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Unakite

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Multicoloured metamorphic rock
Unakite
Epidotized granite[1]
Metamorphic rock
Tumble polished unakite pebbles
Composition
Orthoclase feldspar,epidote,quartz
Physical Characteristics
FabricMottled
Relationships
ProtolithsGranitoids andcharnockite

Unakite is a coarse-grainedmetamorphic rock that is an alteredgranitoid composed oforthoclase feldspar (pink),epidote (yellow-green), andquartz (smokey or colorless).Albite-oligoclaseplagioclase (white) may or may not be also present.[1][2]

Bradley first defined and described Unakite in 1874. He named it forUnaka Range of theGreat Smoky Mountains of westernNorth Carolina and EasternTennessee. He collected his samples primarily from "The Bluff", "Walnut Mountain", and "Max's Patch" inCocke County, Tennessee.[3]

Bear carved from unakite. Length 8 cm.

Origin

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Generally, unakite is interpreted to be ametamorphic rock created by thehydrothermal alteration of eithergranite,granodiorite, orcharnockite. It is argued that the epidote in unakite was created by the alteration of eithermafic minerals;[3]biotite and feldspar;[4][5] or some combination of these minerals by hydrothermal fluids. It is also possible that some of the epidote is the result of directprecipitation from hydrothermal fluids.[6][7]

Most commonly, unakite occurs as comparatively small and restricted bodies in granite and granodiorite. Typically, these bodies are not larger than 15 m (49 ft) in any dimension. In these granitoids, unakite also occurs asveins,dike-like bodies, lenses, irregular masses, or combinations of these.[6][7]

Locally inShenandoah National Park, hydrothermal alteration has convertedcharnockites of theCatoctin Formation to unakite, characterized by green epidote, pink feldspar and blue quartz.[8][9] Where thelava flows of theNeoproterozoic Catoctin Formation directly overlie it, the dark-greenish-gray charnockite is typically bleached light gray due to therecrystallization of its plagioclase and alkali feldspar. Alongjoints, the migration of hydrothermal fluid induced by heat from the overlying lava has altered the charnockites to unakite. Overall, unakite in Blue Ridge region is associated with either Neoproterozoic extrusion of lavas of the overlying Catoctin Formation; enhanced fluid flow associated withfault zones; or local effects of regionalPaleozoicmetamorphism.[10]

Distribution

[edit]

The distribution of unakite is not precisely known. In part, this lack of knowledge it is due to inconsistencies in how unakite is defined and inconsistent classification of it under other names. It occurs in at least 30 locations in the United States including a few places west of the Mississippi River.[6][7] Still, the majority of finest unakite is largely restricted to the Blue Ridge region of North Carolina and Virginia with lessor quality unakite found in westernmost Tennessee.[11]

Unakite from near Buena Vista, Virginia

Although found exposed in roadcuts, crush stone pits, and other excavation in the Blue Ridge region, high quality unakite is also found in the stream beds as rolled, well-rounded stones as in the Rose River, northwest ofSyria, inMadison County, Virginia. The stones have a rusty surface experience and vary in size from cobbles to boulders.[12][13]

When collecting in the Blue Ridge region, it must be remembered that unakite occurs in national and state parks in which, of course, rock collecting is prohibited by law. Rock hunting is permitted in national forests, except in certain designated areas. Outside of the parks, the state and national forests, the land is all privately owned, and land owner permission is required for collecting, even if the land is rugged and mountainous and seemingly deserted.[11][13]

Elsewhere in the United States, the occurrence of unakite has been reported. Within the eastern United States, unakite has been reported from Passic County, New Jersey[6] andMarblehead Neck, Massachusetts.[14] In the Midwest, unakite of unknown quality has also been reported from the Waupacaadamellite fromWaupaca County, Wisconsin.[15] Finally, in the western United States, unakite has also been reported fromTeller County, Colorado andBernalillo County, New Mexico.[6]

Unakite has also been reported and listed as having been found at locations outside of North America. For example, Wahl reports the occurrence of unakite within northeasternFinland at about 30 to 40 locations. These unakites are often associated withhypersthene granites.[16] Unakite is listed by Manutchehr-Danai, without any accompanying documentation, as having been found inZimbabwe,Ireland, andSouth Africa.[17]

Use

[edit]

A good quality unakite is considered asemiprecious stone; it will take a good polish and is often used injewelry as beads orcabochons and otherlapidary work such as eggs, spheres and animal carvings.[6][12][13]

See also

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References

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  1. ^abO’Donoghue, M., 2009.Gems Their Sources, Descriptions and Identification, 6th ed. Jordan Hill, Oxford, Butterworth-Heinemann, 906 pp.ISBN 978-0-75-065856-0
  2. ^Johannsen, Albert., 2009.A Descriptive Petrography of the Igneous Rocks, vol. II. Chicago, Illinois, University of Chicago Press, 906 pp.
  3. ^abBradley, F. H., 1874.On unakyte, an epidotic rock from the Unaka Range, on the borders of Tennessee and North Carolina.American Journal of Science, 7, 3rd series, pp. 519- 520.
  4. ^Watson, T.L., 1904.Granites of North Carolina.The Journal of Geology, 12(5), pp.373-407.
  5. ^Watson, T.L., 1910.Granites of the Southeasterri Atlantic States.US Geological Survey Bulletin 426. 282 pp.
  6. ^abcdefVanlandingham, S. L., 1962a.The gem rocks; Part 3, Unakite.Gems and Minerals, 297, pp. 28-31.
  7. ^abcVanlandingham, S. L., 1962ba.The gem rocks; Part 4, Unakite.Gems and Minerals, 297, pp. 26-29.
  8. ^Gathright, T.M., 1976.Geology of the Shenandoah National Park. Virginia.Virginia Division of Mineral Resources Bulletin, 86. 93 pp.
  9. ^Dilliard, K.A., Simpson, E.L. and Noto, R.C., 1999.A Neoproterozoic paleosurface and associated colluvial and fluvial deposits. Shenandoah National Park, Virginia.Southeastern Geology, 38, pp.239-257.
  10. ^Southworth, S. and Burton, W.C. eds., 2004. 2004.Geology of the National Capital Region-Field Trip Guidebook: Joint Meeting of Northeast and Southeast Sections Geological Society of America Tysons Corner, Virginia March 24-27.US Geological Survey Circular 1264, 1264. 289 pp.
  11. ^abZeitner, J.C., 1968.Appalachian Mineral & Gem Trails. San Diego, California, Lapidary Journal, Inc. 134 pp.
  12. ^abMitchell, R.S., 1977.Unakite.Rocks & Minerals, 52(5), pp.229-229.
  13. ^abcOwens, V.S., 1977.Unakite.The Lapidary Journal, 31(1), pp.182-184.
  14. ^Phalen, W.C., 1904.A New Occurrence of Unakite-a Preliminary Paper.Smithsonian Miscellaneous. Collections, XLV, pp. 306-316.
  15. ^Fronk, J., 1988.An investigation into the chemical processes causing the formation of unakite in the Waupaca adamellite of Wisconsin.Institute on Lake Superior Geology, Thirty-fourth Annual Meeting Marquette, Michigan May 12 and 13, 1988, Proceeding and Abstracts, 34(1), pp. 33.
  16. ^Wahl, W., 1963.The hypersthene granites and unakites of Central Finland.Bulletin de la Commission Géologique de la Finlande, 212, pp. 83-100.
  17. ^Manutchehr-Danai, M., 2005.Dictionary of Gems and Gemology, 2nd ed. Heidelberg, Germany, Springer, 879 pp.ISBN 978-3-540-33559-7
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