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Jade - gift of the gods

JADEITE
By Kim Be Howard, A.G. (C.I.G.)

Introduction

Jadeite is one of the minerals that fall under the generic category of jade.

The word jade is used in both English and French and came, according to the Oxford Universal English Dictionary (Little, Fowler, and Coulson 1955: 1057) from the Spanish word ijada. The Spanish referred to it as piedra de ijada, or colic stone. The reason for this is that when the Spanish conquered Mexico they discovered that people in Mexico powdered jadeite and mixed it with water as a cure for numerous internal disorders. The first recorded use of this term is by Nicol Monardes in a work on medicinal plants of the New World written in 1565 (Easby 1968: 7).

The two stones that are primarily categorized as jade are nephrite and jadeite. initially they were  considered to be the same mineral, but in 1863 they were found to differ (Damour 1863, and see Damour 1846, 1881). Damour discovered that one variety of jade was a silicate of sodium and aluminum, whereas the other was a silicate of lime and magnesia. As a result of his findings, he (1863: 865) proposed the name "jadéite" for the first mineral to distinguish it from the second (i.e., nephrite). The present paper focuses on jadeite.

Jadeite is closely associated with two ancient civilizations, those of Mesoamerica1 and China.  Jadeite was used by most of the major civilizations in ancient Mesoamerica: the Olmec, Aztec, Maya, and so forth. It was highly prized throughout the region: "Gold did not have the same intrinsic value for Mesoamerican peoples... that is has for us...Jade was of greater value" (Noguera 1971: 268). Among the early Spanish writers of the sixteenth century, Sahagun (1963: 222) comments that "emerald green Jade... its appearance is like a green quetzal feather. And its body is as transparent and as dense as obsidian. It is precious, esteemed, valuable..." In his account of Aztec civilization, Vaillant (1965: 139-140) remarks:

The most precious substance among the Aztecs was jade, or stones resembling it in texture and colour... The Aztecs did not have our modern esteem for gold, so the Spaniards had great difficulty in getting it at first. The Mexican Indians responded to the invaders' demands for objects of value by offering jade and turquoise, those substances most precious to themselves... Such misguided compliance was highly irritating to Cortés and his men.

In fact, a number of writers have commented on the contrast in value placed on jade by the people of Mesoamerica and the views towards the stone by the Spanish conquerors. This difference can readily be seen in an account of gifts given by the Aztec ruler Montezuma and the Spanish leader Cortés:

Cortés and Montezuma were accustomed to play each day a native game which in many ways resembles chess... It was their further custom at the close of each day's game to present each other with some gift. At the close of one day's game the Aztec monarch presented Cortés with several large discs of gold and silver handsomely worked. Cortés was greatly pleased and so expressed himself. Montezuma smiled and said: The gift tomorrow shall be such that today's gift will seem in value and preciousness, when compared with it, as no more than a single stone tile on the roadway... The royal treasurer of Montezuma brought in on a golden slaver the royal gift, four small carved jade beads. The bitter disappointment of Cortés was so great that he could scarcely conceal it" (Willard 1926: 146-147).

This is a theme that, to some extent, continues to this day in respect to the difference in views towards jadeite by Chinese and Westerners. There is an interesting sequel to the above story recounted by Vaillant (1965: 139-140) from the writings of Diaz del Castillo (from chapter 128 of his chronicles):

During the night when Cortés retreated from Mexico, the leader, after taking his share of treasure, turned the surplus over to his troops. Many, burdened down with gold, drowned ignominiously in the canals. Diaz, however, noted Indian usage and confined himself to four jades which he was able to exchange later and which, in his words, "served me well in healing my wounds and gathering me food.

Jadeite in Mesoamerica.

The story of jadeite in Mesoamerica begins with the earliest civilization, that of the Olmec. Formative Olmec civilization was centered in the present western Mexican state of Guerrero, from where it spear eastward towards the Gulf of Mexico around the state of Veracruz. The earliest Olmec pieces of worked jadeite found so far (and the oldest found anywhere in the New World for that matter) are votive celts and axes dating from around 1200-1000 BC (Stone 1993: 142). Ward (1996: 29) comments that "the Olmec carved unsurpassed human figures. Theirs are the strongest representations of human faces ever carved in jade." However, as Rands (1965: 579) notes, carved jadeite from "Preclassic horizons which can be related stylistically to this tradition are not numerous, although a number of carvings with Olmecoid features suggest the early importance of jade and jadelike stones."

