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The
temple I frequent is high,
A turquoise-vaulted dome - the sky,
That spans the world with majesty
--Omar
Khayyam
Turquoise
is one of the oldest known gem materials
The
name “Turquoise” may have come from the word Turquie,
French for Turkey, because of the early belief that the mineral
came from that country (the turquoise most likely came from the
Alimersai Mountains in Persia (now Iran) or the Sinai Peninsula
in Egypt, two of the world's oldest known turquoise mining areas.)
Another possibility could be the name came from the French description
of the gemstone, "pierre turquin" meaning dark blue stone.
For
thousands of years the finest and most intense blue turquoise in
the world was found in Persia, and the term "Persian Turquoise"
became synonymous with the finest quality. The ancients preferred
blue because a gem-grade blue stone would not change color (King
Tut's treasures include a substantial amount of this type of blue
turquoise and the colour appears unchanged today.The mines of Nishapur,
in northeastern Iran, described in 1300 AD as having belonged to
Isaac, the son of Abraham, supplied turquoise to Europe and Western
Asia for centuries.
This changed during the late 1800's and early 1900's when modern
miners discovered or rediscovered significant deposits of high-quality
turquoise in the western and southwestern United States. Material
from many of these deposits was just as fine as the finest from
Persia Today, the term "Persian Turquoise" is more often
a definition of quality, rather than a statement of origin.
Exactly when turquoise first came to the attention of man is unknown.
We have archeological as well as literary references that pre date
the Christian era by five millennia. The four bracelets of Queen
Zar, found on her mummified arm, date to the second ruler of the
Egypt's First Dynasty, approximately 5500 BC. Turquoise was used
for beads by the Egyptians. Combined with other ornamental stones,
the turquoise was inlaid in gold by Sumerians and Egyptians to produce
very sophisticated articles of Jewelry.
Large mines were reported around 3,200 BC in the Sinai. The oldest
known source of turquoise is the Maghara Wadi mines in the Sinai
Peninsula. Mining expeditions of up to several thousand laborers
were sent there annually. These mines were worked for the pharaohs
for 2000 years. They, were rediscovered in the mid-nineteenth century
and worked on and off until the beginning of this century.
Turquoise was worn by Pharaohs and Aztec Kings. Its prized blue
color is so distinctive that its name is used to describe any color
that resembles it. Pre-Columbian Indians in Mexico, as well the
American Southwest, used turquoise for beads and pendants.
The Anasazi and Hohokam mined turquoise throughout our Southwest.
Absolute evidence exists that these prehistoric people mined turquoise
at both Cerillos and in the Burro Mountains of New Mexico; also,
at Kingman and Morenci in Arizona as well as the Conejos areas of
Colorado. Turquoise was a popular trade item. We know this because
so much has been found in archeological sites, many hundreds of
miles away from its source. A prime example is the Cerillos, New
Mexico, turquoise found in the Aztec regions of central Mexico.
The
Magic and History of Turquoise
Although
not specifically mentioned in the Bible, many scholars believe that
the robe worn by the high priest Aaron was adorned with turquoise.
Aristotle, Pliny and others refer to stones that must have been
turquoise. After the fourth or fifth century AD, many writings appeared
discussing the stone. Explorers such as Marco Polo took time to
write about it.
Turquoise became a major trade and barter item for the early Persians.
Persian turquoise was found in ancient graves in Turkistan, and
in the first to third century AD, in graves throughout the Caucasus.
Persian stones were much coveted in Afghanistan, and as far north
as Siberia.
Jewelry containing turquoise has always been popular in Tibet, where
it was highly revered, perhaps considered more valuable than gold.
They had their own source of turquoise, usually with a green cast;
a very hard stone often with a significant amounts of spider webbing.
It would be fair to say that every Tibetan wore or carried a piece
of turquoise throughout life. Turquoise was also used for currency
in many areas of Tibet.
The history of turquoise in China dates to the thirteenth century
AD. Although mining did exist, most stone came from trade with the
Persians, Turks, Tibetans, and the Mongols. Much Chinese turquoise
was used for carving and in other decorative ways. The Chinese are
greatly fascinated by turquoise, and to them it is second only to
jade. Turquoise was unknown until the 18th Century in Japan.
Turquoise was not of great import in early and medieval Europe.
However, as Asian conquests and interactions with Europe occurred,
seventeenth century Englishmen traveling there brought the style
back with them. However, it was not until Victorian time that it
became fashionable for European women to wear the stone. Victorian
and Art Nouveau jewelry featured a good deal of turquoise.
