavities and conspicuous intersecting curved striae. Investigation traced these stones to the bottom tips of synthetic boules, particularly those grown around oriented colorless rod seeds. Differences between growth structures in the seed and surrounding material explain the intersecting patterns, while color contrasts can produce patchy appearances. Concentrated elongated bubbles commonly extend perpendicular to growth lines and may spread outward in a fan from the rod, providing evidence of growth by progressive deposition. Benson reports that boule tips, commonly assumed to be waste, were being sold to overseas cutters, sometimes for more than flawless synthetic material, and apparently returned to the trade as cut stones potentially represented as natural ruby. Their visible imperfections could help them escape notice among natural stones. A second group consists of small, rounded, button-shaped boules long invoiced as reconstructed rubies. Cross-sections reveal orderly accumulated curved striae, gas bubbles, and synthetic seed material, supporting identification as early synthetic boules. Benson allows that cooling molten natural ruby could produce irregular swirls, but argues that this would not explain elongated gas bubbles consistently perpendicular to those lines. He concludes that most material identified as reconstructed in the trade is probably synthetic, while acknowledging reported examples retaining intact natural ruby. To reduce confusion, he recommends restricting “reconstructed” to stones consisting of sintered natural fragments that preserve characteristics indicative of natural origin.

ABC for Book Collectors

Book
Carter, J. (1952) ABC for Book Collectors. New Castle, Delaware, Oak Knoll Press, 224 pp.
Record No. 10  |  ISBN/ISSN: 1884718051  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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John Carter’s ABC for Book Collectors, first published in 1952, is an authoritative and often witty dictionary of the specialized terminology employed by antiquarian booksellers, bibliographers, auctioneers, and collectors of rare books. Drawing upon Carter’s extensive experience in the antiquarian book trade, the work was designed to explain the technical language and conventions encountered in booksellers’ catalogues and auction descriptions, particularly those that might confuse newcomers to book collecting. Rather than offering a general history of printing or an encyclopedia of bibliography, Carter concentrates on the vocabulary necessary to understand, identify, describe, evaluate, and purchase collectible books. Arranged alphabetically, the entries explain terms relating to editions, impressions, issues, states, bindings, paper, typography, illustration, provenance, condition, rarity, and bibliographical description. Particular attention is devoted to the frequently misunderstood distinctions between first editions, first impressions, and subsequent issues or states, together with the evidence necessary to establish their chronological priority. Carter also examines the identification of incomplete, altered, restored, or otherwise imperfect copies, explaining such terms as cancels, collation, conjugate leaves, inserted advertisements, facsimiles, and made-up copies. The extensive treatment of bookbinding encompasses historical materials and techniques, including calf, morocco, vellum, buckram, publisher’s cloth, decorative tooling, and the various forms of contemporary and later bindings. Equally useful are the discussions of condition and the subjective language employed by booksellers, from descriptions such as “fine” and “very good” to euphemisms that may conceal serious defects. Carter warns collectors against exaggerated claims of rarity, unsupported assertions of priority, misleading bibliographical descriptions, and the temptation to equate high prices with importance. His observations on auction practices, provenance, association copies, presentation copies, dust jackets, and the preservation of original bindings demonstrate a practical understanding of the factors influencing the desirability and commercial value of books. Throughout the work, technical definitions are accompanied by historical examples, occasional anecdotes, and pointed comments on the habits and pretensions of collectors and dealers. The book’s distinctive combination of scholarship, practical advice, and dry humor distinguishes it from more conventional bibliographical dictionaries. Following Carter’s death in 1975, Nicolas Barker revised and expanded the work, incorporating developments in bibliography, the antiquarian trade, and collecting practices while preserving much of the original author’s distinctive style. Although the book contains no substantive gemological information, it is particularly valuable to collectors of historical gemological literature, providing the terminology and bibliographical principles needed to distinguish original editions from later printings, recognize significant variants, evaluate the completeness and condition of rare volumes, and interpret antiquarian booksellers’ descriptions. It remains an important reference for anyone assembling, cataloguing, or studying a specialized library of rare and historical books.