Jaideite constitutes only a small portion of the green stones worked by the Olmec. The center of green stone working among the Olmec was apparently in the vicinity of the Balsas River in Guerrero State. Archaeologists have discovered a workshop near the confluence of the Amacuzac and Balsas rivers with "fragments of jadeite, silex, jasper, onyx, and quartz, as well as obsidian and marine shells, dating to about 1000 B.C." (Griffin 1993: 206). Luckert (1976: 94-95) argues that green stones such as serpentine and jadeite were closely related to the Olmec's religious beliefs. He links the rise in the use of such green stones over darker stones like basalt to the evolution of what he refers to as the Olmec serpent cult: "The Serpent of the reform movement was green; and the Snake people of La Venta undertook no less a task than to transform their local portion of the Earth Serpent into a green one." Moreover, he believes that "if ordinary green layers of serpentine rock represented the Green Serpent's body, jades and better grades of serpentine signified the cores of the serpentine essence— the Green Serpent's bones and teeth."

The presence of worked jadeite in numerous Olmec archaeological sites has raised questions about the source(s) of the raw material. It is generally recognized that the worked jadeite found in the Gulf coast of Mexico came from somewhere else. In his discussion of Olmec trade, Coe (1968: 94, 103) refers to what he terms the "jade route" from Guerrero to the Gulf. Writing several decades ago, Adams (1977: 87) stated that Olmec jade was "probably obtained from the Balsas Valley in Guerrero (near the sacred caves of Oxtotitlan and Juxtlahuaca), from the Motagua River Valley in Guatemala..., and from other as yet unknown sources." Reviewing what was known as of the early 1990s, Garber, et al (1993: 213) state:

Although serpentine sources are known for Guerrero [see Gay 1987: 33], jadeite sources apparently remain unknown. The late artisan William Spratling was rumored to have been exploiting a Guerrero jadeite source for his workshop in Taxco. If such a source exists, its location has remained a well-kept secret since his death decades ago. Thus, although Guerrero greenstone may have traveled through Middle Formative period exchange networks to Gulf Coast Olmec centers, the stone may have been serpentine rather than the jadeite Coe hypothesized.

Garber, et al, also review other reported sources (pages 213-214), but the only confirmed source of jadeite that is similar to that worked by the Olmec is from the Motagua River Valley, further to the south in Guatemala and within Maya territory (this site will be discussed in greater length later).

For the Maya the color green was associated with two important life-giving substances, water and maize, and the green stone was therefore viewed as having life-giving properties (Digby 1964: 10-11). Non-jadeite greenstone beads dating from around 1500 BC have been discovered within the Maya area on the Pacific coast of Chiapas (Garber, et al 1993: 211) and it is certainly possible that Maya were carving jadeite prior to the Olmec, but this has yet to be proven. The Maya occupied the southern states of Mexico, Guatemala, Belize, and a portion of Honduras. Blom (1934: 542) remarks that among the Maya:

Feathers were used for personal adornment, as was also jade and gold. The brilliant tail feathers of the 'trogan resplendens,' the vivid green of jade, were rare and therefore commanded a high price. The maize-plant was green, the forest was green. All good as well as rare things were green, and therefore the Maya considered green a sacred color, attached special value to green things; just as the Spaniards, and we do to this day, express wealth, abundance and luxury in gold, and more frequently in gilt... Even small slivers of jade were polished and perforated for suspension, and large pieces were carved in the shape of human faces, animals, or... shaped like a hand.

