Fact-checked by Grok 2 weeks ago

Grossular

Grossular is a calcium-aluminum belonging to the group, with the Ca₃Al₂(SiO₄)₃. It crystallizes in the cubic system, typically forming dodecahedral or trapezohedral crystals, and exhibits a vitreous to resinous luster, a Mohs of 6.5–7, and a specific of approximately 3.59. Grossular is notable for its wide color range, from colorless and white (when pure) to shades of green, yellow, orange, red, brown, pink, and even black, influenced by trace impurities such as iron, , and ; it shows the broadest color spectrum among species. As a member of the series, grossular forms complete solid solutions with (Ca₃Fe₂Si₃O₁₂) and partial ones with and , but it is end-member pure in many specimens. It lacks true , instead parting irregularly on {110}, and displays an uneven to , with brittle . Optically isotropic with a of 1.734, grossular is transparent to opaque and may fluoresce weakly golden yellow under light. Grossular primarily occurs in contact and regional metamorphic environments, including marbles, calc-silicate rocks, schists, and serpentinites derived from calcium-rich protoliths, often associated with minerals like , , , , , and . Notable gem varieties include tsavorite, a vivid form colored by and , prized for its emerald-like hue and sourced mainly from East African deposits in and ; and hessonite, the orange to brownish variety due to iron, historically known as "cinnamon stone." These varieties, along with colorless or pale types, are valued in jewelry for their and brilliance, though grossular has limited industrial use compared to other garnets like .

Nomenclature and varieties

Etymology

The name grossular derives from the Latin grossularia, the botanical name for the (Ribes grossularia), owing to the greenish hue of its typical variety that resembles the fruit. German mineralogist first described the mineral in 1803 from specimens collected in , initially naming the brownish-orange form Kanelstein ( stone) in reference to its color. In 1808, Werner renamed it grossularite to encompass the green specimens more accurately, later shortened to grossular. This naming distinguished it within the broader group—named from Latin granatus for seeds due to crystal shape— as the primary calcium-aluminum end-member among related . Historical variations like "cinnamon stone" persisted for the hessonite-like variety before formal classification, highlighting early recognition of its color diversity. Later, specific varieties such as received names tied to their discovery sites, like Tsavo National Park in 1967.

Principal varieties

Grossular, a calcium-aluminum in the group, exhibits a wide range of colors due to trace impurities, leading to several principal varieties distinguished by their hues, , and gemological characteristics. These varieties include hessonite, , hydrogrossular, and lesser-known forms such as leucogarnet, rosolite, and yellowish types, each colored primarily by iron, , , or substitutions. Unlike magnesium-rich garnets like , which are typically deep red and found in kimberlites, grossular varieties are calcium-dominant and occur in metamorphic or environments, avoiding confusion with due to their distinct chemistry and lighter tones. Hessonite, also known as "cinnamon stone," is the orange-brown variety of grossular, characterized by its translucent to transparent appearance and warm, honey-like glow often described as resembling "whiskey in water." The color arises from iron (Fe³⁺) impurities, with higher iron content increasing the reddish tones. It has a Mohs hardness of approximately 7, slightly softer than some other garnets, and a ranging from 1.74 to 1.75, making it suitable for into gems despite occasional inclusions. Historically prized in ancient jewelry, hessonite's value depends on color saturation, with vivid orange specimens commanding higher prices. Tsavorite represents the vivid green, transparent variety of grossular, prized for its emerald-like brilliance and high clarity. The intense green hue results from substitutions of and , with vanadium often predominant (V₂O₃:Cr₂O₃ ratio >1:1). Discovered in near Komolo in Tanzania's Lelatema Hills and later in , it was named after Tsavo National Park by . With a of 6.5–7.5 and of 1.731–1.754, is durable for jewelry and highly valued, often fetching $400–$2,000 or more per for fine, eye-clean stones over 1 . Hydrogrossular is the massive, opaque to translucent green variety, featuring hydroxyl (OH) substitutions in its structure that distinguish it within the grossular-katoite series. Its green color stems from iron or traces, often with black inclusions giving a speckled appearance resembling . Primarily sourced from , it is too opaque for faceting but valued for carvings, beads, and cabochons due to its 6.5–7 hardness and affordability. Other notable varieties include leucogarnet, a colorless form representing nearly pure grossular without significant impurities, ideal for transparent gems; rosolite, a rare pinkish variety colored by ; and yellowish types, sometimes referred to as Merelani grossular, resulting from minor iron content. These less common forms highlight grossular's color spectrum from iron (yellow-orange), chromium-vanadium (green), to (pink), but they are generally lower in demand compared to hessonite and .

