Very aesthetic group of deep green epidote fan-shaped aggregates on matrix. Epidotes have a good luster and intense green colour. There are some gemmy quartz crystals emerging from the epidote. The original label we will send to the buyer indicates that those crystals are clinozoisite, but recent studies show that all the analyzed specimens are epidote (Calvo, M., Subías, I. (2017): Epidote (not clinozoisite) and andradite garnet from Los Serranos quarry, Cabezo Negro, Albatera, Alicante. Mineral Up, 4:44-47).

An unusual specimen of aragonite "flos ferri", found in 1996 at the Gloria mines, in Córdoba. Stalactitic recurved forms, brilliant and with a snowy white color to slightly green-bluish in the internal parts of the specimen. They are disposed on a matrix with colourless fluorite and traces of malachite. Not easy to see samples like this from this mine.

A classic old-time pyromorphite specimen, showing acute hexagonal prisms of beige colour to colorless, brilliant and satin-wet look, forming aesthetic rosettes on the quartz matrix. This specimen is from the famous Rosenberg mine, in Bad Ems, Germany, closed since 1963. It is accompanied by a typed label by Juan Montal, a well-known Catalan mineral dealer from Vilafranca del Penedés (Barcelona), who was active in the middle of the s. XX until the 1980s. The piece is very good for the locality and the label full of history. An European classic.

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Colorful specimen of arsenatian vanadinite crystals, in aggregates of hexagonal prismatic crystals, with hopper cavities on the pinacoidal faces. Intense shine, orange to brown, with zoning, transparent to translucent crystals. They stand out on a white matrix of calcite. An excellent specimen of this Mexican mine.

Many specimens of aragonite are seen, as "pinecone" shape, also isolated, but this specimen has an "I don't know what" that makes it different for me. An elliptical "pinecone" of prismatic, divergent aragonite crystals, which are grouped around a central axis, with more developed crystals. Different and very aesthetic. A classic from Spanish mineralogy.

Excellent, sculptural, two-sided baryte "rose" from Oklahoma. Oxidized sand grains are included in the baryte crystal structure with colorful effect. Essentially a floater. The hole adds much aesthetics. Baryte was precipitated in interconnected voids in the rock, probably from barium-rich marine waters that covered the Permian Garber Sandstone during or shortly after its deposition about 250 million years ago. The rose-like concretions incorporated the iron-stained quartz sand grains and thus acquired the red color of the host Garber Sandstone (online). These are the official Oklahoma State Rock.
Very interesting article in Mineralogical Record July-August 2008.

Excellent, sculptural, two-sided baryte "rose" from Oklahoma. Oxidized sand grains are included in the baryte crystal structure with colorful effect. Essentially a floater. The hole adds much aesthetics. Baryte was precipitated in interconnected voids in the rock, probably from barium-rich marine waters that covered the Permian Garber Sandstone during or shortly after its deposition about 250 million years ago. The rose-like concretions incorporated the iron-stained quartz sand grains and thus acquired the red color of the host Garber Sandstone (online). These are the official Oklahoma State Rock.
Very interesting article in Mineralogical Record July-August 2008.

Hydromagnesite specimens from "Pedreres de l'Àngel" (Angel quarries), in Gualba (Barcelona), are a classic for the Catalan mineralogy. In this specimen we can observe some aggregates formed by radiated crystals, some of them of good size (more than 2 cm.), others smaller (up to 8 mm), very brilliant. Nowadays impossible to be found... This mines are a skarn due to contact metamorphism of Hercynian granodiorite and biotite granite into Cambrian marbles.

This good sized specimen from the late 80s belongs from the Arguijo collection, and it was mined in this famous "onubense" mine. It is a sulphide matrix partially covered by brilliant covellite microcrystals, very defined and visible. It has an intense metallic blue iridescence and this very characteristic color. It is accompanied by numerous crystals of native sulphur with curved faces, brilliance, translucent and showing a delicate yellow tone. It was mined from a sporadic finding in the Corta Atalaya, Minas de Riotinto. A unique occasion to obtain one of these "old" specimens.

