File:Bismuthinite (Llallagua, Bolivia) 2 (18309812433).jpg
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DescriptionBismuthinite (Llallagua, Bolivia) 2 (18309812433).jpg |
Bismuthinite from Llallagua, Bolivia. (SDSMT 3284, South Dakota School of Mines and Technology, Museum of Geology, Rapid City, South Dakota, 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. Bismuthinite is a scarce bismuth sulfide mineral (Bi2S3). It's similar to stibnite (www.flickr.com/photos/jsjgeology/sets/72157654303222578) in its physical properties, and fine-grained specimens are difficult to distinguish visually. Bismuthinite has a metallic luster, silver color, gray streak, one perfect cleavage, is fairly soft (H = 2 to 2.5), and has a high specific gravity (it's heavy for its size). Nicely crystalline specimens often display radiating masses of long, needle-shaped crystals. Finer-grained and massive bismuthinite also occur. Crystals of bismuthinite are known to be slightly flexible, and the crystal faces typically have fine striations. Bismuthinite is a key ore mineral for the element bismuth (Bi). It principally occurs in hydrothermal vein deposits, some pegmatites, and some volcanic exhalation deposits. Photo gallery of bismuthinite: www.mindat.org/gallery.php?min=686 |
Date | |
Source | Bismuthinite (Llallagua, Bolivia) 2 |
Author | James St. John |
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This image was originally posted to Flickr by jsj1771 at https://flickr.com/photos/47445767@N05/18309812433. It was reviewed on 27 July 2015 by FlickreviewR and was confirmed to be licensed under the terms of the cc-by-2.0. |
27 July 2015
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current | 18:43, 27 July 2015 | 1,654 × 1,122 (1.86 MB) | Natuur12 (talk | contribs) | Transferred from Flickr via Flickr2Commons |
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Camera manufacturer | EASTMAN KODAK COMPANY |
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F-number | f/3.2 |
ISO speed rating | 100 |
Date and time of data generation | 11:38, 19 August 2010 |
Lens focal length | 17.6 mm |
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Bits per component |
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Orientation | Normal |
Number of components | 3 |
Horizontal resolution | 480 dpi |
Vertical resolution | 480 dpi |
Software used | Adobe Photoshop Elements 13.0 (Macintosh) |
File change date and time | 14:24, 18 June 2015 |
Y and C positioning | Centered |
Exposure Program | Normal program |
Exif version | 2.21 |
Date and time of digitizing | 11:38, 19 August 2010 |
Meaning of each component |
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Sensing method | One-chip color area sensor |
File source | Digital still camera |
Scene type | A directly photographed image |
Custom image processing | Custom process |
Exposure mode | Auto exposure |
White balance | Auto white balance |
Digital zoom ratio | 0 |
Focal length in 35 mm film | 96 mm |
Scene capture type | Standard |
Scene control | Low gain up |
Contrast | Normal |
Saturation | Normal |
Sharpness | Normal |
Subject distance range | Unknown |
Date metadata was last modified | 10:24, 18 June 2015 |
Unique ID of original document | E5395270717008053450DF3420F824BF |