As turquoise found its way into the mystic arts, ancient doctors
exploited the stone's medicinal potentials, which varied from land
to land and age to age. It was good for nearly every ailment including
insanity. Turquoise is considered beneficial to general physical
well-being, and its cooling nature is thought to help high blood
pressure as well as to purify the blood and benefit the liver. Its
colour could forecast good or bad, predict the weather and influence
dreams. It was thought to prevent injury through accident and prevent
blindness by placing perfect stones over the eyes. Egyptians mounted
turquoise in silver to treat eyes suffering from cataract. It was
ground into a salve or powder, and was rubbed on or ingested to
cure stomach disorders, internal bleeding and ailments of the hip.
It was even said to be used for snake bites and scorpions stings.
As a good luck talisman turquoise found usage in nearly every culture.
Turquoise has been believed to confer foresight as well as protect
the wearer from danger. In various countries, it is believed to
fade when illness or danger is near. Another belief is that a fading
stone indicates a lover's faithlessness or a friend's disaffection.
In many cultures, the stone is regarded as a harbinger of good fortune,
success and health. Aztecs and Egyptians considered it a symbol
of prosperity. In India, one was to wear a turquoise on the little
finger and look at the stone after seeing the new moon to gain great
wealth. Since the fourteenth century, harnesses of dogs, horses
and other animals have been decorated with turquoise to protect
the animal and master from falling injuries.
Turquoise
Use in the Native American World
Certainly the prehistoric peoples of the Western hemisphere knew
of turquoise. Turquoise was likely found and used by early man.
A long time ago someone noticed a clear blue line running through
gray rock, and saw the imagery of sky and water in stone, and from
that time on, turquoise has been cherished above all else in creation.
Pieces of turquoise have been found in burial and archeological
sites throughout the two continents. It seems clear that turquoise
was always considered a stone of life and good fortune and that
it even had healing properties. The stone was used in religion,
art, trade, treaty negotiations as well as for jewelry. It was considered
by some tribes to be associated with life itself.
There are legends saying that the People danced and rejoiced when
the rains came. Their tears of joy mixed with the rain and seeped
into Mother Earth to become the SkyStone. Turquoise, the "fallen
sky stone" hidden in Mother Earth, has been valued by cultures
for its beauty and reputed spiritual and life-giving qualities for
all of history. It is a true gem of the centuries.
Other stories say that the stone brought together the spirits of
sea and sky to bless warriors and hunters, and that a turquoise
arrowhead assured accurate aim. It was also said that fine turquoise
was hidden in the damp ground at the end of the rainbow. A Navajo
belief is that a piece of turquoise cast into a river, accompanied
by a prayer to the god of rain, will cause rainfall.
Another example of the native American view of the power of turquoise
would be if you are wearing a turquoise ring and suddenly you look
down and see a crack in your stone; the Indians would say "the
stone took it," meaning the stone took the blow that may have
been aimed toward you.
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Physical
Properties of Turquoise CuAl6 [(OH)2/PO4]4
Most specimens are cryptocrystalline, meaning that the crystals
can only be seen by a microscope In chemical terms, turquoise is
a hydrated phosphate of copper and aluminum, and is formed as water
trickles through a host stone for about 30 million years, gradually
leaving a deposit. Turquoise is usually found in the "alteration
zones" of arid or desert regions. These zones are areas where
the native, original rocks have been altered through the intrusion
of other rocks from some volcanic or other thermal influence. The
hydrothermal alteration is created by magma solutions from deep
in the earth being forced to the surface through fractures or pores
which eventually change the original rocks.
Several steps and processes are necessary to create turquoise. First
there must be a source of copper. This occurs in a rather limited
number of areas in the world. There must be a source of phosphorus
CO-located with the copper, usually from the mineral Apatite, which
is not always in rocks associated with copper.
There must also be feldspar for the aluminum, along with deep hydrothermal
alteration, which breaks down the feldspars and frees the aluminum
needed for the turquoise. The phosphorus usually comes from phosphoric
acid leached from the Apatite, during the hydrothermal alteration.
The copper is usually introduced into the "host" rocks
by the rising hot magma. The copper readily oxidizes near the surface
when it is in the hot magma solution. It reacts freely with the
aluminum and phosphoric acid to form turquoise. Another key geological
activity is called silicafication; it too is an act of hydrothermal
and intrusive alteration. Here silica, which is a common associate
of turquoise, is introduced into the turquoise deposit. This addition
combined with periods of intense heat are responsible for the hardness
of the turquoise and frequently the matrix as well.
At this time other minerals enter into the turquoise structure and
create color variations. The chemical formula of turquoise is: (CuAl6
(PO4)8 4H2O) this structure will vary greatly with the introduction
of Iron, Calcium, Magnesium, Manganese, Silicon, and Zinc. These
additional elements when incorporated in the molecular structure
of turquoise influence its color and hardness. The color of turquoise
can vary from a deep blue to a deep green, with every variation
of color in-between. Generally, the more copper in the molecular
structure the bluer the turquoise. The introduction of iron causes
a greener cast to the stone.