Very aesthetic specimen formed by several botryoidal aggregates of chrysocolla, with bluish green tones and very brilliant, peppered by prismatic crystals of malachite, transparent, bright and forming sheaves, which are accompanied by botroidal aggregates of intense black colour of heterogenite. A different piece of this classic mine.

Very aerial crystal of gypsum of this classic Murcian locality. It stands out for its transparency, brightness and for visible and aesthetic inclusions. The "matrix" is formed by a group of crystals of the same species. Not usual in the market.

Fine aggregates of bright and translucent gillespita, strawberry red. In a matrix of white sanbornita that contrasts with the color. Gillespita is a rare barium and iron phyllosilicate. This is a very rich, colorful and excellent piece for the species.

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A very aesthetic azurite specimen formed by several elongated prismatic crystals, forming a kind of sheaf. They are partially pseudomorphized by malachite. The blue color of the azurite is exceptional, with very good brilliance. A nice miniature from a classic Moroccan locality.

A specimen of this classic Catalan locality, with several interpenetrated cubic crystals of yellow fluorite, translucent and very defined. They are accompanied by calcite crystals and tiny chalcopyrite crystals. They are partially covered by a thin layer of illite, which we have preferred to leave to preserve the original aesthetic of the specimen. On a quartz matrix with feldspar.

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A very notable specimen for the size of the pyrolusite sharp crystals, which form brilliant aggregates. In some areas they are partially covered by small botryoidal aggregates of goethite, black and very bright. A place under the magnifying glass.

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Aggregates of prismatic crystals of meionite, with cross-linked and parallel growths. It is arranged in a matrix with octahedral magnetite crystals, green epidote and actinolite fibers. Joan Viñals indicated on the label of this specimen (we will send to the buyer) meionite, although specimens such as marialite are described in the area. The marialite-meionite series refers to the proportion of Na and Ca, both of the escapolite group. "Probably from the La Herrería mine where it usually appears in magnetite vugs as acicular and radial aggregates of tetragonal prisms, sometimes centimetric, whitish to transparent" (Mti-Blog).

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Group of octahedral fluorite crystals, of intense green color and in stepped growths. From the classic Berta Quarry, in which it is now totally forbidden to extract minerals.

Se trata de excelente cristal de cuarzo que presenta crecimientos en "ventana" (también llamados "esqueletales") muy marcados en las deformadas caras romboédricas. Prisma muy poco desarrollado. Muy buena transparencia, tono ligeramente ahumado, y un brillo más que excepcional. Se observan inclusiones de tono beige muy habituales en este tipo de crecimientos. Estos ejemplares fueron recogidos cerca del embalse de Urrúnaga, en Legutio.

Aesthetic group of tabular crystals of baryte, with a delicate bluish color, brilliant and transparent. With a good size, they stand out on a matrix of goethite. A extinc classic.

Aggregates of prehnite crystals, with stalactitic forms, translucent, brilliant and with a delicate green tone. From a classic Indian locality.

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An old specimen of this Peruvian mine that shows a large group of cubic galena crystals, interpenetrated, with its characteristic gray tone. They have stepped growths on the faces and some natural cavities, which give them a differentiated appearance.

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Group of chalcopyrite crystals, one of good size, with defined shapes arranged on quartz hyaline crystals. An aesthetic miniature.

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Group of very sharp hematite crystals, well defined edges and faces, intense metallic gray color, almost black, with aesthetic iridescent reflections. Very interesting historical piece, from the former Manchion collection.

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These specimens of banded flint were collected decades ago in the area of El Brull, in the Montseny massif, and identified as agate. They appear in nodules and veins, embedded in a siliceous limestone, presenting bands of gray tones, between light to dark gray. These kind of striped flind are well know in jewelery, and very appreciated. It is a unique curiosity of the Catalan mineralogy of many years ago.

For uranium mineral collectors, this carnotite of an intense yellow color, formed by numerous globular aggregates of crystals, covering the surface of the sandstone matrix. An American classic, labeled E. Kucera (Barcelona).

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