Some additional data on Indian emeralds

Journal Article
Gübelin, E.J. (1951) Some additional data on Indian emeralds. Gems & Gemology, Vol. 7, No. 1, Spring, pp. 13–22, map.
Record No. 2038  |  ISBN/ISSN: 0016626X  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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Gübelin supplements earlier descriptions of Indian emeralds with a detailed examination of four faceted specimens, emphasizing the value of microscopic inclusions for distinguishing their origin. He outlines the discovery and development of emerald deposits in the Aravalli Mountains between Ajmer and Udaipur, particularly near Kaliguman and Bhilwara, where wartime prospecting for beryl and mica revealed emerald-bearing rocks. The emeralds occur in biotite schists associated with hornblende, talcose, and chloritic schists and probable pegmatitic intrusions. Gübelin compares this geological setting with deposits in the Urals, South Africa, and especially Austria’s Habach Valley. His four specimens, weighing 0.70–2.42 carats, display colours comparable to fine Colombian emeralds, although their lustre and visible inclusions vary. Because all were cut stones, he could not examine their original crystal forms directly, but inferred a conventional hexagonal prismatic habit from enclosed negative crystals. Refractive indices range from 1.580 to 1.598, with birefringence of 0.0075–0.009, and specific gravities range from 2.739 to 2.781. These comparatively high values resemble those of emeralds from the Urals and Transvaal but do not independently establish geographic origin. The stones show distinct to strong blue-green and yellow-green dichroism. Lighter specimens exhibit the usual emerald absorption spectrum, whereas darker examples show stronger absorption in the red region. All four remain green through the colour filters tested and are inert under ultraviolet radiation; the two lighter stones exhibit faint dull-red luminescence under X-rays. Gübelin concludes that these physical and optical properties must be supplemented by inclusion evidence. The most characteristic features are liquid-filled negative crystals containing movable gas bubbles, aligned parallel to the emerald’s optic axis. At lower magnification they appear rectangular, square, or comma-shaped; stronger magnification and darkfield illumination reveal their crystalline forms and show that the comma-like outlines arise from groups in which one elongated cavity projects beyond shorter companions. These two-phase inclusions are contrasted with the characteristic three-phase inclusions of Colombian emeralds. A second prominent inclusion type consists of biotite tablets and flakes oriented parallel to the basal plane, often with negative crystals arranged perpendicular to them. Minute actinolite rods and calcite crystals may also occur. The biotite association reinforces the comparison with emeralds from the Urals and Habach Valley, while the combined arrangement and morphology of the inclusions provide the principal distinguishing features described. Through numerous photomicrographs, the article presents an early framework for recognizing Indian emeralds by relating their internal features to their geological environment and measurable gemmological properties.

Australian sapphire fields not fully exploited

Journal Article
Stratton, V. (1951) Australian sapphire fields not fully exploited. Gems & Gemology, Vol. 7, No. 4, Winter, pp. 125–128.
Record No. 1656  |  ISBN/ISSN: 0016626X  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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V. Stratton surveys the sapphire fields around Rubyvale in the Anakie district of central Queensland, presenting them as an extensive but incompletely developed resource whose prospects depend on stronger markets and improved mining methods. The fields are described as covering approximately 1,200 square miles, about 192 miles west of Rockhampton. Despite important discoveries and growing American interest, mining remains small in scale, intermittent, and largely dependent on individual miners using simple equipment. Sapphires occur in old river gravels from the surface to depths of about 50 feet. Miners sink shafts in promising ground, extract the sapphire-bearing material, and wash it through sieves; an illustrated example uses a spring sieve in a 100-gallon water tank. Stratton reports that no more than about 50 men are mining in the district at any one time, with low financial returns discouraging sustained work and making the field’s potential difficult to assess. The account contrasts occasional valuable finds with the modest circumstances of the mining community. It describes veteran miners, individual claims, accumulated stocks of rough material, and substantial differences between owners’ expectations and buyers’ valuations. Yellow or golden sapphires receive particular praise, while green stones are also described as high quality. Blue sapphires, although prominent in the world market, are generally considered too dark for buyers favoring lighter material, and American purchasers are reported to show greater interest in green stones than in ordinary dark blues. Two recently recovered golden sapphires are each valued at approximately 1,500 Australian pounds, while the Black Star of Queensland, reportedly once used as a doorstop, illustrates the publicity generated by exceptional discoveries. James and Harry Kazanjian’s acquisition of five Rubyvale sapphires is cited as evidence of American attention. Arthur Wirth, president of the New South Wales branch of the Gemmological Association of Australia, anticipates possible American investment in bulldozers and open-cut mining to work the gravels more extensively. His forecast rests partly on uncertainty surrounding supplies from Thailand. Stratton nevertheless records a less active immediate situation: in August 1951, production was virtually at a standstill because many regular miners had left for better-paid work, including timber cutting and kangaroo shooting. The article combines observations of mining practices and local life with an optimistic assessment of future development, while showing that market preferences, labor availability, and miners’ returns constrained exploitation.