To explain further, turquoise must consist of copper, aluminum and
phosphorus. Other elements can replace various percentages of these
and change the molecular structure. For example, two very rare minerals,
Chalcasiderite (where iron replaces the aluminum, creating a yellow-green
color), and Faustite (where zinc replaces the aluminum, creating
a lime yellow-green color), do exist in turquoise environments.
Usually there will only be a partial replacement of the aluminum
with iron and zinc, thus leaving the turquoise altered only in color.
Turquoise is opaque and has a Mohs scale hardness that varies greatly.
The deeply mined chalk-like turquoise may only have a mohs hardness
slightly over 2, while a gem specimen mined closer to the surface
may be up to 6. The hardness varies due to several factors, including
both the environment and the matrix or host rock in which
the turquoise is found.
In silica varieties of turquoise, quartz particles are present and
the stone will be hard enough for use as a gem stone. Silicafication
will strengthen some of the matrix as well. If some extent of silicification
has not occurred, the turquoise will likely be chalky, porous, and
soft. It will not be usable in jewelry without undergoing some form
of treatment to harden or stabilize the stone. Stabilization may
also be used because moisture will cause turquoise to turn toward
green This can occur in the ground or in jewelry by absorbing moisture
and oils. This is not unlike blue azurite changing to green malachite
as its creation environment increases its water content.
Turquoise can be formed in many ways. It can appear as nuggets or
it can be deposited in cracks in rocks, which then form vein turquoise.
Turquoise can be formed in a cavity lined with quartz crystals and,
most interesting, can take the place of another crystal when that
crystal dissolves and become a "pseudo morph"
or false form. This could give the impression that it is an actual
turquoise crystal. Since turquoise is a mineral that is deposited
by water solutions, turquoise can take the shape of cavities left
when the stems and parts of fossil plants were dissolved out of
harder rock or matrix, leaving turquoise in its place. Although
this is sometimes referred to as "Fossil" turquoise,
the term is incorrect, since "fossil" means the
actual remains of plants or animals preserved in the rocks of the
earth's crust.
If
you believe, as Native Americans believe, that the earth is alive,
then all things, no matter how small or apparently inanimate, are
precious. To the Native American, Turquoise is Life. In the modern
age, there is still this primal recognition of life-giving rock:
the smooth stones that lie in streams, the clear quartz that juts
from limestone, the humble stone found on a walk, the little black
pebble lying mysteriously on the path to your door. There are stones
medicine men keep in their sacred bundles because they possess powers
of healing. There is the stone that comes to you in dreams and the
magic ring you wear on your finger. These rocks and stones are alive
and give forth energy to those who wear and hold them. Stones and
crystals have unique attributes that support and heal us. Turquoise,
especially, is known for its positive healing energy, an aid in
mental functions, communication and expression and as a protector...
Here
in the United States, turquoise is synonymous with the Southwest.
In streets, plazas and in the middle of the desert; over plain dresses,
velvet blouses, satin skirts, cowboy shirts and ceremonial costumes,
Anglos as well as Pueblo and Navajo Indians wear turquoise necklaces,
turquoise pendant, turquoise bracelets, belts and pins and as much
as they can at one time. Elsewhere, turquoise may come and go with
fashion. Here turquoise is more precious than gold, an enduring
expression of Native American culture. It is the birthstone of December
and signifies success. All pictures on this page are of untreated,
beautiful, Natural Turquoise.
Turquoise,
once a luxury intended only for the noble, is worn by every native
of the Southwest as a sign of relative wealth. The rain gods and
the kachinas wear it. The Earth Mother herself was once a little
figure made of turquoise, before Talking God brought Changing Woman
to life.
Today, turquoise can be found in many countries of the world, but
high-grade turquoise is found mostly in China, Tibet, Persia and
the Southwest.
The
name is derived from "Turkish Stone" because it was brought
to Europe through the ancient trade route, via Turkey. Pure blue
is rare; with most stones either a blue-green hue or else containing
matrix. Deposits are found in Iran, China, Australia, Israel and
the southwest United States. The deposits in the Sinai were already
worked out by 4000 BC. At that time turquoise was used for jewelry,
amulets and the preparation of cosmetics by the Egyptians.
Considered
precious by the Native Americans, turquoise evokes peace of the
soul, as when we gaze at the immensity of the sky. By gazing at
turquoise the same way, we eventually feel a peace that surpasses
all analysis. Turquoise amplifies light blue and blue/green rays
in the Divine Light spectrum. When handled or worn, turquoise often
turns a darker green, which is said to be caused by the absorption
of lotions and body oils.