Crystal structure and properties

Crystal structure

Grossular crystallizes in the ( with \overline{3}d (No. 230). The unit cell is cubic with a lattice parameter a ≈ 11.85 and contains eight units (Z = ). In this structure, calcium cations occupy 24 dodecahedral sites, aluminum cations fill 16 octahedral sites forming [AlO6] polyhedra, and silicon occupies 24 tetrahedral sites as [SiO4] tetrahedra, all interconnected by shared oxygen anions to form a three-dimensional framework. A notable variation occurs in hydrogrossular, where partial substitution of [SiO4]4- by [(OH)4]4- (or H4O4) disrupts the regular tetrahedral arrangement, often resulting in lower symmetry and a massive, non-crystalline habit rather than well-formed crystals. Grossular typically exhibits dodecahedral or trapezohedral crystal habits, though it can also form granular masses or compact aggregates. This structural arrangement contributes to its characteristic hardness of 6.5–7 on the Mohs scale.

Physical and chemical properties

Grossular is a member of the group with the ideal Ca₃Al₂(SiO₄)₃, representing the calcium-aluminum end-member composition. Minor substitutions, such as Fe³⁺ replacing Al³⁺ at the octahedral site, can occur in natural specimens, though these are typically limited and do not significantly alter the core structure. The mineral exhibits a Mohs of 6.5 to 7, which, combined with its good toughness, renders it suitable for applications despite its brittleness. Its specific gravity ranges from 3.59 to 3.64, reflecting the dense packing of its isometric crystal structure. Grossular displays a vitreous to resinous luster and produces a white streak when tested on an unglazed plate. Grossular lacks true , instead fracturing conchoidally to unevenly under . It demonstrates high . Chemically, grossular is insoluble in common acids such as , though hydrogrossular varieties, which incorporate hydroxyl groups, show increased reactivity due to their hydrated structure.

Optical properties

Grossular, a member of the group, exhibits isotropic optical behavior typical of cubic crystals, with no under standard conditions, though weak strain birefringence may occur due to internal stresses. Its refractive index ranges from 1.731 to 1.754, varying by composition and variety; for instance, the chromium-bearing variety often shows values around 1.743, slightly higher due to the influence of Cr³⁺ ions. The dispersion of grossular is moderate at 0.028, contributing to subtle in faceted stones but less pronounced than in other garnets. is generally absent, but weak effects can appear in colored varieties, such as a slight yellow-green shift in green when viewed along different axes. Absorption spectra in grossular depend on trace elements: green varieties like display characteristic chromium-related bands near 440 nm, causing broad absorption below approximately 490 nm, while iron-influenced brown specimens show bands around 530 nm. is typically inert or weak, producing a golden yellow to orange-red glow under long-wave or short-wave light in some specimens, particularly those with or impurities. In gemological testing, grossular is distinguished from similar green garnets like demantoid (andradite variety) by its lower (0.028 versus 0.057), resulting in reduced fiery , alongside confirmatory and lack of characteristic horsetail inclusions.

Geological occurrence

Formation

Grossular primarily forms through contact or regional of impure limestones or siliceous sediments, where calcium-rich protoliths react with silica and alumina under elevated temperatures and pressures. In these settings, particularly in skarns developed at the margins of igneous intrusions, grossular crystallizes as part of calc-silicate assemblages, often alongside minerals such as , , , and . These processes typically occur at temperatures between 500 and 700°C and low to medium pressures (generally below 7 kbar), with hydrothermal fluids playing a key role in facilitating metasomatic reactions that concentrate calcium and aluminum. Secondarily, grossular can form in bodies or altered basic rocks through , where fluids rich in calcium and silica interact with ultramafic or protoliths during serpentinization or rodingitization. As the calcium-aluminum end-member of the group, grossular is characteristic of these calc-silicate environments, stabilizing in assemblages that reflect the availability of CaO and Al₂O₃ under the prevailing conditions. Varieties like hydrogrossular may develop in such altered, low-temperature hydrothermal settings.