Most of Mayan jadeite objects date from the Classic period (300-1000 AD). In the Maya lowlands of Yucatan during the late Classic Period many jadeite items have been found (see Proskouriakoff 1974), but much (if not all) of this appears to have been imported, probably from the Motagua River Valley. During the postclassic period, Rands (1965: 579) states that "Maya jadeworking seems to have suffered a severe decline." Nevertheless, jade remained highly valued. Bishop Diego de Landa (1941), writing around the time of the Spanish conquest reported that jade beads were used by the Maya of Yucatan as money.

Archaeologists have been interested in discovering the source of Maya jadeite for a long time. Blom (1934: 542) wrote in the 1930s that "... the knowledge of the ancient jade-mines has been lost. There is an indication that these mines were already lost or exhausted in [ancient] Maya times." The latter belief was based on the fact that when Blom was writing archaeologists had found that relatively large pieces of carved jade were found in the older burial sites, whereas in more recent sites they tended to find "re-worked pieces—i.e., larger objects that have been cut into smaller pieces and re-carved." As will be discussed at length later, it is now believed that most, if not all of the jadeite worked by the ancient Maya came from the Motagua River Valley.

Peoples living further to the north of the Olmec and Maya, such as the Aztec and Mixtec, also valued jadeite and other green stones. Among these peoples, the colossal toad (chalchihuitl) was the symbol for precious stone or jade (Nicholson 1971: fig. 41, pg. 116). I have already mentioned how highly the Aztec valued jadeite. In discussing central Mexico around 600 BC, Adams (1977: 126) states the "jade was used in ear ornaments and other personal jewelry, although this was uncommon. Quite probably, the stone already had assumed its mystical and high status properties and was restricted to persons of high social rank." Further south, in Oaxaca, Adams (1977: 213) mentions archaeologists finding "some carved jades" in the tombs of Monte Alban that "are relatively simple in technique and motif. The best were imports from the Maya highlands."

Jadeite objects also have been found south of the Maya area. A relatively large number of objects have been found in Costa Rica in particular. As noted by Easby (1968: 9), "no region [in ancient Mesoamerica] produced a greater abundance of jade objects than Costa Rica, whose lapidaries were among the most skillful in pre-Columbian America." Unfortunately, relatively little is known about the people who made these figures. Jadeite objects discovered in Costa Rica date primarily from between 500 BC and 700 AD (Stone 1993: 143). The source of the jadeite found in Costa Rica appears primarily to be the Motagua River Valley in Guatemala, although some may have come from local sources as well. Stone (1993: 141) notes that, while jade objects have been found in El Salvador, southern Honduras, and Nicaragua, they are very rare. Garber, et al (1993: 215-219) provide a brief overview of jadeite objects from Honduras (also see Hirth and Hirth 1993). They note (page 215) that jadeite carving in central and eastern Honduras "is part of a broader Honduran stone-working tradition that developed independently of the jadeite carving found among the Maya further to the west." Jadeite appears in Honduras during the Formative Period (700 BC to 400 AD) and "the use of jadeite in public and ritual offerings reached its peak during the first part of the Classic period" (i.e., shortly after 400 AD). Its use in Honduras appears to decline later during the Classic period (which lasted until about 1000 AD) and, while some jadeite objects have been found dating from the postclassic period, they are relatively rare.

Jadeite production in Mesoamerica came to a virtual halt with the coming of the Spanish in the early sixteenth century. The Mesoamerican jadeite industry was revived in 1974 with the founding of Jades, S.A., in Antigua, Guatemala, which was established following the discovery of jadeite deposits in the Motagua River Valley.

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[1]  I use the term Mesoamerica in the present paper to refer to central and southern Mexico, Guatemala, Belize, and western Guatemala.

Nephrite

Nephrite is a variety of the calcium and magnesium rich amphibole mineral actinolite (aggregates of which also make up one form of asbestos). The chemical formula for nephrite is Ca2(Mg,Fe)5Si8O22(OH)2. It is one of two different mineral species called jade. The other mineral species known as jade is Jadeite, which is a variety of pyroxene. Nephrite jade is an ornamental stone, used in carvings, beads, or cabochon cut gemstones.

The name nephrite is derived from lapis nephriticus, the Latin version of the Spanish piedra de ijada.

Nephrite can be found in a translucent white to very light yellow form, in an opaque white to very light brown or gray, as well as in a variety of green colours.