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Since the late 1950’s, there has been a larger demand for
turquoise than there has been supply. Since supply has not been
able to satisfy the demand, there have been many market-oriented
business people (sometimes unscrupulous), who have tried to fill
this void with alternate products. The range of turquoise treatments
is huge. Soaking soft, light colored turquoise soaked in a liquid
plastic creates the effect of a much higher quality material. This
idea was not new as it was done with animal fat and tallow thousands
of years ago. Another technique is achieved by grinding soft turquoise
into a powder and then compressing it, later adding various resins
and sometimes dye, to create a “reconstituted” block
of turquoise.
The
various possibilities are numerous and I will try to make some sense
of them for you. The words treated and stabilized are similar, but
not necessarily synonymous. They describe the same type process,
and there are several, for impregnating soft porous turquoise with
liquid plastic and hardening or stabilizing it. One of the newer
processes being used today is called 'enhancing'. This process creates
a slurry, and then charges the turquoise with electrical energy,
intensifying its hardness and color. The actual chemical structure
does not change, as opposed to stabilizing with plastic. Most of
these processes are well-guarded secrets, so any description is,
at best, only an educated opinion.
The treating of turquoise is not to be condemned and it is not wrong
to buy or sell it; but it is wrong to misrepresent it or to mislead
people. It should be sold as treated or stabilized and should not
hold the status and value of Natural Gem Turquoise, which is the
true gemstone. In my opinion 98% of all turquoise mined is stabilized
or enhanced in some way. This is generally the turquoise that is
softer, porous and chalky and will not hold together by itself.
Treating the stone in this way makes it darker and harder, less
likely to fall apart or crack when worked.
To complicate the subject even further, there is high-quality turquoise
that is stabilized due to the seam-structure in the stone that might
fracture if not treated. This material is often treated with “opticon”,
a kind of super glue used as a fracture-seal, just before cutting,
in an effort to hold the matrix together. It is getting more difficult
for even gemologists and turquoise experts to tell the difference
between some forms of treated turquoise as opposed to the natural.
Here are a few terms and their definitions that may help in understanding
the various processes:
NATURAL
TURQUOISE means a stone with no alteration to its original state.
Such stones are merely polished and cut into shapes before being
made into jewelry. Natural turquoise remains porous, as all natural
stone is to varying degrees, and may tend to change color over time
as it is worn and handled, absorbing ones natural body oils.
STABILIZED
TURQUOISE means that the natural material as it comes from the ground
has been chemically altered to harden the stone, usually by infusing
an epoxy or similar chemical into the porous surface of the stone.
The stabilization process serves to maintain or sometimes darken
the color of the stone so it will not change. Generally the color
remains natural in this process.
COLOR
TREATED TURQUOISE means that the natural material, as it comes from
the ground, is usually too soft and pale to be of any commercial
use. It is then altered in similar ways as the stabilized product,
but a blue dye is also added to the mix. Treated turquoise is best
recognized by its transparent plastic appearance. It looks unnatural
because it looks too blue and too highly polished.
RECONSTITUTED
TURQUOISE is the name used for turquoise dust and chips that are
mixed with plastic resins and dye and compressed into a solid block
so as to resemble natural turquoise.
SIMULATED
or IMITATION TURQUOISE is not really turquoise. This material is
pure plastic which has been colored with blue dye. It contains absolutely
no actual turquoise whatsoever. Pieces of rocks, sand, pyrite and
black dye are often added to the formula to imitate matrix.
Sources
and references
Turquoise, The Gem of the Centuries, by Oscar T. Branson, Treasure
Chest Publications
Bob Jones, Senior Editor, Rock & Gem Magazine, Turquoise, Blue
Sky...Blue Stone"
The Turquoise Trail, by Carol Karasik, Harry N. Abrams Publisher
Arizona Highways, January 1974
Silver Sun, 656 Canyon Road,Santa Fe, New Mexico 87501, www.silversun-sf.com
The
natural turquoise used in many of the pieces we offer on this website represents
less than 1 percent of the all the turquoise mined. If we state
that the turquoise is untreated and Natural, we will guarantee it.
We generally buy our turquoise either from the miner in rough rough stones
or cut cabs, or else we cut our own stones from our extensive personal
collection of turquoise. In most cases we design our jewelry our jewelry and then give the stones to one of the many Native American artists who work with us, to execute the design. That way we can guarantee the quality
and authenticity of our jewelry and stones. The best guarantee to
the buyer as to the authenticity of a piece and the stones that
are set in it is to deal with a reputable dealer that you can trust.