Major deposits

Grossular is primarily extracted from metamorphic deposits worldwide, with significant concentrations in regions of contact metamorphism. The most prominent sources of gem-quality grossular, particularly the vibrant green variety, are located in , especially and . Mining in the Merelani Hills of northern Tanzania began in the 1970s following the discovery of tsavorite in 1967 near Tsavo in Kenya, and these areas remain the epicenter of production. Kenya's tsavorite output from sites like the Mwatate region drives much of the global supply. In , the Jeffrey Mine in (now ), , has historically yielded exceptional grossular specimens, including hydrogrossular and green varieties, from its asbestos operations that ceased in 2001 but continue to provide collector material. The mine's skarn-hosted deposits produced lustrous, gemmy crystals up to several centimeters, renowned for their clarity and color range from peach to deep green. South Africa's region, particularly around , is a key locality for hydrogrossular, a massive, translucent variety often marketed as "Transvaal jade" due to its jade-like appearance in green and gray-green hues. These deposits, formed in serpentinized ultramafic rocks, have been exploited since the early for ornamental stone. Other notable deposits include hessonite grossular from Sri Lanka's gem gravels and India's and regions, where cinnamon-brown crystals are recovered from alluvial sources. In , the Vilui River Basin in produces the olive- viluite variety, a less common grossular type linked to alkaline intrusions. In the United States, occurrences in California's Inyo County and Vermont's Belvidere Mountain Quarries yield diverse grossular forms, including transparent and crystals from asbestos-associated skarns. As of 2025, sustainable mining initiatives in East Africa's districts continue to gain momentum, including efforts by organizations like to improve artisanal practices, reduce environmental impact, and enhance community health in and Tanzania's operations.

Applications and cultural significance

Gemstone and industrial uses

Grossular garnet, particularly its transparent varieties such as and hessonite, is highly valued in jewelry for faceting into gems that showcase their vibrant colors and brilliance. , with its intense green hue, is typically cut into faceted shapes like ovals and cushions to maximize light return, making it suitable for high-end pieces such as engagement rings and necklaces. Hessonite, known for its warm orange to reddish tones, is also faceted but often exhibits a distinctive "cinnamon stone" effect due to inclusions, which adds character without detracting from its appeal in earrings and pendants. The value of grossular gems is primarily determined by color intensity, clarity, and size, with premium examples commanding higher prices. For , vivid green shades free of brownish tones are most desirable, while clarity is generally good in stones under 2 s, though inclusions like pockets can appear in larger specimens; prices typically range from $400 to $2,000 per for faceted stones of 1-2 s, escalating significantly for rarer sizes over 2 s. Hessonite values emphasize rich, unbrownish orange hues and moderate clarity, as eye-visible inclusions are common but acceptable, with prices generally lower than due to greater availability. Opaque varieties, such as those with or translucency, are often cut as cabochons to highlight surface effects, suitable for bold statement jewelry. In industrial applications, grossular garnet contributes to abrasives and , leveraging its of 6.5-7.5 on the for effective material removal without excessive wear. Since the late 19th century, grossular has been used alongside other -group minerals in abrasive powders for grinding and polishing metals and , though remains more dominant. In , abrasives, including grossular varieties, are propelled with high-pressure water to precisely slice metals, stone, and composites in , prized for their durability and low dust production. Grossular also finds niche use in refractories for , where its calcium-aluminum composition provides thermal stability in high-temperature environments like furnace linings. Ornamental applications highlight hydrogrossular, the massive, translucent to opaque variety often resembling , which is carved into decorative objects such as spheres, skulls, and figurines to exploit its mottled green appearance and mid-range hardness. These carvings, sourced mainly from , serve as affordable jade substitutes in sculptures and inlays. Hydrogrossular is also fashioned into beads for necklaces and bracelets, valued for their earthy tones and durability in strung jewelry; historically, grossular varieties have been used in intaglios and cameos for seals and adornments since ancient times. Market trends for grossular reflect growing demand in the colored gem sector, with the global projected to expand from USD 737 million in to USD 1.07 billion by 2033 at a CAGR of about 4.8%, driven by jewelry and industrial needs. , as a grossular , sees heightened interest in ethical sourcing from East mines, where initiatives promote to ensure conflict-free origins and community benefits. technology is increasingly adopted for supply chains, including , to provide verifiable provenance from mine to , enhancing and supporting sustainable practices. Treatments for grossular are rare, with most gems entering the market untreated to preserve their natural appeal. , applied sparingly to hessonite, involves controlled heating to intensify orange hues and reduce inclusions, resulting in more vibrant colors that are stable and undetectable without advanced testing. Such enhancements are uncommon for , which is prized for its untreated, vivid green.

