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A really interesting good size and gemmy fluorapatite crystal. We can observe perfectly the combination of the first and second order prisms; very sharp terminal faces, with first order hexagonal dipyramid, truncated by the pinacoid. A specimen to enjoy crystallography and aesthetics.
Crystal shows excellent brilliance, transparence and a vivid yellow color with green tones. These specimens with this quality and size are not common on the market, the small ones are used for gem cutting. The specimen is from a Moroccan classic mine located in the Imilchil mountains area. A chance to get a good representative for the species and locality.
In this specimen we can enjoy some groups of rhombohedral cobaltoan calcite. With good pink to purple color, translucent and which are disposed randomly on the matrix. The color is excellent.
These globular vanadinite aggregates, formed by hexagonal crystals, were collected Taouz mine few days before our visit. These groups, which are sometimes partially covered by calcite, are very brilliant, translucent and they are disposed on the matrix covered by lenticular goethite. A new Taouz curiosity.
Druse of divergent prismatic cobaltoan calcite crystals showing flattened rhombohedral terminal faces, with marked geometric pink color zoning. Translucent and very showy. We can observe original calcite as brown transparent crystals, with a thick layer of intense pink color. Very interesting and different.
In this huge size specimen we observe groups of tabular lenticular aggregates of barite with a delicate reddish tones, along with gray galena that has been almost completely substituted and covered by nice cerussite crystals. Taking a look under the microscope, cerussite shows long striated prisms terminated by pyramidal faces. Also note several cyclic star twins, well defined and spectacular. See the huge size twinned crystals of cerussite, close to the mineralized areas. Different specimens from Mibladen.
The large mine of Les O is mined under the town of Mibladen. It has been worked during generations of miners in search of specimens, usually galena cerussite, barite and some wulfenite. Few weeks before my visit in February 2013 were found some mineralized veins and vugs with the specimens we offer. When those cavities were formed they had been filled by cube octahedral crystals of galena and barite. Due to the hydrothermal fluids galena was partially or totally corroded to favor the formation of cerussite.
Druse of cobaltoan calcite crystals, with an excellent brilliance, transparence and showing very sharp terminal rhombohedral faces ad edges. Color is really good, a gemmy specimen.
In this huge size specimen we observe groups of tabular lenticular aggregates of barite with a delicate reddish tones, along with gray galena that has been almost completely substituted and covered by nice cerussite crystals. Taking a look under the microscope, cerussite shows long striated prisms terminated by pyramidal faces. Also note several cyclic star twins, well defined and spectacular. See the huge size twinned crystals of cerussite, close to the mineralized areas. Different specimens from Mibladen.
The large mine of Les O is mined under the town of Mibladen. It has been worked during generations of miners in search of specimens, usually galena cerussite, barite and some wulfenite. Few weeks before my visit in February 2013 were found some mineralized veins and vugs with the specimens we offer. When those cavities were formed they had been filled by cube octahedral crystals of galena and barite. Due to the hydrothermal fluids galena was partially or totally corroded to favor the formation of cerussite.
A very nice huge size goethite specimen showing stalactitic-habit, well developed, with aesthetic botryoidal forms. Exterior color is olive green, with very curious terminations, very thin. We can observe that these growths are formed by several goethite crystals in radial disposition. A high quality specimen for this Moroccan mine.
A very nice specimen of goethite showing stalactitic-habit with botryoidal forms. Exterior color is olive green, with very curious terminations. In the base we can observe that these growths are formed by several goethite crystals in radial disposition. A quality specimen for this Moroccan mine.
This is one of the gemmy axinite-(Fe), that came out in the late 1980s from this remote mining region, in the North Urals.Brilliance and transparence is excellent, with internal reflections and lights. Perfectly defined triclinic faces and marked edges. Good size and quality.
Elegant crystal of amazonite, a variety of microcline, good size, from a classic American locality. This crystal shows many faces delimited by triclinic pinacoids, along with growth in the upper faces. Good color and transparency when the light hits on the edges.
A very rich botryoidal growths of mottramite, with an excellent dark green color and velvety. These mottramite specimens were recently found in the mina Ojuela and for their quality could be considered a good representative for the species and, of course, the best specimens from this mine. A huge size specimen for the more selected display.
A very rich specimen of cuprian adamite, formed by several very sharp pseudooctaedral crystals, with an excellent brilliance and transparence. Color is different than usual for the species and mine, with a green to bluish tones. Adamite crystals are partially covering a vug in the goethite matrix. A display huge size specimen and a very good aesthetics. From this classic classic Mexican mine.
Groups of tabular wulfenite crystals of intense orange color, showing parallel growth. If anything distinguishes these wulfenite crystals is its vivid color. The brilliance is excellent and in thin areas show transparence. Disposed very aerial and accompanied by fan-shaped barite crystals.
This specimen was collected a few days before our visit to the mine. A group of vanadinite crystals with a hexagonal shape and forming nice globular aggregates. The color is orange to reddish, with good transparency and disposed on vugs in the compact limonite matrix, covered by small goethite lenticular crystals. A not very common specimen from this classic mine.