After over 40 years as an Indian Trader, and being fortunate to live
and work in Santa Fe, the 'heart of the Indian Jewelry business',
we have access to the sources that enable us to offer such quality
items. Native
American artisans may buy turquoise cabochons directly from miners,
but most buy from jewelry supply stores or trading posts.
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The Ajax mine, a small mine located in south central Nevada in the
Royston area, is one of the relatively new turquoise mines. The
mine yields stones from light blue with darker blue veins to predominately
dark green with light blue areas. This latter coloration is considered
quite unusual for turquoise.
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“Bisbee
Blue” is a name that originates from the Bisbee Mine,
near Bisbee, Arizona, in Cochise County, USA. The term refers to
the turquoise that comes from copper mines in this region. Turquoise
from Bisbee has a reputation as a hard, finely webbed stone with
high blue color, ranging from sky blue to a dark lavender blue.
The matrix patterns vary a great deal, but can be characterized
by the deep chocolate brown to black webbing. The hardness is 4.5
on the mohs scale.
The
name “Bisbee” conjures a mystique among all turquoise
aficionados, and it is one of the most sought after of all domestic
turquoise. The turquoise from Bisbee is highly collectible and it
is one of the more famous of the American mines. Although the turquoise
from Bisbee has a wide variety of color and hardness, the most exceptional
quality originates from the Lavender Pit, especially the east side.
Such stone has beautiful high blue color with a dark distinct matrix.
The turquoise is found as stringers that form as much as a few inches
wide, as well as minute stringers in pyrite; also, small nugget
masses in granite and quartzite.
Bisbee
turquoise was one of the first to appear on the modern American
market, which is at least partly responsible for its fame. The turquoise
mine was a secondary operation to the Bisbee copper mine, operated
by the Phelps Dodge Corporation. The vast majority of Bisbee turquoise
surfaced when the Phelps Dodge started their open pit mining operations
at the location now known as the Lavender Pit.The mine has been
closed since the early 1970's, so anything new coming from the mine
has been scavenged from the old dumps.
Much
conglomerate rock had to be removed by Phelps Dodge before the deeper
copper ore could be mined. This conglomerate was considered waste
rock to the mining company, but was actually a hidden treasure as
the host rock for Bisbee turquoise. This waste was discarded in
huge piles called "dumps." The corporation made no decided
effort to recover the turquoise, so almost all of it was recovered
by company employees taking it out covertly in lunch boxes.Though
this activity was prohibited, it was rarely enforced. For several
years, through the late 1970’s, these individuals (locally
known as "dumpers"), were the only source for this fine
turquoise. Also, during this time, Phelps Dodge began leasing out
rights to individuals to mine the dumps for turquoise. However,
the large majority of Bisbee turquoise was extracted during the
1950’s and 1960’s through the covert actions of mine
employees.
There
are other very rare materials from Bisbee that were mined both from
stream beds in the Mule Mountains, as well as from the Campbell
shaft. The various lesser known formations, other than turquoise,
among the copper oxides of Bisbee are of interest, as they rarely
form in a similar way anywhere else in the world. There is a conglomerate
mix of Azurite, chatoyant malachite, chrysacola and cuprite…all
in a single stone, coming from the Campbell Pit, that is incredibly
understated and altogether unrecognized for its uniqueness.
Sources:
Turquoise, The Gem of the Centuries, by Oscar T. Branson, Treasure
Chest Publications
Bob Jones, Senior Editor, Rock & Gem Magazine, Turquoise, Blue
Sky...Blue Stone"
The Turquoise Trail, by Carol Karasik, Harry N. Abrams Publisher
Arizona Highways, January 1974
Silver Sun, 656 Canyon Road, ,Santa Fe, New Mexico 87501, www.silversun-sf.
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The Blue Diamond Mine, south of Austin, Nevada produces a very hard
light to deep blue turquoise, with an attractive swirl or mottled
pattern of light and dark blues. It has brown to black matrix. The
mine is located at a high altitude and cannot be mined in the winter
months due to the extreme cold and snow.
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The Blue Gem Lease mine has been staked also as the Turquoise Tunnel
and the Contention, and at one time it was on the Pedro Lode claim
belonging to the Copper Canyon Mining Company. The Blue Gem mine
is in the SE 1/4 of Section 29, T. 32 N., R. 44 E., about 4,000
feet north - northeast of Copper Basin. It is surrounded by the
copper workings of the Copper Canyon Mining Co. The parent company
is the Duval Corporation.
Blue
Gem turquoise occurs in argillized quartz monzonite cut by two limonite-stained
sheer zones, one trending N. 35 o W. and dipping 75 o NE., the other
trending N, 25 o E. and dipping 55 o NW. An extensive breccia zone
about 10 feet wide is developed between the two bounding sheers.