Cultural significance

Grossular garnet has been utilized in historical artifacts, particularly in ancient . Archaeological evidence from reveals worked , including varieties of grossular such as hessonite, used in beads and seals as part of Indian Ocean maritime trade networks dating back to antiquity. Similarly, grossular sourced from Indian and deposits featured in Hellenistic-Roman jewelry and carvings, highlighting its early cultural value in decorative and trade contexts. During the , hessonite grossular appeared in European jewelry, often set in gold rings, while the yellow variety was known as "hyacinth" or "cinnamon stone" for its warm hues reminiscent of spices from its origins. In modern times, grossular holds symbolic status as the state gem of , , designated in 1991 to honor local green varieties from deposits near Eden Mills, symbolizing the region's geological heritage. In crystal healing practices, grossular is associated with abundance, manifestation, and emotional balance, particularly through its connection to the ; green forms like are linked to prosperity and renewal. , the vivid green grossular from , evokes national pride in and as a rare local treasure discovered in the , often incorporated into contemporary jewelry reflecting regional identity. Grossular's collectibility extends to museums worldwide, where specimens showcase its color diversity, from the transparent crystals at the Smithsonian to those highlighting Vermont's rodingite-hosted varieties. Unlike or other red garnets with deep mythological associations in ancient lore, grossular lacks prominent ties to legends, emphasizing instead its role in practical and symbolic human endeavors. In 2025 bridal trends, garnets appear in sustainable, colored-stone designs, blending tradition with modern elegance for engagements and weddings.