One of the specimens with a exceptional color, excellent brilliance, a real gem. Very rich group of vanadinite crystals showing a defined hexagonal shape, with very well defined faces and edges, intense red color. Good brilliance and some transparence, with internal reflections between red and orange. Main crystals size are remarkable. Covering the barite matrix. The presence of this barite matrix is highly appreciated by collectors.
This sample was collected from one of these shafts where berber (amazigh) miners are working hard during months till they found a vug. This extended area, called Coud'a (Coudia), is located about half mile from well known ACF mine, but it is not the same mine. The vanadinite veins mined in Coud'a, which are approximately 30 to 50 feet deep, are not the same than ACF mine and their particular mineralogy.
Excelent group of vanadinite crystals showing a defined hexagonal shape, with very well defined faces and edges, intense red color. Good brilliance and some transparence, with internal reflections between red and orange. Main crystal size and thickness are remarkable. They are disposed very aerial and isolated on a lenticular barite crystal matrix. The presence of this barite matrix is highly appreciated by collectors and gives to the specimen a special aesthetics.
This sample was collected from one of these shafts where berber (amazigh) miners are working hard during months till they found a vug. This extended area, called Coud'a (Coudia), is located about half mile from well known ACF mine, but it is not the same mine. The vanadinite veins mined in Coud'a, which are approximately 30 to 50 feet deep, are not the same than ACF mine and their particular mineralogy.
The large mine of Les O is mined under the town of Mibladen. It has been worked during generations of miners in search of specimens, usually galena cerussite, barite and some wulfenite. Few weeks before my visit in February 2013 were found some mineralized veins and vugs with the specimens we offer. When those cavities were formed they had been filled by cube octahedral crystals of galena and barite. Due to the hydrothermal fluids galena was partially or totally corroded to favor the formation of cerussite.
In this specimen we observe groups of tabular lenticular aggregates of barite with a delicate reddish tones, along with gray galena that has been almost completely substituted and covered by nice cerussite crystals. Taking a look under the microscope, cerussite shows long striated prisms terminated by pyramidal faces. Also note several cyclic twins, well defined and spectacular. Different specimens from Mibladen.
In this specimen we can observe some groups of tabular wulfenite crystals of intense, very intense orange color, showing defined faces and parallel growth. If anything distinguishes these wulfenite crystals is its vivid color. The brilliance is excellent and in thin areas show transparence. Some of the dominant crystals are disposed very aerial and accompanied by groups of barite crystals. If you observe closely the specimen under the microscope you will see numerous perfect tabular crystals of wulfenite. Very aesthetic specimen.
In this specimen we can observe some groups of native copper crystals, with defined faces and edges, good luster and color. They are disposed on a black layer of pyrolusite and accompanied by some white to translucent calcite flattened rhombohedral crystals. These specimens were collected in a concrete areas of this mine.
Excelent group of vanadinite crystals showing a defined hexagonal shape, with very well defined faces and edges, intense red color. Good brilliance and some transparence, with internal reflections between red and orange. Main crystals size are remarkable. They are disposed very aerial on a lenticular barite crystal matrix. The presence of this barite matrix is highly appreciated by collectors and gives to the specimen a special aesthetics.
This sample was collected from one of these shafts where berber (amazigh) miners are working hard during months till they found a vug. This extended area, called Coud'a (Coudia), is located about half mile from well known ACF mine, but it is not the same mine. The vanadinite veins mined in Coud'a, which are approximately 30 to 50 feet deep, are not the same than ACF mine and their particular mineralogy.
Group of vanadinite crystals showing a defined hexagonal shape, with very well defined faces and edges, intense red color. Good brilliance and some transparence, with internal reflections between red and orange. Main crystals size are remarkable. They are disposed very aerial on a lenticular barite crystal matrix. The presence of this barite matrix is highly appreciated by collectors and gives to the specimen a special aesthetics.
This sample was collected from one of these shafts where berber (amazigh) miners are working hard during months till they found a vug. This extended area, called Coud'a (Coudia), is located about half mile from well known ACF mine, but it is not the same mine. The vanadinite veins mined in Coud'a, which are approximately 30 to 50 feet deep, are not the same than ACF mine and their particular mineralogy.
Druse of divergent prismatic cobaltoan calcite crystals showing rhombohedral terminal faces, which is not usual, perfectly defined and with good brilliance and translucent. The color varies between pink and tile red . Some of these crystals are partially covered on prism by small and brilliant minute calcite. This color zoning can be seen in the fractured area of the sample. From a Moroccan classic locality.
Although our country is rich in different forms of calcite, we want to emphasize on this specimen that shows two generations of crystal growth. The first generation calcite clusters have a good size and orange to yellowish pastel tones. With an elongated striated prism and rhombohedral terminal top forms. They are translucent and brilliant, with echeloned growths on faces.
A second generation of small, but transparent and brilliant calcite crystals, is disposed near to perpendicular on the prism of the first generation. A colored and strongly fluorescent calcite from la Cala.