Exceptionally good quality turquoise forms veinlets up to three-quarters
of an inch thick along the shears. Pyrite-bearing quartz veins are
closely associated with the turquoise.
The
Blue Gem mine was at one time located deep underground, accessed
by tunnels as deep as 800 feet. This is of interest because the
Blue Gem Mine and the Bisbee Mine in Arizona are the only two mines
(of which we are aware) that turquoise was found that deep in the
earth. The Blue Gem mine was once developed in extensive underground
workings. An adit several hundred feet long on the main structure
connected to numerous shorter tunnels and several open stopes. Directly
above the main adit was a glory hole some 100 feet long.
The
Blue Gem deposit was first noted by Duke Goff in 1934. It was subsequently
leased from the Copper Canyon Mining Co. by the American Gem Co.
of San Gabriel, CA., owned by Doc Wilson and his sons, Del and William.
The company operated the property until 1941 when the outbreak of
the war caused a shortage of experienced miners. When both Del and
William Wilson were called into the Army, the mine was closed for
the duration of the war. Consequently, the lease was allowed to
lapse and work was abandoned. In 1950 the mine was leased by Lee
Hand and Alvin Layton of Battle Mountain.
In
the early days of the operation, production of turquoise at the
Blue Gem Lease was enormous. Although there is no exact information,
it is reported that the output amounted to nearly $1 million in
rough turquoise. The mine is still active, although it is currently
in the center of a major copper deposit being developed by Duval
Corp.
Pyrite
in Blue Gem is unusual to see but not unheard of. Very little large
material ever came out of Blue Gem. The majority found was small
1-3 mm "bleeder" veins, which often came in sheets measuring
2 inches x 2 inches, as well as tiny nuggets which was perfect for
Zuni inlay and fine needlepoint, petit-point and snake-eyes jewelry.
Blue Gem turquoise was very popular in the late 1930's and 40's
and was commonly used in the Fred Harvey "railroad and tourist
jewelry" that is so collectable today. Blue Gem turquoise is
extremely hard and stands up well to the test of time.
Blue
Gem turquoise is a rare, valuable and historic American treasure.
Quality Blue Gem Turquoise has been gifted with a wide range and
variety of color, from a beautiful sky blue to an aqua blue-green,
not unlike parts of the Mediterranean Sea. Because Blue Gem turquoise
is very hard, a high polish is associated with this stone, and unlike
most turquoise, it won't easily change color. This turquoise has
a unique character and many different looks all of which are striking,
full of wonder and pleasing to the eye.
Production
of the mine started about 1934 and continued into the 1970's. Blue
Gem Turquoise is still some of the finest turquoise ever found,
and unlike most turquoise mines, (in which the majority mined is
chalky and only usable if stabilized) most of the turquoise found
there was of gem-quality. Today the Blue Gem mine can no longer
be worked, as it sits in the middle of a huge mining operation.
The emphasis is on precious metals; the extraction of turquoise
is considered more of a hindrance in the mining process than an
asset. Even the ever popular "Dump Diving" for turquoise
is not tolerated due to the very real danger of becoming buried
in a slide. Insurance factors, equipment hazards, high explosives
and safety issues, along with a lack of interest from the mining
company, keep Blue Gem turquoise unavailable to the world, at least
for now.
The
original Battle Mountain blue Gem Mine no longer produces turquoise,
although numerous other mines in the area now carry the same name.
The only true old Blue Gem turquoise available today is through
old collections.
Sources:
Turquoise, The Gem of the Centuries, by Oscar T. Branson, Treasure
Chest Publications
Bob Jones, Senior Editor, Rock & Gem Magazine, Turquoise, Blue
Sky...Blue Stone"
The Turquoise Trail, by Carol Karasik, Harry N. Abrams Publisher
Arizona Highways, January 1974
Silver Sun, 656 Canyon Road, ,Santa Fe, New Mexico 87501, www.silversun-sf.
Return
To Table Of Contents
Carico
Lake turquoise is named after the location of its mine, located
on a dried up lake bed in a high, cool area of Lander County, Nevada.
It’s clear, iridescent, spring green color is due to its zinc
content and is highly unique and collectible. Carico Lake turquoise
is also found in a dark blue as well as a blue-green color with
a black, spider web matrix. The Carico Lake mine is primarily a
gold producing mine. However, from time to time, the mining company
leases the turquoise producing part of the mine to individual miners
who are permitted to work that part. The limited amount of time
allowed to mine Carico Lake turquoise and the limited amount of
turquoise yielded, combine to make Carico Lake turquoise a valuable
addition to one's collection.