References

  1. [1]
    [PDF] Grossular Ca3Al2(SiO4)3 - Handbook of Mineralogy
    Optical Properties: Transparent to opaque. Color: Yellow-green, pale to dark green; golden yellow, pink, red, orange, brownish red, yellowish brown; ...
  2. [2]
    Grossular Garnet - Smithsonian National Museum of Natural History
    Grossular is the garnet mineral that shows the widest range of colors. As pure calcium aluminum silicate it is colorless, but impurities can tint it shades.
  3. [3]
    [PDF] Gem-Quality Grossular Garnets - GIA
    Hessonite is the name traditionally applied to the yel- low, orange, or brown transparent variety of grossular. However, color descriptions of hessonite are ...
  4. [4]
    Grossular - WGNHS
    Grossular is a member of the garnet family found as pale white, green or tan crystals, most often in marbles, calc-silicate and other metamorphic rocks.
  5. [5]
    Grossular: Mineral information, data and localities.
    Originally named "cinnamon stone" ("Kanelstein" in German) in 1803 by Abraham Gottlob Werner and renamed grossularite by Werner in 1808.Missing: discovery | Show results with:discovery
  6. [6]
    Garnet Group: Mineral information, data and localities.
    [Grossular] Dave Bodnar collection. +1 other reference · i Old Mine Plaza construction site. [Grossular] Cristofono (n.d.) +1 other reference. Weston. i Garnet ...Grossular · Almandine · Spessartine · Pyrope
  7. [7]
    Grossular (var. tsavorite) | Smithsonian National Museum of Natural ...
    Tsavorite was first discovered in 1967 in northern Tanzania and again in 1970 in Kenya's Tsavo National Park by world renowned geologist, Campbell Bridges. In ...
  8. [8]
    Celebrating 50 Years of Tsavorite | Gems & Gemology - GIA
    ... discovered, near Komolo, Tanzania, in 1967. These are among the first samples that were analyzed to identify this new gemstone. Next, the tsavorite in ...
  9. [9]
    Jewelry Television in Tucson | Gems & Gemology - GIA
    They took a small margin and sold the production quickly; 5 to 7 ct gem-quality tsavorites went for $500 per carat.
  10. [10]
    Hydrogrossular Garnet Value, Price, and Jewelry Information - IGS
    Jan 15, 2021 · Hydrogrossular differs from the other garnets in that it is never transparent. It ranges from translucent to opaque. The most common color is a blueish green.
  11. [11]
    [PDF] Grossular Ca3Al2(SiO4)3 - Handbook of Mineralogy
    Grossular. Ca3Al2(SiO4)3 c. ○2001 Mineral Data Publishing, version 1.2. Crystal Data: Cubic. Point Group: 4=m 3 2=m: Commonly in dodecahedra or trapezohedra ...
  12. [12]
    The Study of Crystal Structure on Grossular–Andradite Solid Solution
    Nov 8, 2019 · The unit-cell parameters of grossular and andradite end-member garnets were 11.848(0) and 12.054(0) Å (PXRD) and 11.842(0) and 12.053(1) Å ...
  13. [13]
    [PDF] Nomenclature of the garnet supergroup
    Abraham Gottlob Werner. Dana and Brush. (1868). Bohemian ruby pyrope. Robert Webster, Basil. William Anderson. Bayliss (2000). Böhmischer granat pyrope- ...
  14. [14]
    [PDF] The crystal structures of grossular and spessartine between 100 and ...
    The unit- cell dimension of grossular, 11.8502(4) Å, determined by powder X-ray refinement and 11.850(1) Å by single-crystal X- ray diffraction at 298K, agrees ...
  15. [15]
    Control of chemical composition of hydrogrossular prepared by ...
    The 4(OH)− may be substituted by (SiO4)4− in the structure, resulting in the formation of intermediate compositions between Ca3Al2Si3O12 and Ca3Al2(OH)12. ...
  16. [16]
    Garnet - Common Minerals
    Garnets are usually easy to identify by their hardness, crystal habit and occurrence in metamorphic rock.
  17. [17]
    Grossular Garnet Value, Price, and Jewelry Information - Gem Society
    Jan 18, 2022 · Another popular gem grossular, this gem gets its name from its source, Merelani, Tanzania and, of course, its light minty green color. Leuco ...
  18. [18]
    Garnet - Smith College
    Grossular: Ca3Al2(SiO4)3. Andradite: Ca3Fe2(SiO4)3. Uvarovite: Ca3Cr2(SiO4)3. Compositions can be expressed by the general formula A3B2(SiO4). A may be (Mg, Mn ...
  19. [19]
    The solubility of natural grossular-rich garnet in pure water at high ...
