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AL ORDWAY COLLECTION
ex. Al Ordway
This is a rare potassium, sodium sulfate which is almost never found in euhedral, barrel shaped crystals of this size, up to 8 mm in length. The crystals are lustrous and translucent and exhibit a light gray. This is from an early expedition to the salt domes of Iran. This piece, with numerous crystals to about 1 cm, is (i am told) of a superior quality. I have seen only one other of any quality, for sale, from the Zinn collection rarities suite back in 2003. In fact, that piece is still, 8 years later, one of only a very few Iranian examples illustrated on MINDAT: http://www.mindat.org/loc-190502.html
ex. Robert Fender
Equant crystals of lustrous and translucent, apple-green apophyllite, to 6 mm across, are stacked on lustrous and translucent, tan crystals of stilbite on this rare locality combination specimen. Self-collected by Robert Fender many years ago (probably circa 1960s-1970s)
ex. Al Ordway
A lustrous and translucent, dark gray-green boracite crystal, measuring 1.2 cm in length, is perched aesthetically on top of a color contrasting light gray matrix. What makes this additionally special is the presence of penetration twin boracite crystal on the very top termination of the underlying crystal. This is a classic, textbook example of this rare species from its ancient type locality, and seldom seen in such an aesthetic piece today. Also, teh crystal size and quality is relatively large, and very choice for this material.
ex. Al Ordway
A remarkable, rare piece with stark aesthetics in the simplicity of its crystal habit and snowy white color. This is a fine example of well formed crystals of hanksite being pseudomorphed to borax. It is the only good example of this, that I have seen; and the only one in this collection (Al being one of the well known borate collectors, too). The largest crystal is doubly-terminated and measures 6 cm in length. The crystals have some moderate luster and are offwhite or ivory-colored.
ex. Al Ordway
Perched beautifully on top a gray matrix of crude borax, is a well formed octahedron of lustrous and translucent, yellow Sulphohalite, measuring 2.4 cm in length. This is a superb, sharp, and colorful example of this very rare species from its type locality. It also happens to be an aesthetic specimen on its own merits. We have not seen such a nice example of this species in the overall quality level, before.
Emplaced on a vein of foliated, purple actinolite are sharp crystals of lustrous, deep green, chromium rich, lawsonite, an uncommon silicate. The crystals reach 1 cm across and some appear to be doubly terminated. A remarkable new find from the Tucson 2012 show, of green lawsonite crystals (the color induced by chromium), in contrasting matrix with thin veins of purple actinolite and white muscovite. This uncommon silicate is found in good crystals at only a few locales wordlwide. And, never have we seen them with such color! This is from a small find, but it is unclear exactly when it was found and leaked out to the market. CORRECTION NOTED WITH THANKS TO DR. Maarten Broekmans: The “purple actinolite” you mention in the descriptions, however, is glaukofane or crossite, a sodic amphibole characteristic of high-pressure terranes. This complies with lawsonite being a sodic HP mineral itself, far better than an actinolite would, a calcic (Fe,Mg) amphibole. the silvery white mica is rather paragonite, the Na equivalent of K-muscovite. Also typical for HP settings. Besides that, Cr would color an actinolite stark green too, not purple. In fact, whole (scarcely vegetated) valleys on the island have this bluish-purplish tone over them, an amazing view
Crystals of lustrous, dark green chromium rich lawsonite, to 1.7 cm across, are festooned on both sides of the host matrix. Several crystals appear to be doubly terminated. A remarkable new find from the Tucson 2012 show, of green lawsonite crystals (the color induced by chromium), in contrasting matrix with thin veins of purple actinolite and white muscovite.These are lustrous, deep green crystals of chromium-rich lawsonite, which is a very uncommon silicate found in good crystals at only a few locales wordlwide. And, never have we seen them with such color! This is from a small find, but it is unclear exactly when it was found and leaked out to the market. CORRECTION NOTED WITH THANKS TO DR. Maarten Broekmans: The “purple actinolite” you mention in the descriptions, however, is glaukofane or crossite, a sodic amphibole characteristic of high-pressure terranes. This complies with lawsonite being a sodic HP mineral itself, far better than an actinolite would, a calcic (Fe,Mg) amphibole. the silvery white mica is rather paragonite, the Na equivalent of K-muscovite. Also typical for HP settings. Besides that, Cr would color an actinolite stark green too, not purple. In fact, whole (scarcely vegetated) valleys on the island have this bluish-purplish tone over them, an amazing view
A remarkable new find from the Tucson 2012 show, of green lawsonite crystals (the color induced by chromium), in contrasting matrix with thin veins of purple actinolite and white muscovite.These are lustrous, deep green crystals to 1.5 cm, of chromium-rich lawsonite, which is a very uncommon silicate found in good crystals at only a few locales wordlwide. And, never have we seen them with such color! This is from a small find, but it is unclear exactly when it was found and leaked out to the market.Several crystals appear to be doubly terminated. This particular specimen is the largest good example I saw, and also has a very rich association with the purple actinolite matrix for contrast. CORRECTION NOTED WITH THANKS TO DR. Maarten Broekmans: The “purple actinolite” you mention in the descriptions, however, is glaukofane or crossite, a sodic amphibole characteristic of high-pressure terranes. This complies with lawsonite being a sodic HP mineral itself, far better than an actinolite would, a calcic (Fe,Mg) amphibole. the silvery white mica is rather paragonite, the Na equivalent of K-muscovite. Also typical for HP settings. Besides that, Cr would color an actinolite stark green too, not purple. In fact, whole (scarcely vegetated) valleys on the island have this bluish-purplish tone over them, an amazing view
