(Fr- agate; Ger- Achat;
Nor-agat; Rus-
)
AGATE, SiO2. (See also CHALCEDONY, ONYX and THUNDER EGG entries.)
A. Agate, polished surface of a Lake Superior agate (width ~ 8 cm) from Keweenaw Point, Michigan. Specimen collected, cut and polished by Robert J. Barron. Seaman Museum, Michigan Technological University. (© photo by John Jaszczak)
B. Fire Agate (greater dimension - 2.1 cm) from Deer Creek, Arizona. Rincon Mineral Co. (© photo by Jeffrey A. Scovil)
C. Iris agate (width - 9 cm) from Patagonia, Argentina. St. Paul Gems & Minerals. (© photo by Jeffrey A. Scovil)
D. Agate mouse (height - ca. 6 cm) carved by Gerd Dreher. Silverhorn. (© photo by Jeffrey A. Scovil)
E. "Joshua tree agate" (width - 6.4 cm). Jimmy Vacek collection. (© photo by Jeffrey A. Scovil)
F. Moss agate cabochon (greater dimension - 4.8 cm) from India. Zeolites India. (© photo by Jeffrey A. Scovil)
G. Agate (width - 28.4 cm) from Rio Grande
do Sul, Brazil, that has been dyed with diverse hues. Frederick
H. Pough collection. (© photo by Jeffrey A. Scovil)
H. Agate from Idar-Oberstein, Germany --
see photograph, full caption and related text under REMARKS
subheading.
[See also Figures 51-59 and AppB1-AppB10 in the MIMETOLITH file on this web site.]
DESCRIPTION: Primarily, agate is
conspicuously banded chalcedony; the bands range from parallel to
highly uneven, even within some individual specimens. Both
color and light transmission commonly differ from band to band.
In addition, chalcedony with variously shaped splotchy areas,
commonly having arborescent shapes are called agate, usually moss
agate.
Colors - reddish brown, yellowish brown,
green (rare), blue (rare), purplish, white
(including milky and bluish white), gray, greenish gray, black,
and brown
H. 6½-7
S.G. 2.59-2.67
Light transmission - transparent to
subtranslucent
Luster - waxy
Breakage - subconchoidal
fracture yielding fine granular appearing surfaces
Miscellaneous
- commonly triboluminescent.
1. John Sinkankas (1959) described flame agate as a "highly translucent, colorless agate with few typical agate bands, but rather containing long streaks or 'flames' of a bright red color" (see Johnson and Koivula, op cit., Figs. 4 and 5). The material he described came from Villa Ahumada, Chihuahua, Mexico.
2. H.G. Macpherson (1989) applied the term flame agate to an "agate of any color in which the pattern resembles a candle flame" (see Johnson and Koivula, op cit., Fig. 3). Many agates from many worldwide localities, if correctly fashioned, could be designated as flame agate under this definition.
USES: Jewelry, letter openers, handles for cutlery, paper weights, bookends, picture frames, giutar picks, bowls, coasters, etc. High quality cameos and intaglios and other engravings fashioned from agate (see also ONYX entry) have been used in such diverse pieces as earrings, brooches, pendants, plaques and tietacks -- see the fine example pictured on the cover of the spring issue of Gems & Gemology, volume 19. One of the most interesting pieces fashioned from agate that I know about is the head of a Scepter from Cyprus, now in the Metropolitan Museum of Art at New York City.
Eye agates, especially those with dark centers, were used for the eyes in carvings of idols, particularly in ancient Egypt.
Spendlove (1979) illustrates agates – e.g., ruin agates – upon which art work has been painted. Painters have also used other agates as backgrounds for their paintings.
Chalcedony, especially agate, has been used along with other gemrocks, such as lapis lazuli, malachite and rhodochrosite, in the production of intarsias (gemstone inlays) since at least the late 17th century.
Two other uses of agates, not as a gemrock but of possible practicable interest, are for the production of mortars and pestles and the fulcrums for balances.