    Mar 2, 2017 · Above 0.38 GPa, grossular melts incongruently to liquid + wollastonite + anorthite at temperatures of 1000–1020 °C.Missing: refractories | Show results with:refractories
  20. [20]
    Grossular : Properties, Formation, Locations - Geology Science
    Feb 4, 2024 · Refractories: Grossular, along with other garnet minerals, is sometimes used in the manufacturing of refractory materials for high-temperature ...
  21. [21]
    Minerals insoluble in Hydrochloric acid, HCl - TrekGEO
    Grossular · Halite; Hambergite; Hedenbergite · Hercynite · Hinsdalite · Hyalophane · Hydroxycalciopyrochlore · Jadeite. Kainite; Kamiokite · Kyanite. Latrappite ...
  22. [22]
    [PDF] The hydrous components in garnets: Grossular-hydrogrossular
    The OH content of grossular garnets can be obtained from infrared spectra using the equation HrO wto/o : 0.0000786 x integrated absorbance per cm in the OH ...Missing: solubility acids
  23. [23]
    Tsavorite (Garnet) - National Gem Lab
    Luster: Vitreous to Resinous ; Refractive Index: 1.743 Isotropic ; Birefringence: 0.00 Isotropic; weak strain birefringence ; Dispersion: Moderate; 0.027.
  24. [24]
  25. [25]
    [PDF] garnet-grossular-tsavorite-34358.pdf - GIA
    Refractive Index: Birefringence: None. LWUV: SWUV: None. Not applicable ... Absorption Spectrum: Broad absorption below 490 nm. Luster: Vitreous. 1.741.
  26. [26]
    Luminescence Characteristics of Green Grossular Garnets - MDPI
    The emission spectra of the grossular in this work have a weak band at near 600 nm and a series of peaks at around 700 nm, which imply manganese-, chromium- and ...
  27. [27]
    The Garnet specs - Pierres de charme
    Demantoid garnet shows a very high dispersion (fire) of 0.057, which is higher than that of diamond 0.044. Gre-2. In Cours de base en gemmologie Gem-A. London, ...<|separator|>
  28. [28]
    15 Metamorphism of Calcareous Rocks – Open Petrology
    Tremolite, diopside, enstatite, and dolomite coexist between 660 and 725 oC as Reaction 7 occurs, and fluid composition follows the reaction curve to higher ...
  29. [29]
    Vesuvianite-wollastonite-grossular-bearing calc-silicate rock near ...
    Jun 3, 2007 · This paper reports the occurrence of vesvianite + wollastonite + grossular + diopside + microcline + quartz assemblage in an enclave of ...
  30. [30]
    [PDF] Garnet-forming reactions in calc-silicate rocks from the Polička Unit ...
    Sep 25, 2009 · Metamorphic P–T conditions of 640–680 °C and 6–7 kbar obtained for the calc-silicate rocks from the MZ and SU correspond to data from adjacent ...
  31. [31]
    Formation of Micro-Rodingites from IODP Hole U1309D
    Aug 2, 2008 · In this paper we describe prehnite–grossular assemblages after plagioclase that formed during serpentinization of olivine-rich troctolite in Integrated Ocean ...Mineral Compositions · Grossular/hydrogrossular · Chlorite And Serpentine<|control11|><|separator|>
  32. [32]
  33. [33]
    Discovery of Color-Change Chrome Grossular Garnets from Ethiopia
    The first known group of color-change gem-quality chrome grossular garnet, reportedly from Ethiopia, is examined in GIA's Carlsbad lab ... pleochroism ...
  34. [34]
    Vibrant Green Grossular Garnet “Transvaal Jade” - GIA
    Specimens of this material are typically more translucent and lighter in color (J. Frankel, “Uvarovite garnet and South African jade (hydrogrossular) from the ...
  35. [35]
    Lithostratigraphic and structural controls of 'tsavorite' deposits at ...
    The 'tsavorite' and 'tanzanite' mineralizations in the Merelani, Lemshuku and Namalulu mining districts all occur in the Lelatema Fold Belt of the Eastern ...<|separator|>
  36. [36]
    Grossular Garnet: Value, Properties & Gemstone Trends 2025
    Grossular Varieties: Hessonite, Tsavorite & Hydrogrossular ; 1. Grossular Tsavorite · Intense green, ranging from grassy to bluish-green shades. · Transparent ...Grossular Garnet: Value... · Grossular Meaning And... · Grossular Varieties...
  37. [37]
    Grossular from Jeffrey Mine, Val-des-Sources, Les Sources RCM ...
    Grossular from Jeffrey Mine is a chrome-bearing mineral with formula Ca3Al2(SiO4)3, found in an open-cast mine, with colors including colorless, white, orange, ...
