Ingrid Mine, a new Mozambican collector locality famed for chrysoberyl on quartz matrix; limited production, sharp yellow-green crystals, and growing rarity.
Key facts
The Ingrid Mine is a very new collector locality in western Mozambique, recorded mineralogically as a gemstone pit in Báruè District, Manica Province. For collectors its importance is unusually focused: Ingrid is, on present published and dealer-documented evidence, a chrysoberyl locality above all else. The best pieces from the 2025 production are not waterworn gem gravel but sharply crystallized, yellow-green chrysoberyl on pale quartz matrix—an uncommon presentation for a species more often encountered as loose twins, alluvial pebbles, or cuttable rough. Several documented specimens show V-twins, trilling crystals, and single prismatic crystals perched in or on quartz, with individual chrysoberyl crystals around 2–3.2 cm and matrix specimens reaching miniature to small-cabinet size.
Regional View
Country View
Geologically, the locality sits within the broader high-grade Precambrian terranes of central Mozambique, in the Báruè–Manica region where gneiss, schist, migmatite, and pegmatite-related gemstone mineralization are all part of the regional collector vocabulary. Nearby Nhampassa-area documentation describes mica schist, micaceous gneiss, quartzo-feldspathic gneiss, and pegmatite dykes, a setting fully compatible with beryllium-bearing chrysoberyl mineralization. Ingrid specimens themselves point to a quartz-rich, pegmatite-related environment: the characteristic collector pieces are yellow-green, lustrous chrysoberyl crystals on granular or fractured quartz, rather than isolated detrital stones.
Historically, Ingrid matters because it entered the specimen market abruptly as a limited modern find. Mindat records were added from Simon Harrison in 2025, and dealer listings from the same period repeatedly describe the material as a recent, limited find from a small artisanal mine. That combination—a new locality, a small production window, and matrix chrysoberyl crystals of legitimate display quality—quickly made Ingrid a name serious chrysoberyl collectors began watching.
Search for specimens: View all specimens from Ingrid mine, null
The Ingrid Mine is recorded as a pit in Báruè District, Manica Province, Mozambique, with chrysoberyl and gemstones listed for the locality. The locality is commonly marketed by dealers as “Ingrid mine, Nhampassa, Manica, Mozambique,” while Mindat places it within Báruè District. Its published mineral list is remarkably narrow: chrysoberyl is the single verified mineral species tied to the mine in the available locality records.
The deposit is best described, for collector purposes, as a pegmatite-related gemstone occurrence in quartz-rich host material. Formal geological descriptions of the Ingrid pit itself are not yet available in the public literature, but the mineralogical evidence is direct: documented specimens consist of chrysoberyl crystals on quartz matrix, including granular quartz and fractured quartz. The broader Báruè–Manica region includes high-grade metamorphic rocks of the Mozambique/Zambezi belt context, and Nhampassa-area mining documentation records mica schist, micaceous gneiss, quartzo-feldspathic gneiss, and pegmatite dykes carrying gemstone minerals such as tourmaline, rubellite, and aquamarine. Ingrid’s chrysoberyl fits that regional pattern of Be-bearing gem mineralization associated with pegmatitic fluids and aluminous wall-rock environments.
No detailed published ore-body model, production report, shaft plan, or pocket map has yet surfaced for Ingrid. The specimen evidence suggests localized extraction from quartz-rich pockets or lenses rather than large-scale industrial ore mining. Matrix pieces show chrysoberyl partly embedded in quartz, crystals standing on quartz, and in some cases multiple partial crystals intergrown into the matrix. The best collector pieces are therefore locality specimens rather than simply gem rough: they preserve the relationship between chrysoberyl and quartz and show enough crystal form to be read mineralogically.
The mining history currently visible to collectors is brief and modern. The key production appears to have been in or around 2025, when specimens were collected by a mining team and began appearing in Mindat photographs and on the international dealer market. Dealer descriptions repeatedly call the occurrence a recent limited find; one Weinrich/Minfind listing notes that the equipment at the small artisanal mine had reportedly been removed and that further production was not expected. That report should be treated as market intelligence rather than a formal mine-closure notice, but it helps explain why the better specimens were absorbed quickly by collectors.
Access today should be regarded as controlled and non-public. Ingrid is a mine locality, not a casual collecting site, and any visit would require permission from landholders and mineral-rights holders as well as current safety information. There is no reliable public collecting guide, no published access arrangement for visiting collectors, and no evidence that the site is open for fee collecting. For most collectors, the practical route to Ingrid material is through documented specimens already in the trade.