Perhaps one of the best known uses of agate, especially in the past but persisting today, is as the small spheres used for "shooting marbles." Indeed, some people call marbles (mibs) -- including those not made of agate -- "agates."
OCCURRENCES: Agates most commonly occur as cavity fillings (nodules) in consolidated basaltic magmas and in detrital material (e.g., alluvium, beach gravels and glacial deposits) derived from those rocks. Noteworthy quantities also occur as so-called replacement fossils -- e.g., agatized wood.
NOTEWORTHY LOCALITIES: Much of the color-banded agate of the marketplace has come from a roughly belt-shaped region that extends from near Salto, in eastern Argentina, to near Porto Alegre, Rio Grande do Sun, southern Brazil. Noteworthy quantities have also come from the Deccan "trap rocks" (i.e., basaltic rocks) of India; from a number of regions in China; and from the Agate Creek area of North Queensland, Australia. Several diverse kinds of agates have been found at literally scores of localities in North America -- see, for example, those noted in the articles in the book compiled and edited by Leiper (1966). See also those noted after some of the agates listed under the OTHER NAMES subheading.
Another possible locality(?): David Livingstone, the famous Scottish missionary and African explorer who discovered Victoria Falls in 1855, wrote (1865), "The ground is strewn with agates for a number of miles above the falls." According to information Craig Gibson (personal communications and enclosures sent 2005) agate amygdules do occur in basaltic lavas that crop out at Victoria Falls; however, he also notes, "I have never heard of the agates from the Falls area being used in any commercial manner and I am sure that if they had been that would have been mentioned in the literature."
REMARKS:Theophrastus in his well-known On Stones (ca. 315 B.C.) indicates that the designation agate was based on the source of such stones from the Achates (now Drillo) River in southwestern Sicily, which, by the way, is still a source of agate and chalcedony. Be that as it may, between 3000 and 2300 B.C., Sumerains (and apparently even earlier, Babylonians) fashioned agate into axe heads, some of only ceremonial use.Many color-banded agates of the marketplace have been dyed. Indeed, agate can be dyed almost any color or black by soaking it in various chemical solutions (see Fig. G). (It is surprising that someone has not differentially dyed, for example, fortification or ruin agates, to distinquish what might be interpreted as ground versus sky, etc. -- Perhaps someone has and I have just not seem the results.) In addition, heat treatments have been used -- both alone and along with, for example, immersion in certain chemicals -- to change agates' colors.
Agate per se has long been reputed to prevent or help cure all sorts of disorders -- e.g., to prevent insomnia and even as a follow-up to promote pleasant dreams. In addition, agate has been said to make people more persuasive and less disagreeable. Also, eye agate amulets have been, and in some places continue to be, attributed the power of curing skin diseases; but, elsewhere their "fixed stare" is said to have raised all kinds of reprehensible reactions, including those associated with the proverbial "evil eye." In addition, moss agate also has been given several health-related attributes, especially those related to people's eyes and mouths. -- A list of legends associated with agate could go on and on ... and on. The following lines of poetry about moss agate, said to have been written in the 4th century A.D. (King, 1865), serve, I think, as a fitting closing for this paragraph:
"Carrying the Tree-Stone with thee to the shrine,
Thou shalt propitiate each power divine.
The gem the semblance of a garden shows,
Where growing trees entwine their leafy boughs;
Hence a fit title bears it with the wise
Who the Tree-Agate is a treasure prize:
One part displays the perfect Agate-stone,
In one a shaggy grove is plainly shown."
H. Agate slice (greater dimension - 13
cm) from Baumholder, near Idar-Oberstein, Rhineland-Palatinate,
Germany -- see the following paragraph for additional information.