  38. [38]
    Garnet v. Grossular - Collector's Edge Minerals
    In stock 14-day returnsMar 25, 2024 · The Jeffrey Mine was an open-pit chrysotile asbestos mine that operated from 1879 to 2001. It has produced, arguably, the world's finest ...
  39. [39]
    Uvarovite garnet and South African jade (hydrogrossular) from the ...
    The pale green, fine-grained, ornamental rock known as South African Jade is found to be hydrogrossular that varies in composition over a restricted range near ...
  40. [40]
    Hessonite Garnet Value, Price, and Jewelry Information - IGS
    Dec 27, 2022 · Also known as the “cinnamon stone,” hessonite is the yellow-orange to reddish orange variety of grossular garnet. Hessonites can make ...Does Hessonite Make A Good... · Identifying Characteristics · How To Care For Hessonites
  41. [41]
    Viluite: Mineral information, data and localities.
    Oct 10, 2025 · Named for the Vilui River region, Saha Republic (Yakutia), Russia. This name has been frequently used since the 19th century for two different minerals.
  42. [42]
    [PDF] East African Journal of Environment and Natural Resources
    Nov 13, 2024 · This study investigated major occupational health and safety issues associated with artisanal gemstone mining using a variety of methods ...
  43. [43]
    Garnet Quality Factors - GIA
    68.82 Carat Tsavorite Garnet. This tsavorite garnet has an appealing green color and is a 68.82-carat gem. - Courtesy New Era Gems. 3.20 Carat Demantoid Garnet.Missing: per | Show results with:per
  44. [44]
    Tsavorite Garnet Value, Price, and Jewelry Information - IGS
    Jan 10, 2023 · $$$per carat. 1-1.99 Carat. avg. $$$per carat. 2-4.99 Carat. avg. $$$per carat. 5-7.99 Carat. avg. $$$per carat. See Gem Price Guide for more ...
  45. [45]
  46. [46]
    [PDF] Mineral of the Month Club October 2017
    Page3. HISTORY, USES & LORE: In 1803, German geologist and mineralogist Abraham Gottlob. Werner (1749-1817) studied specimens of a previously unknown type of ...
  47. [47]
    Garnet: The Versatile Industrial Mineral for Abrasive and Waterjet ...
    Aug 8, 2025 · Garnet is the preferred abrasive in waterjet cutting applications. Mixed with high-pressure water, garnet efficiently cuts through metals, ...Missing: grossular refractories
  48. [48]
  49. [49]
    Hydrogrossular Garnet Gem: Traits, Meaning, Prices & More
    ### Summary of Hydrogrossular Garnet Ornamental Uses, Carvings, Beads, and Historical Intaglios
  50. [50]
    Garnet Market Size, Share, Growth, Trends & Forecast by 2033
    The global garnet market size was USD 704.18 million in 2024 & is projected to grow from USD 737.49 million in 2025 to USD 1067.39 million by 2033.Missing: ethical blockchain
  51. [51]
    Constraints from In Situ U-Pb LA-ICP-MS Dating - MDPI
    Gem-quality green vanadium grossular (var. tsavorite) is exclusively hosted in the Neoproterozoic Metamorphic Mozambique Belt (NMMB).3. Materials And Methods · 4. Results · 4.1. Gemological Properties
  52. [52]
  53. [53]
    Sri Lankan Garnet and Garnet Beads in the Indian Ocean Maritime ...
    Sep 20, 2022 · In this paper, based on our analysis of worked and raw garnets from archaeological contexts, both within and outside Sri Lanka, and historical records,
  54. [54]
    Study of Garnets in Hellenistic–Roman Jewellery From the ...
    Aug 1, 2025 · The use of garnets predates the Hellenistic–Roman Eras. They were sporadically used as beads and seals in Predynastic Egypt (5500–3100 BCE), the ...
  55. [55]
    Renaissance gold ring with a hessonite garnet. - Ref.110387
    A Renaissance gold ring set with a table cut hessonite garnet. Western Europe, second half of the 16th century. Ring Size U UK / 10 US.<|control11|><|separator|>
  56. [56]
    All About Jewels Glossary: G - Enchanted Learning
    The yellow variety is called cinnamon stone, hyacinth or jacinth. Transvaal "jade" is a type of green to gray grossular garnet from South Africa. Pink grossular ...
  57. [57]
    Grossular Garnet - Vermont State Gem
    Official State Gem of Vermont. Vermont designated the grossular garnet as official state gem in 1991.Missing: deposits | Show results with:deposits<|separator|>
  58. [58]
  59. [59]