Gemological Digests: Repeated twinning lines seen in synthetic corundum

Journal Article
Anonymous (1951) Gemological Digests: Repeated twinning lines seen in synthetic corundum. Gems & Gemology, Vol. 7, No. 1, Spring, p. 25.
Record No. 292  |  ISBN/ISSN: 0016626X  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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This digest reports repeated twinning lines in synthetic corundum examined at the Gem Trade Laboratory of the Gemological Institute of America, challenging the assumption that such features establish natural origin. The principal example is a transparent blue synthetic sapphire discovered during the identification of a group of blue stones. It displayed both curved striae, regarded as evidence of synthetic origin, and repeated twinning lines, previously considered exclusive to natural material. The accompanying photograph records the coexistence of these features in the same specimen. An earlier laboratory observation involved a yellow synthetic sapphire with a single line described as a repeated twinning line. Subsequent examination of both the yellow and blue sapphires in a polariscope revealed irregular extinction resembling that of naturally occurring repeatedly twinned corundum. Thus, neither the visible twinning features nor the associated extinction behavior provided an exclusive distinction between natural and synthetic stones. A further example appeared only a few days later, when a dealer submitted a 5.6-carat cabochon ruby showing prominent repeated twinning lines. The dealer had purchased it as natural specifically because of these features, but laboratory examination identified it as synthetic. Its dark color prevented an adequate photograph for publication. Together, the three observations demonstrate the practical danger of accepting a familiar structural feature as sufficient evidence of natural origin without continuing the search for indications of synthesis. The blue sapphire is particularly instructive because its curved striae and twinning lines bring two previously contrasting identification criteria together within one stone. The ruby illustrates the commercial consequence of relying on twinning alone: a synthetic specimen had already been purchased under an incorrect identification. The digest therefore advises further examination for synthetic features whenever repeated twinning is observed, rather than treating its presence as conclusive. It also draws an educational distinction between the curved pattern of striae and the crystallographic organization of synthetic corundum, cautioning against the beginner’s assumption that crystallization itself follows those curves. The report presents these cases as a correction to identification practice, extending the recognized range of structural appearances in synthetic ruby and sapphire.

A Study of Classic Maya Sculpture

Book
Proskouriakoff, T. (1950) A Study of Classic Maya Sculpture. Washington, DC, Carnegie Institution, 209 pp.
Record No. 28711  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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Two important studies in Maya archaeology form the foundation of this book: A Study of Maya Art: Its Subject Matter and Development, by Herbert J. Spinden (1913); and The Inscriptions of Peten, by Sylvanus G. Morley (1937–38). The first established, with notable success, a series of stylistic changes in sculpture at a number of the larger Maya sites; the second provided epigraphic decipherments which permitted the dating of many more monuments in the Peten than was formerly possible. With this much more substantial body of dated material than was available at the time of Spinden’s study, we are now able to confirm many of his findings and to elaborate the basis of stylistic appraisal, extending it to all Classic Maya sites. It is because so much reliance has been placed on Morley’s epigraphic work that disagreements between his stylistic appraisals and mine have been stressed in this book. This, however, should not be construed as a derogation of his conclusions, which rest primarily on epigraphic sources. Our differences serve only to indicate the need to establish definite and significant style characteristics on which future discussion can be based. This is the principal aim of this study; it would have been futile to pursue it without the collection of epigraphic data and interpretation which Morley’s work makes available.