Perched high on a ridge of matrix are several , lustrous, dark green crystals of chromium rich lawsonite, an uncommon silicate mineral. The crystals reach 1.2 cm across and a few appear to be doubly terminated. A remarkable new find from the Tucson 2012 show, of green lawsonite crystals (the color induced by chromium), in contrasting matrix with thin veins of purple actinolite and white muscovite.These are lustrous, deep green crystals to 1.2 cm across, of chromium-rich lawsonite, which is a very uncommon silicate found in good crystals at only a few locales wordlwide. And, never have we seen them with such color! This is from a small find, but it is unclear exactly when it was found and leaked out to the market. CORRECTION NOTED WITH THANKS TO DR. Maarten Broekmans: The “purple actinolite” you mention in the descriptions, however, is glaukofane or crossite, a sodic amphibole characteristic of high-pressure terranes. This complies with lawsonite being a sodic HP mineral itself, far better than an actinolite would, a calcic (Fe,Mg) amphibole. the silvery white mica is rather paragonite, the Na equivalent of K-muscovite. Also typical for HP settings. Besides that, Cr would color an actinolite stark green too, not purple. In fact, whole (scarcely vegetated) valleys on the island have this bluish-purplish tone over them, an amazing view
A remarkable new find from the Tucson show, of green lawsonite crystals (the color induced by chromium), in contrasting matrix with thin veins of purple actinolite and white muscovite.These are lustrous, deep green crystals to 1 cm, of chromium-rich lawsonite, which is a very uncommon silicate found in good crystals at only a few locales wordlwide. And, never have we seen them with such color! This is from a small find, but it is unclear exactly when it was found and leaked out to the market.Several crystals appear to be doubly terminated. This specimen has perhaps the sharpest crystals here, with higher luster and sharper edges than most other examples. CORRECTION NOTED WITH THANKS TO DR. Maarten Broekmans: The “purple actinolite” you mention in the descriptions, however, is glaukofane or crossite, a sodic amphibole characteristic of high-pressure terranes. This complies with lawsonite being a sodic HP mineral itself, far better than an actinolite would, a calcic (Fe,Mg) amphibole. the silvery white mica is rather paragonite, the Na equivalent of K-muscovite. Also typical for HP settings. Besides that, Cr would color an actinolite stark green too, not purple. In fact, whole (scarcely vegetated) valleys on the island have this bluish-purplish tone over them, an amazing view
A remarkable new find from the Tucson 2012 show, of green lawsonite crystals (the color induced by chromium), in contrasting matrix with thin veins of purple actinolite and white muscovite.These are lustrous, deep green crystals to 2 cm across, of chromium-rich lawsonite, which is a very uncommon silicate found in good crystals at only a few locales wordlwide. And, never have we seen them with such color! This is from a small find, but it is unclear exactly when it was found and leaked out to the market. Although slightly corroded , several crystals appear to be doubly terminated. CORRECTION NOTED WITH THANKS TO DR. Maarten Broekmans: The “purple actinolite” you mention in the descriptions, however, is glaukofane or crossite, a sodic amphibole characteristic of high-pressure terranes. This complies with lawsonite being a sodic HP mineral itself, far better than an actinolite would, a calcic (Fe,Mg) amphibole. the silvery white mica is rather paragonite, the Na equivalent of K-muscovite. Also typical for HP settings. Besides that, Cr would color an actinolite stark green too, not purple. In fact, whole (scarcely vegetated) valleys on the island have this bluish-purplish tone over them, an amazing view
ex. Al Ordway
A very aesthetic, sharp cluster of bipyramidal crystals of thenardite, a rare sodium sulfate, to 4 cm on a side. The display view clearly highlights the main crystal which resembles a spearpoint. These are generally considered best of species material, and really good ones are seldom seen on the market today.
ex. Al Ordway
A cluster of sparkling and translucent, pinkish brown crystals, to 7 mm in length, of poldervaartite, a calcium and manganese rich silicate from the Wessels mine in South Africa. Notably, this is from the type locality and probably from the type pocket material. This mineral was discovered in the early 1980s but only recognized and named by 1993. Specimens were always extremely rare and hard to obtain: Literally, these were like gold to the collectors of Kalahari rarities suites. Almost impossible to obtain. Von Bezing, Key, a few people had them. Later, similar-looking material was found in N'Chwaning and it turned out to be the new , related species Olmiite. This remains, thus, a rare species that few can own (despite all the hundreds of mislabelled olmiite on the market now, out there!). Probably (according to Charlie Key) any piece from this pocket can be considered a co-type with the material used to describe the species. Aesthetic, significant, and an important rarity.
ex. Al Ordway
Emplaced on a gray matrix are crystals of pseudocubic, lustrous and translucent, light orangy-yellow colored chabazite, an uncommon member of the zeolite family. The largest crystals reach 1.8 cm in length. A superb and pretty example from this classic locality, examples of which we seldom see on the market today.
ex. Al Ordway
From the ancient type locality for analcime in the Mount Etna volcano complex of Sicily, here we have a cluster of superbly-terminated, limpid, glassy and gemmy crystals. They are sharp and perhaps the most gemmy analcime I have seen from any lcoale, and reach to 1.5 cm across. These are TEXTBOOK and important, for the type locality of this species. As well, it is a nice display specimen, too.
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