File:Sphalerite (Herja Mine, Baia Mare, Romania).jpg
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Summary
DescriptionSphalerite (Herja Mine, Baia Mare, Romania).jpg |
English: Sphalerite from Romania. (public display, Carnegie Museum of Natural History, Pittsburgh, Pennsylvania, USA)
A mineral is a naturally-occurring, solid, inorganic, crystalline substance having a fairly definite chemical composition and having fairly definite physical properties. At its simplest, a mineral is a naturally-occurring solid chemical. Currently, there are over 4900 named and described minerals - about 200 of them are common and about 20 of them are very common. Mineral classification is based on anion chemistry. Major categories of minerals are: elements, sulfides, oxides, halides, carbonates, sulfates, phosphates, and silicates. The sulfide minerals contain one or more sulfide anions (S-2). The sulfides are usually considered together with the arsenide minerals, the sulfarsenide minerals, and the telluride minerals. Many sulfides are economically significant, as they occur commonly in ores. The metals that combine with S-2 are mainly Fe, Cu, Ni, Ag, etc. Most sulfides have a metallic luster, are moderately soft, and are noticeably heavy for their size. These minerals will not form in the presence of free oxygen. Under an oxygen-rich atmosphere, sulfide minerals tend to chemically weather to various oxide and hydroxide minerals. Sphalerite is a somewhat common zinc sulfide mineral (ZnS). It has a metallic to submetallic to resinous to adamantine luster. Many metals can substitute for the zinc, such as iron, cadmium, and manganese. Sphalerite almost always has some iron in it, so a better chemical formula would be (Zn,Fe)S. Sphalerite has a wide color range, depending principally on iron content. Pure to almost pure sphalerite is whitish to greenish. With increasing iron content, sphalerite becomes yellowish to brownish to blackish. One variety of sphalerite has a strikingly intense dark red color (ruby sphalerite). It's streak color also varies with iron content from whitish to pale yellowish to brownish. Sphalerite is also distinctive in being moderately heavy for its size and having six different planes of cleavage. Sphalerite is the most important zinc ore mineral. Zinc produced from sphalerite is used for many purposes, including mixing with copper to produce brass, rust protection of iron & steel, and for making modern American pennies (although the cost of making each zinc penny is >1¢). Locality: Herja Mine, Baia Mare, Romania Photo gallery of sphalerite: www.mindat.org/gallery.php?min=3727 |
Date | |
Source | Sphalerite (Herja Mine, Baia Mare, Romania) |
Author | James St. John |
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This image was originally posted to Flickr by jsj1771 at https://www.flickr.com/photos/47445767@N05/17698181764. It was reviewed on 12 June 2015 by FlickreviewR and was confirmed to be licensed under the terms of the cc-by-2.0. |
12 June 2015
Items portrayed in this file
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some value
25 July 2010
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Date/Time | Thumbnail | Dimensions | User | Comment | |
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current | 03:42, 12 June 2015 | 2,485 × 1,766 (3 MB) | Tillman | Transferred from Flickr via Flickr2Commons |
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Date and time of data generation | 14:27, 25 July 2010 |
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Image title | |
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Horizontal resolution | 180 dpi |
Vertical resolution | 180 dpi |
Software used | Adobe Photoshop Elements 13.0 (Macintosh) |
File change date and time | 17:44, 31 May 2015 |
Y and C positioning | Co-sited |
Exif version | 2.21 |
Date and time of digitizing | 14:27, 25 July 2010 |
Meaning of each component |
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Scene capture type | Standard |
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Date metadata was last modified | 13:44, 31 May 2015 |
Unique ID of original document | 6116927D9A0F23AFC05A4DB88A813D42 |