Canada is now the principal source of modern lapidary nephrite.

 

Jadeite

Jadeite is a pyroxene mineral with composition NaAlSi2O6.

It is monoclinic. It has a Mohs hardness of about 6.5 to 7.0 depending on the composition. The mineral is dense, with a specific gravity of about 3.4. Jadeitite forms solid solutions with other pyroxene endmembers such as augite and diopside (CaMg-rich endmembers), aegirine (NaFe endmember), and kosmochlor (NaCr endmember). Pyroxenes rich in both the jadeite and augite endmembers are known as omphacite.

Jadeite is formed in metamorphic rocks under high pressure and relatively low temperature conditions. Albite (NaAlSi3O8) is a common mineral of the Earth's crust, and it has a specific gravity of about 2.6, much less than that of jadeite. With increasing pressure, albite breaks down to form the high-pressure assemblage of jadeite plus quartz. Minerals associated with jadeite include: glaucophane, lawsonite, muscovite, aragonite, serpentine, and quartz.

Rocks that consist almost entirely of jadeite are called jadeitite. In all well-documented occurrences, jadeitite appears to have formed from subduction zone fluids in association with serpentinite, as discussed by Sorensen et al. (2006). Jadeitite is resistant to weathering, and boulders of jadeitite released from the serpentine-rich environments in which they formed are found in a variety of environments.

Jadeite's color commonly ranges from white through pale apple green to deep jade green but can also be blue-green (like the famous and recently rediscovered "Olmec Blue" jade), pink, lavender, and a multitude of other rare colors.  Color is largely affected by the presence of trace elements such as chromium and iron. Its translucence can be anywhere from entirely solid through opaque to almost clear. Variations in color and translucence are often found even within a single specimen. Currently, the best known sources of gem quality jadeite are California, Myanmar, New Zealand and more recently Guatemala; other localities of jadeite include Kazakhstan, Russia, British Columbia, Alaska, and Turkestan.

Jadeite is one of the minerals recognized as the gemstone jade. The other is the green amphibole, nephrite. Jadeite from the Motagua Valley, Guatemala is the stone used by the Olmec, Maya peoples, and the indigenous peoples of Costa Rica.

Typically, the most highly valued colors of jadeite are the most intensely green, translucent varieties, though traditionally white has been considered the most valuable of the jades by the Chinese, known for their carefully crafted jade pieces. Currently, the most highly valued variety of jadeite is known as "Imperial Green" jade and is characterized by an emerald green color with a high level of translucence. It the most expensive gem in the world, weight for weight costing more than diamond. Other colors, like "Olmec Blue" jade, which is characterized by its deep blue-green, translucent hue with white flecking, are also becoming more highly valued because of its unique beauty and historical use by the Mesoamerican Olmec and also in Costa Rica; however, this variety was only recently rediscovered and is only being minimally exploited by native Guatemalans. It is thus difficult to obtain and as yet too rare and little known to have attained great value as a gemstone. When purchasing jade, quality is determined by the degree of translucence, cleanness of color, and purity of color. Occasionally, other minerals like serpentine or quartz are sold as jade but the difference can be determined by cleavage and hardness.


Jadeite Color Examples

Other Ancient American Stones
Greenschist

Greenschist - also known as greenstone - is a general field petrologic term applied to metamorphic and/or altered mafic volcanic rock. The green is due to abundant green chlorite, actinolite and epidote minerals that dominate the rock. However, basalts may remain quite black if primary pyroxene does not revert to chlorite or actinolite. To qualify for the name a rock must also exhibit schistocity or some foliation or layering. An alternate term for these rocks is greenstone. The rock is derived from basalt, gabbro or similar rocks containing sodium-rich plagioclase feldspar, chlorite, epidote and quartz. Chlorite and epidote give the green color.

Greenstone

Greenstone is a common generic term for valuable, green-hued minerals and stones which were used in the fashioning of jewelry, statuettes, ritual tools, and various other artefacts in early cultures. Greenstone artefacts may be made of greenschist, chlorastrolite, serpentine, or other green-hued minerals; the term can also, though less commonly, refer to jade.