Maya Hieroglyphic Writing: Introduction

Book
Thompson, J.E.S. (1950) Maya Hieroglyphic Writing: Introduction. Washington, DC, Carnegie Institution, 347 pp., many plates
Record No. 28577  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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Introduction to the Mayan writing system, including many mentions of jade.

Are synthetic red spinels available?

Journal Article
Gübelin, E.J. (1950) Are synthetic red spinels available? Gems & Gemology, Vol. 6, No. 10, Summer, pp. 307–309, 322.
Record No. 2036  |  ISBN/ISSN: 0016626X  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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E.J. Gübelin investigates whether synthetic red spinel was commercially available, correcting a statement in A.K. Seemann’s 1949 account of American synthetic crystals that listed ruby-red and garnet-red spinel among available colors. Literature review and correspondence with W.F. Eppler establish a distinction between the experimental possibility of producing red spinel and the practical manufacture of transparent, durable material suitable for cutting and sale. Gübelin explains that conventional Verneuil production of single-crystal spinel requires a substantial excess of alumina over the equimolar proportions of magnesium oxide and aluminum oxide represented by natural spinel’s formula, MgAl₂O₄. Attempts using the natural proportions instead produce aggregates of differently oriented crystals that crack readily on cooling. Commercial synthetic spinel may contain approximately 3.5 moles of alumina per mole of magnesia. This compositional difference affects the colors produced by added metal oxides: a coloring agent need not impart the same hue to spinel and corundum because their crystal structures differ. Chromium, responsible for red ruby and natural pink spinel, produces dark green in the alumina-rich synthetic spinel under discussion. Gübelin reviews the characteristic absorption and fluorescence associated with chromium and describes contrasting thermal behavior in ruby and green synthetic spinel. Ruby becomes green at approximately 500–600 °C but recovers its original red color on cooling. Green synthetic spinel undergoes precipitation of excess alumina at approximately 950–1050 °C, becoming cloudy; above about 1075 °C, structural changes can produce red coloration accompanied by deterioration of transparency and gem quality. The article interprets these effects through the behavior of chromium-bearing alumina within different crystal structures. M.T. Mackowsky’s published observations and Eppler’s experimental experience agree that red synthetic spinel can be obtained when magnesia and alumina are maintained near a 1:1 molar ratio, but the resulting specimens are generally tiny, cracked, or shattered. Eppler reports that increasing the alumina content toward the proportions needed for satisfactory commercial boules immediately changes the color from red to green. Gübelin therefore concludes that red synthetic spinel is producible in principle, while satisfactory cutting material had not been established as a commercial product at the time of writing. He regards Seemann’s listing as an overlooked error, while allowing that future technical advances might overcome the manufacturing difficulties.

Cleavage and the structure of gem minerals

Journal Article
Mitchell, R.K. (1950) Cleavage and the structure of gem minerals. Journal of Gemmology, Vol. 2, No. 6, April, pp. 251–252.
Record No. 1284  |  ISBN/ISSN: 221252  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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The relationship between crystal structure and splitting behaviour in gem minerals is examined through discussion of spinel, corundum and chrysoberyl, with particular attention to the distinction between cleavage and parting. Cleavage is attributed to the atomic arrangement and bonding of a crystal and is theoretically reproducible down to atomic dimensions, whereas parting occurs along comparatively coarse discontinuities such as twin planes, structural faults or defects. Corundum illustrates the difficulty of applying this distinction. Its rhombohedral splitting is described, following Miers, as associated with lamellar twinning, potentially produced by pressure and movement along glide planes. Basal parting is attributed to incipient decomposition and microscopic cavities along planes susceptible to solution, while a less distinct prismatic parting is also recognised. Corundum has an approximately hexagonal close-packed oxygen arrangement, with aluminium occupying octahedral sites, and its three parting directions parallel principal directions of atomic layering. Strong aluminium–oxygen bonding helps explain why splitting is difficult to produce in most gem specimens; crystals exhibiting pronounced twinning or decomposition are generally unsuitable for gem use. Synthetic spinel is noted to show a tendency towards cubic cleavage, tentatively associated with excess gamma alumina in its structure. Gamma alumina, a synthetic polymorph possessing the spinel structure, is also discussed in connection with wartime manufacture of industrial cutting and abrasive tools. Spinel boules containing excess alumina in solid solution could be shaped and subsequently hardened through a process converting that alumina to the corundum structure, producing tough material with little tendency to cleave. Chrysoberyl is compared with olivine because of their similar crystal habits, dimensions and fundamental structures, as established by X-ray analysis. Beryllium occupies tetrahedral coordination sites corresponding to silicon in olivine, while aluminium occupies octahedral sites corresponding to magnesium. Although beryllium–oxygen and aluminium–oxygen bonds are considered similarly covalent, the smaller beryllium atom forms stronger bonds distributed among four oxygen neighbours rather than six. Cleavage is consequently expected along planes involving the relatively weaker aluminium-linked portions of the structure, an interpretation consistent with chrysoberyl’s imperfect (010) cleavage. Its second imperfect cleavage, (011), is less readily explained, particularly because the corresponding cleavage apparently does not occur in olivine, and the discrepancy is left for subsequent discussion.

