Sunstone

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Sunstone
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General
CategoryTectosilicate minerals
GroupFeldspar group
SeriesAlkali feldspar series
Formula(Ca,Na)((Al,Si)2Si2O8)
IMA statusVariety of microcline or oligoclase
Crystal systemTriclinic
Identification
ColorColorless, orange, yellow, red, green, blue, brown, and copper shiller
Crystal habitEuhedral crystals, granular
TwinningLamellar
Cleavage001
Mohs scale hardness6.0–6.5
DiaphaneityTransparent to translucent and opaque
Specific gravity2.64–2.66
Refractive index1.525–1.58

Sunstone is a microcline or oligoclase feldspar, which when viewed from certain directions exhibits a spangled appearance. It has been found in Southern Norway, Sweden, various localities in the United States, and on some beaches along the midcoast of South Australia.

Properties

Physical properties

Unpolished sunstone
A small rolled sunstone

The optical effect is due to reflections from inclusions of red copper, hematite, or goethite, in the form of minute scales, which are hexagonal, rhombic, or irregular in shape, and are disposed parallel to the principal cleavage-plane. These inclusions give the stone an appearance something like that of aventurine, hence sunstone is known also as "aventurine-feldspar". The optical effect is called schiller and the color of Oregon Sunstone is due to copper. The middle part of this crystal sparkles, and usually the color is darkest in the middle and becomes lighter toward the outer edges.

The feldspar which usually displays the aventurine appearance is oligoclase, though the effect is sometimes seen in orthoclase: Hence two kinds of sunstone are distinguished as "oligoclase sunstone" and "orthoclase sunstone".

Distribution

Sunstone was not popular until recently.[when?] Previously the best-known locality being Tvedestrand, near Arendal, in south Norway, where masses of the sunstone occur embedded in a vein of quartz running through gneiss.

Other locations include near Lake Baikal in Siberia, and several United States localities – notably at Middletown Township, Delaware County, Pennsylvania; Plush, Oregon; and Statesville, North Carolina.

The "orthoclase sunstone" variant has been found near Crown Point and at several other localities in New York, as also at Glen Riddle in Delaware County, Pennsylvania, and at Amelia Courthouse, Amelia County, Virginia.

Sunstone is also found in Pleistocene basalt flows at Sunstone Knoll in Millard County, Utah.[1]

Oregon sunstone

Various gem colors of Oregon sunstone

A variety known as "Oregon sunstone" is found in Harney County, Oregon and in eastern Lake County north of Plush. Oregon Sunstone contains elemental copper.[2] Oregon Sunstone is unique in that crystals can be quite large. The copper leads to variant color within some stones, where turning one stone will result in manifold hues: The more copper within the stone, the darker the complexion.[3]

On 4 August 1987, the Oregon State Legislature designated Oregon Sunstone as its state gemstone by joint resolution.[4]

Andesine controversy

In the early 2000s, a new variety of red or green gemstone resembling sunstone and called "andesine" appeared in the gem market. After much controversy and debate, most of these gemstones, allegedly sourced from China, were subsequently discovered to have been artificially colored by a copper diffusion process.[5] A Tibetan source of bona fide (untreated) red andesine, however, was eventually verified by a number of independent groups of well-respected gemologists.[6][7][8][9][10]

See also

References

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  1. ^ Page Module:Citation/CS1/styles.css has no content."Sunstones at Sunstone Knoll, Millard County". Utah Geological Survey (geology.utah.gov). Retrieved 14 September 2007.
  2. ^ Page Module:Citation/CS1/styles.css has no content.Hofmeister, A.M.; Rossman, G.R. (1985). "Exsolution of metallic copper from Lake County labradorite". Geology. 13: 644–647.
  3. ^ Page Module:Citation/CS1/styles.css has no content."Oregon sunstone – official state gemstone". Rock hounding. Nature of the Northwest (naturenw.org). Archived from the original on 24 April 2015. Retrieved 7 March 2013.
  4. ^ Page Module:Citation/CS1/styles.css has no content."Chapter 186 – State Emblems; State Boundary". Oregon Revised Statutes (Legislation). 2017 – via oregonlegislature.gov.
  5. ^ Page Module:Citation/CS1/styles.css has no content."Three occurrences of Oregon sunstone". Gemological Institute of America (gia.edu). Gems & Gemology.
  6. ^ Page Module:Citation/CS1/styles.css has no content.Huges, Richard W. (14 November 2011). "Tibet andesine mines; Part 2". ruby-sapphire.com. RWH Publishing. Retrieved 9 November 2014.
  7. ^ Page Module:Citation/CS1/styles.css has no content.Huges, Richard W. (3 November 2010). "Tibet's andesine mines [Part 1]". ruby-sapphire.com. RWH Publishing. Retrieved 9 November 2014.
  8. ^ Page Module:Citation/CS1/styles.css has no content.Abduriyim, Ahmadjan (10 September 2009). "A mine trip to Tibet and Inner Mongolia: Gemological study of andesine feldspar" (PDF). Bangkok, TH: Gemological Institute of America in Thailand (GIA Thailand). Retrieved 9 November 2014 – via giathai.net.
  9. ^ Page Module:Citation/CS1/styles.css has no content.Abduriyim, Ahmadjan (2009). "The characteristics of red andesine from the Himalaya Highland, Tibet". The Journal of Gemmology. 31 (5–8): 134–150. doi:10.15506/JoG.2009.31.5.283.
  10. ^ Page Module:Citation/CS1/styles.css has no content.Abduriyim, Ahmadjan; Kobayashi, Taisuke (2008). "Visit to andesine mines in Tibet and Inner Mongolia; Gemological properties of andesine collected in Tibet and Inner Mongolia". Gem news international. Gems & Gemology. 44 (4): 369–373. doi:10.5741/GEMS.44.4.369.

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