( Fr- graphique granit/pierre hébraïque/; Ger- Schriftgranit; Nor- skriftgranitt;
Rus-  )


A. Graphic granite specimen (greatest dimension  ~12 cm) from Berry pegmatite, Poland, Maine. The Hadleigh Collection.  (©  photo by F.C. Wilda,

B. Graphic granite cabochon pendant (greater axis of cabochon - 3.0 cm) fashioned by  Frederick C. Wilda from rock collected at the Berry pegmatite, Poland, Maine. The Hadleigh Collection. (©  photo by F.C. Wilda,

C.  Graphic granite background. Tiled image of polished surface (vertical dimension  ~7.5 cm) cut perpendicular to the length of the quartz "rods".  (© photo by Dick Dietrich)

[See also Figure 27 in the MIMETOLITH file on this web site.]

DESCRIPTION: Typical graphic granites consist of nearly parallel rodlike masses of quartz surrounded by feldspar -- see Figure A.  The quartz:feldspar ratio in these rocks ranges from about 10:90  to  50:50 -- i.e., the feldspar component is greater in nearly all specimens.
    Colors - felsdpar "host" may be off white, cream, tan, pink or salmon;  quartz ranges from nearly colorless through white to smoky.  The feldspar -- typically perthitic, commonly  macroperthitic so the volume of the potassium feldspar can be seen to exceed that of the plagioclase - - of virtually all individual specimens comprise single grains.
    H. 6 (feldspar), 7 (quartz)
    S.G. ~2.6 -- i.e., 2.574 (feldspar) and 2.65 (quartz)
    Light transmission -overall subtransparent to opaque
    Luster - pearly to dull (feldspar), vitreous on fractures (quartz)
    Breakage -  tends to break along cleavage planes of feldspar and/or away from the quartz rods (i.e., so-to-speak freeing them from the surrounding feldspar)
    Miscellaneous - Appearance, often referred to as an "intergrowth" of alkali feldspar and quartz, is the definitive characteristic.


USES: As gemstones -- typically cabochons or free forms -- for pieces such as pendants;  spheres (some extremely attractive!);  relatively large pieces such as desk sets and bookends.

OCCURRENCES: In some, but not all, granitic pegmatite masses and as clasts in, for example, beach shingles and glacial debris derived from those masses.  

NOTEWORTHY LOCALITIES: So far as its use as a gem rock, none in particular;  however, graphic granite should be looked for wherever granitic pegmatites occur -- e.g., in the Piedmont Province of Virginia and North Carolina.  Three locations of pegmatites masses where I have found good specimens are:  near Pala, San Diego County, California;  at Bedford, Westchester County, New York;  and near Custer, Custer County, South Dakota.  In addition, I have also collected graphic granite pebbles and cobbles, which have been fashioned into pendants, from glacial debris in Michigan and from beaches along northern Lake Michigan and southern Lake Superior.  And, some noteworthy specimens in the CMU student collections are labeled as coming from near Ohio, Gunnison County, Colorado.  Also, my attention was recently directed to a photograph of an especially fine specimen of graphic granite from the Talacha pegmatite field, which is near the Duldurginsky granite massif in Agin-Buryat Autonomous Okrug -- i.e., about 150 km south of the city of Chita, which is in theTransbaikal region, east of Lake Baikal, Russia (Margarita I. Novgorodova, personal communication, August, 2005).

REMARKS: The names given this rock in different several languages are based on the appearance of its isolated quartz rods as seen on surfaces cut perpendicular to their lengths:  They roughly resemble letters of cuneiform inscriptions or letters the Hebrew or Arabic alphabets.

From an historical standpoint, and interesting petrographically, the term pegmatite -- currently used widely to describe coarse-grained igneous/igneoid (e.g., granitic) rocks -- was originally applied by L'Abbe Hauy to graphic granite (Brongniart, 1813, p.32).  Hauy's use is quite understandable when one considers the derivation of the word pegmatite -- from the Greek  πηγματ  meaning “thing joined together or conglutinated” + ite (OED), certainly in allusion to the intimate "intergrowth" of the alkali feldspar and quartz of graphic granite.

These "intergrowths" range in size from microscopic to the gemrock material with individual feldspar grains up to several decimeters in greatest dimension and quartz rods up to several centimeters long.  The term "intergrowth" is enclosed herein by quotation marks because there is less than a consensus among petrologists as to how these rocks originated:  Some consider them true intergrowths -- i.e., that the feldspar and quartz formed as the result of essentially simultaneous crystallization;  others conclude that the quartz represents partial replacement of   previously crystallized feldspar grains;  and others offer other hypotheses or suggest that each occurrence needs to be considered individually and some may have originated one way and others other ways.   For those interested in the genesis or geneses of this gemrock, several articles are in geological publications (see, for example, Barker, 1970 and Fenn, 1986). 

Early use of graphic granite as a decorative stone is shrouded in antiquity.  More recently, it was incorporated in the façade of one of the Vitelli family  Palaces, built during the late 15th or early 16th century at Città di Castello,Italy (  Currently, “graphic granite is used by cooperatives and amateur craftsmen as a decorative material” in the Chelyabinsk region of the southern Urals, Russia -- i.e., at the Taiginka graphite deposit ( --  as well as by several lapidaries here and there throughout the world .

SIMULANTS:  None that I have seen or seen described.

REFERENCES: No general reference. VanLandingham, 1962, pt.8.

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R. V. Dietrich © 2014
Last update:  16 August 2005
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