Willemite, zincite in calcite - Sterling Hill. Ogdensburg, NJ

$35.0
Franklin Mineral Museum
Fluorescent mineral species
Country/Region of Manufacture
United States
condition
Used
Here, we have a classic "red and green" specimen from the Sterling mine. The matrix is coarse, white to off-white, opaque, semi-vitreous calcite. Embedded in several places of the calcite are dull-lustered, elongated tan willemite elongated resinous orange-red zincite plus black, metallic sections of franklinite. 

Willemite was named after King Willem of the Netherlands, after the locality at the Moresnet (Plombières-Altenberg-Moresnet) mining district in Verviers, Liège Province, Belgium. This species was previously discovered in 1825 and was identified as "siliceous oxyde of zinc" by Lardner Vanuxem and William Hypolitus Keating. At the time, "siliceous oxyde of zinc" was a synonym for electric calamine, now known as hemimorphite. A series of errors and misunderstandings eventually led to the Belgian location getting the type locality attribution rather than Franklin.
 
Under shortwave (254 nm) ultraviolet light, the willemite fluoresces a bright green and the calcite a bright red. This specimen is a representative example of the occurrence of this mineral species. It would be a nice small addition for anyone needing a classic "red and green" from the Sterling mine.

Dimensions are 9.0x7.9x6.2cm - 3½x3¼x2½in. Please note the centimeter cube and inch bar for scale.

Weight in grams and ounces: 541.5g - 19.10oz.

From the Sterling mine, Ogdensburg, NJ.
 
The previous collection this specimen was in is #243, Richard Bostwick Collection.

#243 is the museum's Collection Sale number previously offered in the museum shop.

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All potential buyers need to be aware that being able to view fluorescent minerals requires an ultraviolet lamp. Most of the minerals from the Franklin and Sterling Hill zinc mining district fluoresce under shortwave ultraviolet lightThe shortwave wavelength is 254nm or otherwise known as UV C. Always read the description carefully to determine if the main mineral of interest for a particular specimen will fluoresce. ALL fluorescent minerals depicted in our storefront are illuminated by two (2) 35 watt Triple short/mid/long wave AC 35SML-110/220 Way Too Cool LLC ultraviolet lamps. There are several available brands and models of ultraviolet lights on eBay and other online sources. For further information on ultraviolet light and fluorescent minerals, copy and paste the following and go to >>> geology.com/articles/fluorescent-mineral/.

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DISCLAIMER: Every reasonable effort was made to identify the mineral species noted in each specimen accurately. The occasional label from previous collection(s) may misidentify some species, and the current title and description here reflect the latest mineral species identification. A modest effort was made to depict a fluorescent specimen accurately as possible.
In some cases, overexposure should be expected in select photographs to compensate for a fluorescent specimen's weak response. All buyers should exercise safe viewing practices regarding the use of ultraviolet light. Visual dark adaption is highly recommended in the optimal viewing of fluorescent minerals. Buyers should also be aware of what type of lighting to view the specimens under. This can result in perceived differences of color and contrast due to color and contrast shifting under various kinds of lights available.
All photographs were taken with a Nikon D5300 digital camera with a Nikon DX AF-S 18-55mm lens attached with a UV filter. Lighting was done with a pair of OSRAM 8.5 watt LED A19 5000K 800 lumens bulbs in brushed aluminum reflectors. The photographs were processed on a color-calibrated flat panel monitor. Do note the Imperial measurement conversion is the nearest equivalent to the listed metric measurement.

--- All photographs appearing on this listing or any other Franklin Mineral Museum listing are the property of the Franklin Mineral Museum. Photographs can be used strictly for personal use only. Otherwise, the photographs posted here are protected by U.S. Copyright Laws. They are not to be downloaded or reproduced for public use or distribution in any way without the written permission of the Franklin Mineral Museum.