American synthetic crystals – Sapphire to titania

Journal Article
Seemann, A.K. (1949) American synthetic crystals – Sapphire to titania. Gems & Gemology, Vol. 6, No. 5, Spring, pp. 151–159.
Record No. 1573  |  ISBN/ISSN: 0016626X  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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A.K. Seemann reviews the development of American synthetic crystal production during and after the Second World War, explaining the manufacture, properties, and commercial applications of corundum, spinel, star corundum, and titania. Adapted from a presentation to the American Gem Society’s 1949 conclave, the article describes how wartime demand for instrument bearings stimulated a domestic industry that subsequently developed new crystal forms and gemstone materials. The basic Verneuil process is outlined: finely prepared oxide powder passes through an oxyhydrogen flame, melts, and crystallizes on a progressively lowered support. Control of powder supply, flame conditions, and lowering rate determines the growth and dimensions of the boule. Seemann discusses powder preparation by calcining purified salts, the introduction of coloring agents, and the importance of purity, noting that some contaminants become visible even at concentrations of a few parts per million. Chromium produces ruby, while titanium and iron additions produce blue sapphire; various metal oxides provide colors in synthetic spinel. A major American advance was the growth of long, cylindrical sapphire rods, reducing the labor and material loss involved in converting conventional split boules into small bearings. Studies connected crystallographic orientation with splitting, transverse cracking, and deformation at high temperatures. Near the melting point, rods could be bent or stretched, with material oriented at approximately 45° between the c-axis and growth direction proving easiest to deform. Flame polishing offered an economical means of obtaining smooth surfaces and rounded phonograph-needle tips, whose service life also depended strongly on crystal orientation. High-temperature annealing permitted larger whole boules to be worked without splitting. Additional applications included precision sapphire balls for pen tips and decorative use. Seemann identifies synthetic star ruby and sapphire as a particularly striking development, attributing their asterism to fine needles while withholding the manufacturing method pending patent action. The final section treats titania, synthetic rutile, emphasizing its exceptionally high refractive indices and dispersion alongside its relative softness and cutting difficulties. Produced by a modified Verneuil process, the initially black, opaque, oxygen-deficient crystals become transparent after heating in an oxidizing atmosphere, with a corresponding large increase in electrical resistance. The material’s potential applications therefore extend beyond gems to monitoring furnace atmospheres. For gemstone use, crystal orientation, accurate facet angles, and suitable polishing procedures are essential to avoid a cloudy appearance and excessive rounding of facet junctions. Seemann recommends alumina for final polishing and cautions against overheating during sawing, cutting, or polishing because changes in oxidation state can cause discoloration or fracture. The article presents gemstone synthesis and industrial crystal engineering as closely connected fields, with advances in growth control, orientation, annealing, and finishing supporting both jewelry and technical applications.