Sources:
Turquoise, The Gem of the Centuries, by Oscar T. Branson, Treasure
Chest Publications
Bob Jones, Senior Editor, Rock & Gem Magazine, Turquoise, Blue
Sky...Blue Stone"
The Turquoise Trail, by Carol Karasik, Harry N. Abrams Publisher
Arizona Highways, January 1974
Silver Sun, 656 Canyon Road, ,Santa Fe, New Mexico 87501, www.silversun-sf.
Return
To Table Of Contents
Turquoise
from the Cerrillos district is not only an uncommon and unique form
of native New Mexican turquoise, but also has a long history which
is deeply entwined with both the ancient native peoples of the Southwest
and the more recent American mining companies. Considered the oldest
known source for turquoise in America, the Pueblo peoples continued
to extract turquoise from the Cerrillos mine until the 1870's when
a silver mining boom raised interest in the area. The Tiffany Company
in New York and its associates bought up the mine area and extracted
$2,000,000 worth of turquoise between 1892 and 1899, the per carat
value of which has never again been attained.
Cerrillos
turquoise was created and mined under unusual circumstances, as
it is the only turquoise that has been known to form at the base
of a volcano. Thus, a variety of colors developed from the minerals
in the various volcanic host stones. Cerillos turquoise thus offers
a huge range of different colors, from tan and khaki-green to a
rich, blue-green to a multitude of blues and even white. Cerrillos
is a very hard stone and so takes a brilliant polish. Much of the
host rock is riolite.
In
addition to producing distinctive colored stones, the Cerrillos
mines are considered the oldest mines of any kind in North America.
Located ten miles south of Santa Fe, it was the site of the largest
prehistoric mining activity on the continent because the huge turquoise
deposit was partially exposed at the surface. Miners from the San
Marcos Pueblo, who later moved to Santo Domingo Pueblo south of
Santa Fe, most heavily worked the mine. Using only stone axes, mauls,
antler picks, and chisels, Pueblo miners removed 100,000 tons of
solid rock to create a pit mine 200 feet deep. They dug other vertical
shafts into the ground to reach veins of turquoise. Miners carried
tools and leather rock buckets on their backs as they climbed in
and out of the shafts using notched logs as ladders.
The
turquoise obtained from the workings at Cerillos was traded via
the old trade route, first to workshops at Chaco Canyon, New Mexico,
where artisans polished stones that were coveted by nobles of distant
lands. Turquoise from these workshops has been found as far south
as Oaxaca, Mexico. The kings and emperors of the Mixtec and Aztecs
wore crowns and pendants of turquoise, as amulets of good fortune
and long life. The material was also traded east to Pecos and on
to the land of the mound builders. Indisputable proof of the movement
of this turquoise exists through laboratory analysis of turquoise
found in many different geographic locations. Vast numbers of pieces
of Cerrillos turquoise for personal and trade use have been unearthed
in the prehistoric ruins of Pueblo Bonito in Chaco Canyon, as well
as in Aztec ruins after the Spanish conquest.
The
mine is currently owned by Douglas Magnus, Santa Fe painter and
jeweler extraordinaire, who has made a lifelong project of preserving
and protecting what little of this material still exists. I have
spent many hours digging around in the dumps of the old Castilian
claim and remember every piece I was lucky enough to find. In fact
I once staked the claim next to the Castilian, the Spanish Gem,
where I never found a single piece of turquoise. Rarely does this
material come on the market, as it is coveted by those fortunate
enough to possess it.
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Cripple
Creek turquoise comes from the Cripple Creek mining area, located
in Teller County Colorado, near the town of Cripple Creek. This
is a very hard stone with colour range from light and dark blues
with brown matrix, and more rarely a golden limonite matrix to blue-green.
Hardness can be up to 6 mohs. The best use over all is for inlay
and cabbing, although the medium quality is often a little pithy
or porous, the result of which does not become visible until the
end of the polishing process. This turquoise, like Carico Lake turquoise,
is found as a by product of gold mining. This stone is found as
both vein material and nodules.
This
history of Cripple Creek Turquoise is quite interesting. One of
the last great Colorado bonanza camps, the district was first discovered
in 1891 by cowboy Bob Womack and turned out to be one of the richest
gold mining camps in US history. The 500 mines in the area have
yielded over 600 metric tons of gold, making it the third most productive
gold district in the history of the United States
Cripple
Creek is unusual in that it is one of only a few domestic Turquoise
mines still active today, although production has been limited.
There are currently two active turquoise mines in the area being
operated by two different families. The area is also quite mineral
rich; along with gold and turquoise, over 120 other mineral species
have been found.