Donald Gabriel Collection (DCG 355) in Seaman Museum, Michigan Technological University. (©
photo by George Robinson)
Agates, in lava flows in the vicinity of Idar-Oberstein, southwestern Germany, served to initiate the stone cutting industry that led to these towns' becoming one of the world's largest centers for cutting and polishing colored stones. Foshag (1953) notes that "The Idar-Oberstein agate is a distinctive type .... It is, generally, more colorful than agates from other areas; many show a rich, red color delicately mottled or spotted. Other types show a sharp narrow zoning of dense layers. A common characteristic is an outer zone of dense, finely banded agate with a central filling of crystalline quartz or amethyst. Although many small amygdules of agate can be seen in the basalt cliffs [of the area], pieces of usable size were and are now extremely rare." George Robinson (personal communication, September, 2004) notes of the specimen shown as "H": "Its colors are incredible (and natural!) and it is perhaps the finest agate in our [theSeaman Museum] collection."
Agate was apparently the first stone in Aaron's
breastplate
(see GLOSSARY) and is thought by some scholars to have occupied
position number nine in High Priests' breastplates. Agate is considered by some people to be the birthstone for June, and by others to relate
to the zodiac symbol Gemini (May 21 - June 21).
A rather interesting aspect of recovery of
dendritic agates in central India is reported by Weldon (2008):
"Miners work the riverbed twice a year during the region's dry
seasons. One unusual approach taken by local miners is to plant
cucumbers and other deep-rooting vines in the riverbed, where the
fast-growing roots reportedly loosen the soft alluvium, causing many
nodules to rise to the surface. These are then easily collected
for cutting."
The Fairburn agate, also called fairburnite is the official state gemstone of South Dakota; individual specimens of these agates, which are fine examples of fortification and riband agates, occur sporadically in gravels in the Black Hills of South Dakota (Clark, R.W., 1998). Agate referred to as Lake Superior or Duluth agate in Minnesota, and sometimes called Keweenaw or Isle Royale agate in Michigan, is the official state gemstone of Minnesota. Blue agate and Prairie agate are, respectively, Nebraska's official state gem and state rock. Agate, otherwise not specified, is one of two state gemstones of Montana.
SIMULANTS:
***Agate ware - Wedgwood china made to roughly resemble agate. - [Appearance is sufficient to distinguish this material from agate.].
Brecciated travertine - this gemrock is sometimes marketed as mosaic agate. - [inferior hardness].
***Ceramic ware with enclosed horsehair --e.g., some off-white ceramic bowls (etc.), whose clay precursor had horsehair added to it prior to its being fired, that roughly resemble moss agate. I have seen only photographs of these advertized as having been made by "Acoma Pueblo artists." - [Appearance suffices to distinguish this material from moss agate.].
***Glass - Marilyn Jobe of Ellenton, Florida has produced glass, fashioned as beads and cabochons, that closely resembles agate - [inferior hardness (H. ~ 5)].
Imposed (etc.) dendrites - 1.a somewhat complicated procedure has been used to produce native copper dendrites on chalcedony (Koivula, 1986, p.246); 2.the dendritic inclusions of some plume agates have been produced by electrically stimulated chemical precipitation and thence incorporated as parts of assembled stones; [and] 3.a chalcedony cabochon with a dendritic-shaped pattern painted on it to give it a moss agate appearance has been recorded (Kane, 1988).
***Plastic - a photograph of a "plastic imitation
simulating agate" is shown by Nassau (1974). - [inferior hardness (H.
< 5)].
Royal agate - term sometimes given to mottled obsidian. - [inferior hardness (H. 5-5½)].
***Stratified Pyrex - pyrex glass with layers of more than one color. - [inferior hardness (H. ~ 5)].
Whale molar (dyed) - some beads of this material closely resemble agate; Liu (1994, p.74) illustrates a couple of these beads that have been termed "crane's crest" - [texture and inferior hardness (H. ~ 3)].
REFERENCES: Cross,
1998;
Dake, Fleecer and Wilson, 1938; Frondel, 1962; Leiper,
1966;
Macpherson, 1989. (For information re dendrites, see Potter and
Rossman, 1979A).
R. V. Dietrich © 2008
Revised: November 1, 2008
web page created by Emmett Mason