Observations on reconstructed rubies

Journal Article
Gübelin, E.J. (1949) Observations on reconstructed rubies. Gems & Gemology, Vol. 6, No. 6, Summer, pp. 186–187.
Record No. 879  |  ISBN/ISSN: 0016626X  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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E.J. Gübelin describes microscopic features used to distinguish reconstructed rubies from natural rubies and synthetic material, relating their internal appearance to the fusion and subsequent cooling of natural ruby fragments. He argues that identification should concentrate on internal structures because reconstruction differs from both geological formation and the growth of synthetic ruby. Although the starting fragments are natural, their original inclusions, such as rutile silk, mineral crystals, and fluid feathers, should generally disappear during melting; preservation would be exceptional, chiefly where fragments were merely joined rather than fully melted. Conversely, the regularly curved growth striae characteristic of synthetic ruby need not occur because reconstruction does not involve the periodic deposition of molten droplets. Gübelin instead emphasizes irregular curved swirls formed within the viscous moving mass as it cooled and recrystallized. These can initially resemble features in synthetic ruby or even red glass, making preliminary determination of refractive indices, density, and absorption spectrum important. Closer examination shows that the swirls have strongly curved, unusually short radiating elements, arranged in groups that meet at sharp angles. Their marked irregularity contrasts with the comparatively parallel curved striae of synthetic ruby. Air entering the heated material produces abundant gas cavities, predominantly spherical but also elongated, angular, and unusually shaped. Some closely resemble the liquid-filled tubes, channels, and other cavities encountered in natural gemstones, creating a risk of misidentification. Gas inclusions may also combine into undulating veils or featherlike systems that imitate natural fluid feathers. Gübelin states that these deceptive formations are accompanied by individual bubbles and remain black when viewed from different directions, whereas natural liquid inclusions become transparent at a suitable viewing angle. A further feature described in cabochon-cut reconstructed rubies is a dense network of minute air-filled fissures immediately beneath the domed surface. He attributes this network to the release, during cutting, of internal strain generated by rapid cooling, and reports that comparable formations had not been observed in natural or synthetic ruby. The article presents the combined character of irregular swirls, abundant gas inclusions, deceptive featherlike arrangements, and subsurface fissures as diagnostic evidence of reconstruction, supported by examinations conducted in Gübelin’s Lucerne laboratory and illustrated by accompanying photomicrographs.

Reconstructed rubies in rod and faceted form

Journal Article
Alexander, A.E. (1949) Reconstructed rubies in rod and faceted form. Gems & Gemology, Vol. 6, No. 6, Summer, pp. 184–185.
Record No. 224  |  ISBN/ISSN: 0016626X  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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A.E. Alexander investigates the existence and identifying features of “reconstructed” ruby, reporting an experimental rod made from natural ruby fragments and a faceted stone independently judged to have a similar origin. The inquiry arose from repeated encounters with rubies submitted as reconstructed material that proved to be synthetic, leaving Alexander doubtful whether reconstruction was commercially or technically genuine. To test the possibility, he assembled 14 carats of natural ruby chips selected for good color and identifiable natural inclusions, including rutile needles, and submitted them to A.K. Seeman of Linde Air Products Company. Instead of being fused directly into a mass suitable for faceting, the chips were ground to 200 mesh and made into a rod approximately 1½–2 millimeters in diameter and 41 millimeters long. A section was examined longitudinally with a binocular microscope and subsequently prepared as a thin section for petrographic study. Fusion produced a slight loss of color and eliminated recognizable evidence of the original mineral inclusions, even during examination at 450× and 900×. The rod contained spherical and irregular gas cavities, cometlike inclusions with distinct tails arranged in a broadly fan-shaped pattern, and curved growth lines transverse to its length. Its c-axis lay approximately 70° from the rod’s length, while examination between crossed polarizers revealed occasional grains oriented differently from the surrounding mass. During this investigation, a dealer submitted a 1.28-carat faceted ruby that initially resembled an early Verneuil synthetic. Examination by immersion in alpha-monobromonaphthalene instead led Alexander to identify it as reconstructed. Following donation of the stone to the Gem Trade Laboratory, it was examined in July 1948 by B.W. Anderson and E.J. Gübelin at Gübelin’s Lucerne laboratory; both agreed with that interpretation. Features described include peculiar swirl markings, some sharply terminated, four distinct undulating veils, gas cavities, and other inclusions resembling those encountered in natural corundum. Recorded properties were refractive indices of 1.760–1.767, specific gravity of 4.00, bright red fluorescence under ultraviolet radiation and X-rays, and the characteristic ruby absorption spectrum. The article presents these observations as evidence that reconstructed ruby can exist in both rod and faceted forms, while showing that the fusion process can create features resembling synthetic corundum and destroy recognizable inclusions inherited from the natural starting material.