The standout finds documented so far include small-cabinet quartz matrix specimens with chrysoberyl crystals to about 3 cm, V-twinned crystals on matrix, trilling chrysoberyl crystals on quartz, and loose or matrix-supported prismatic crystals in the 1.9–4.5 cm specimen-size range. Several dealer and Mindat records emphasize yellow-green color, vitreous luster, twinning, and the presence of stabilized quartz matrix. Crystal Classics listings show that higher-end matrix examples from the find were offered in the several-thousand-dollar range, while Weinrich Minerals listings document smaller thumbnails and miniatures at lower but still strongly collector-driven prices.
Ingrid chrysoberyl is known as lustrous yellow-green crystals, most characteristically on quartz matrix, with documented habits including prismatic terminated singles, V-twins, trilling crystals, and intergrown partial crystals set into granular or fractured quartz. Published Mindat photo records include matrix specimens about 47 x 33 x 20 mm with a 22 mm twinned crystal, 60 x 55 x 45 mm with a 32 mm V-twin and multiple embedded crystals, and 80 x 57 x 40 mm with a 30 mm trilling crystal plus an untwinned crystal on the reverse; dealer records add loose or matrix specimens from thumbnail to small-cabinet size, including a 7.5 x 6.0 x 4.5 cm example in archived Weinrich listings. The better pieces from Ingrid separate themselves by sharp visible twinning, saturated yellow-green color, bright luster, intact terminations, and natural-looking placement on quartz; ordinary examples tend to be thinner, more embedded, partly broken, or dependent on stabilized matrix for display.
Other minerals from Ingrid remain poorly documented. At present, the verified locality list for the mine records chrysoberyl as the only valid mineral species, with gemstones as the commodity. No type-locality minerals, no formally described new species, and no confirmed suite of accessory minerals have been tied specifically to Ingrid in the accessible public records. Quartz is repeatedly present as matrix in specimen descriptions, but the formal mineral listing remains centered on chrysoberyl.
Ingrid chrysoberyl is a locality where documentation matters. Because the find is recent and the name is still settling into the marketplace, labels may vary between “Ingrid Mine,” “Ingrid mine, Nhampassa,” “Báruè District,” “Manica Province,” and, in at least some archived dealer listings, the erroneous or simplified “Tete, Mozambique.” Well-documented pieces should preserve the dealer label, date of acquisition, and any reference to the 2025 find, especially for larger matrix specimens.
The main condition issue is matrix stability. Multiple dealer descriptions explicitly note stabilized quartz matrix. That is not automatically a defect—fractured quartz matrix often needs consolidation to preserve an important specimen—but it should be disclosed and priced accordingly. Collectors should distinguish between stabilization of friable or fractured quartz and repair or reattachment of chrysoberyl crystals. On Ingrid pieces, inspect contact points carefully under magnification: the most desirable examples show crystals naturally seated in quartz, without glue halos, mismatched contact surfaces, or suspiciously isolated crystals planted on matrix.
No specific documented fakes or treatments unique to Ingrid have been found, but the broader risk is locality mislabelling. Yellow-green chrysoberyl from Brazil, Madagascar, Zimbabwe, Russia, and other localities can be superficially similar in loose crystals; Ingrid matrix pieces are more distinctive because of their quartz association and modern find history. Loose crystals require stronger provenance than matrix examples, especially if sold simply as “Mozambique chrysoberyl.”
Rarity is real but still market-defined. Ingrid is not an old classic locality with decades of literature behind it; it is a fresh, limited-production occurrence whose importance rests on a small number of attractive matrix chrysoberyls entering the trade in 2025–2026. Current availability has been strongest through dealers who handled the original find, with EarthWonders, Weinrich Minerals, Minfind-indexed listings, and Crystal Classics records all showing examples. The supply of good matrix pieces appears limited, and the best V-twins and trilling crystals on quartz should be treated as the locality’s premium format.
Chrysoberyl is hard—8.5 on Mohs—and generally durable, but Ingrid pieces should still be handled as matrix specimens rather than gemstones. Avoid ultrasonic cleaning, soaking, or aggressive mechanical cleaning on stabilized quartz. Store larger matrix specimens so that projecting chrysoberyl crystals do not bear weight, and keep label information with the specimen; for a new locality like this, provenance is part of the value.