Greenstone minerals were presumably selected for their color rather than their chemical composition.

Porphyry

Porphyry is a variety of igneous rock consisting of large-grained crystals, such as feldspar or quartz, dispersed in a fine-grained feldspathic matrix or groundmass. The larger crystals are called phenocrysts. In its non-geologic, traditional use, the term "porphyry" refers to the purple-red form of this stone, or in the Pre-columbian context usually the green colored feldspar, highly valued for its appearance.

The term "porphyry" is from Greek and means "purple". Purple was the color of royalty, and the "Imperial Porphyry" was a deep brownish purple igneous rock with large crystals of plagioclase.

Subsequently the name was given to igneous rocks with large crystals. Porphyry now refers to a texture of igneous rocks. Its chief characteristic is a large difference between the size of the tiny matrix crystals and other much larger crystals, called phenocrysts. Porphyries may be aphanites or phanerites, that is, the groundmass may have invisibly small crystals, like basalt, or the individual crystals of the groundmass may be easily distinguished with the eye, as in granite. Many types of igneous rocks may display porphyrytic texture.

Serpentine

Serpentine is a group of common rock-forming hydrous magnesium iron phyllosilicate ((Mg, Fe)3Si2O5(OH)4) minerals; it may contain minor amounts of other elements including chromium, manganese, cobalt and nickel. In mineralogy and gemology, serpentine may refer to any of 20 varieties belonging to the serpentine group. Owing to admixture, these varieties are not always easy to individualize, and distinctions are not usually made. There are three important mineral polymorphs of serpentine: antigorite, chrysotile and lizardite.

"Their color and mottled scaly appearance is the basis of the name from the Latin serpentinus, meaning serpent rock," according to Best (2003). They have their origins in metamorphic alterations of peridotite and pyroxene. Serpentines may also pseudomorphously replace other magnesium silicates. Alterations may be incomplete, causing physical properties of serpentines to vary widely. Where they form a significant part of the land surface, the soil is unusually high in clay.

Antigorite is the polymorph of serpentine that most commonly forms during metamorphism of wet ultramafic rocks and is stable at the highest temperatures -- to over 600°C at depths of 60 km or so. In contrast, lizardite and chrysotile typically form near the Earth's surface and break down at relatively low temperatures, probably well below 400°C. It has been suggested that chrysotile is never stable relative to either of the other two serpentine polymorphs.

Rock composed primarily of these minerals is called serpentinite. Serpentines find use in industry for a number of purposes, such as railway ballasts, building materials, and the asbestiform types find use as thermal and electrical insulation (chrysotile asbestos). The asbestos content can be released to the air when serpentine is excavated and if it is used as a road surface, forming a long term health hazard by breathing. Asbestos from serpentine can also appear at low levels in water supplies through normal weathering processes, but there is as yet no identified health hazard associated with use or ingestion. In its natural state, some forms of serpentine react with carbon dioxide and re-release oxygen into the atmosphere.

The more attractive and durable varieties (all of antigorite) are termed "noble" or "precious" serpentine and are used extensively as gems and in ornamental carvings. Often dyed, they may imitate jade. Misleading synonyms for this material include "Korean jade", "Suzhou jade", "Styrian jade", and "New jade". New Caledonian serpentine is particularly rich in nickel, and is the source of most of the world's nickel ore.

Soapstone

Steatite in its raw mineral formSoapstone (also known as steatite or soaprock) is a metamorphic rock, a talc-schist. It is largely composed of the mineral talc and is rich in magnesium. It is produced by dynamothermal metamorphism, which occurs at the areas where tectonic plates are subducted, changing rocks by heat and pressure, with influx of fluids, but without melting. It has been a medium for carving for thousands of years.  Colors - white, gray, greenish gray, pale green -- commonly discolored in reddish or brownish hues and mottled.

 

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[1] Some of the artifacts presented are held by commercial Private Collections.  While they lack their provenience or provenance, the visual representation has value for comparative purposes, and is presented for that reason.  Also, they are presented since these items may never be available in any other way for scholarly study.

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