Geology of India and Burma

Book
Krishnan, M.S. (1949) Geology of India and Burma. Madras, Madras Law Journal Press, 544 pp.
Record No. 151  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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M.S. Krishnan’s Geology of India and Burma is a comprehensive survey of the geological structure, stratigraphy, tectonics, and mineral resources of the Indian subcontinent and Burma (Myanmar), incorporating the findings of the Geological Survey of India and other geological investigations. The work begins with an examination of the physical geography and structural features of the region, including the Himalayas, the ancient crystalline rocks of Peninsular India, the Indo-Gangetic plains, and the complex mountain belts of Burma. It then presents a systematic account of geological formations from the Archaean through the Pleistocene, discussing their distribution, lithology, fossil contents, structural relationships, and economic significance. Particular attention is devoted to the ancient metamorphic and igneous rocks of southern India, Rajasthan, and the Eastern Ghats, together with the geological formations of the Himalayan and Burmese mountain belts. Of special gemological interest are the sections dealing with corundum, beryl, garnet, tourmaline, spinel, zircon, and other gem minerals. Krishnan describes corundum occurrences associated with highly metamorphosed aluminous rocks and ultrabasic intrusions in southern India, including the Salem district of Tamil Nadu and parts of Andhra Pradesh, Karnataka, and Odisha. The discussion of Burma’s Mogok Stone Tract is particularly important. Krishnan identifies the crystalline complex of the Mogok region as consisting principally of gneisses and schists, including calc-silicate rocks and crystalline limestones, together with granitic and other igneous intrusions. He describes the metamorphic mineral assemblages associated with ruby and sapphire occurrences, including calcite, diopside, scapolite, forsterite, spinel, garnet, and other minerals. Ruby is associated particularly with crystalline limestone and calc-silicate rocks, while sapphire, spinel, tourmaline, zircon, and other gemstones are recorded from the region. Krishnan notes the long history of ruby mining in the Mogok district and the continued importance of its gemstone production. The broader survey of mineral resources includes references to precious and semiprecious stones such as moonstone, peridot, aquamarine, amethyst, topaz, cat’s-eye, and garnet, as well as the diamond deposits of India. The diamond-bearing formations of the Vindhyan System receive particular attention, including the historic workings around Panna in Madhya Pradesh and the occurrence of diamonds in conglomerates and associated geological formations. Krishnan also discusses the geological conditions of the diamond-bearing districts of southern India and their relationship to ancient sedimentary deposits and volcanic rocks. Throughout the work, mineral occurrences are considered within their geological and structural settings rather than simply as isolated localities. Numerous geological maps, stratigraphic tables, diagrams, and bibliographies accompany the regional descriptions. The book provides a valuable historical synthesis of geological knowledge in India and Burma during the first half of the twentieth century, particularly for understanding the geological environments of important ruby, sapphire, diamond, and other gemstone deposits before the development of modern plate-tectonic interpretations.

A Handbook of Precious Stones

Book
Iyer, L.A.N. (1948) A Handbook of Precious Stones. Calcutta, Baptist Mission Press, 188 pp.
Record No. 3184  |  Sinkankas/Born No.: 3151; NIB  |  RWHL
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Sinkankas: A fairly complete general treatment of gemology written in popular terms and presumably meant to replace or supplant the somewhat similar publications above, especially insofar as Iyer emphasizes the gemstones that occur in India, Burma, and Ceylon. The first part treats principles and is followed by a second part on descriptions. Because of the author’s familiarity with native gemstones, this work remains a valuable reference. Commendable features include descriptions of native mining methods used, histories of previous mining attempts in the countries named, and a bibliography that is large, detailed, and paginated! This work is scarce.

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