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The
Damale mine is a small, tightly run operation, located thirty miles
from Austin, Nevada. The mine is located on The Dry Creek Ranch
owned by the Damale family. There, they raise unique horses that
carry the Damale name. Benny Damele discovered the mine sometime
around 1973. Soon thereafter, Clyde Wright became involved in mining
the claim and worked it for approximately 18 years. Tony Cotner,
a shrewd merchandiser and colorful character, has owned the claim
since 1990 when he bought it from Benny Damele. Cotner, also known
as "Mean Green", states there is an ancient subtropical
zone located beneath the mine that may be responsible for the unusual
colors associated with Damele turquoise although he is unsure whether
the organic environment has anything to do with the coloration.
Damale
is a well known mine, distinctive because it is one of the few turquoises
that can be truly yellow-green, either from iron or environmental
conditions, but without zinc. Turquoise from the Damale mine is
wonderfully distinctive; very hard, and visually appealing. It forms
in veins and occasionally as nuggets in carbonaceous chert and also
diatomaceous earth.
The
mine is extraordinarily versatile, it’s colors ranging from
pure lime-green through bright chartreuse; it can also be yellow
with black webbing, or white, orange and brown, or even a caramel
color with bright green polka dots. The mine also produces small
black nuggets with bright yellow-green bumps poking out of the black
matrix. Its availability is extremely limited because the mine is
small and difficult to work. Due both to its limited quantity as
well as its rare color and quality, turquoise from the Damale is
an exceedingly collectible turquoise.
Sources:
Turquoise, The Gem of the Centuries, by Oscar T. Branson, Treasure
Chest Publications
Bob Jones, Senior Editor, Rock & Gem Magazine, Turquoise, Blue
Sky...Blue Stone"
The Turquoise Trail, by Carol Karasik, Harry N. Abrams Publisher
Arizona Highways, January 1974
Silver Sun, 656 Canyon Road, ,Santa Fe, New Mexico 87501, www.silversun-sf.
Return
To Table Of Contents
The
Dry Creek turquoise mine is located on the Shoshone Indian Reservation
near Battle Mountain, Nevada. The mine was first discovered in 1993,
but the nature of the material led to much confusion, due both to
its extreme hardness and odd color. After having the material assayed,
it was proven to be turquoise. The miners at Dry Creek have also
found a white stone at this deposit that is mistaken as “white
turquoise”, but is actually Aluminite.
The
turquoise from the Dry Creek mine, which has also been known as
the Godber as well as the Burnham mine, is a creamy pastel-blue
and blue-white turquoise. The gem grade material from this mine
is very hard and available only in small quantities. Since turquoise
gets its pigment from the heavy metals in the ground where it is
formed, and this area has a distinct lack of heavy metals, the odd
color is due to a slightly heavier balance of aluminum rather than
copper in the stone's chemistry makeup. The matrix in Dry Creek
Turquoise is typically light golden or brown-gray to gray-black.
This turquoise is beautiful alone in a piece of jewelry and is especially
striking when juxtaposed with other colors of turquoise in a single
creation.
To
date, no other vein of this color turquoise has been discovered,
and when this current vein runs out, that will be the last of it.
Because this turquoise is as rare as the legendary sacred white
buffalo, the Indians call it “White Buffalo” Turquoise.
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The
origin of the Old Fox mine is near Lander County, Nevada. While
indigenous people found large nuggets in this area in prehistoric
times, the area was first discovered for contemporary mining purposes
in the early 1900’s. In the 1940's, Dowell Ward purchased
& developed the old Cortez claims. Turquoise from this mine
comes under several different names including Fox, White Horse,
Green Tree and Smith, to differentiate the different deposits and
colors and to create a larger perceived share of the turquoise market.
Color range is from a soft sky blues, sometimes with a subtle water-marked
matrix, to blue-green to green. While quite a bit of this material
came out in nugget form, there is also large seam material, sometimes
as thick as two inches. The colors in the seam material go to a
deeper green, sometimes in conjunction with a very nice blue. The
nugget material, while usually small, makes very nice cabs or can
be used for inlay. The seam material, often not of ultra high quality,
is better suited for carving and, with the better quality for cabbing.
Hardness is 4.5.
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Kingman
Turquoise originates in the Mineral Park Mining District near Kingman,
Arizona. One of the largest domestic turquoise mines, it is found
in a large open pit copper mine in the high desert country. The
Kingman Mine district was first mined by Native Americans; it was
part of the most extensive prehistoric workings in Arizona.
However,
modern production of turquoise dates back to the 1880's when James
Haas rediscovered the area. Natural Kingman Turquoise ranges in
color from light to very dark blue and sometimes tints of green.
Matrix can range from white, light brown to black and frequently
flecked with pyrite and occasionally quartz. The most famous stones
from this mine are rounded bright blue nuggets with black matrix.
Few turquoise mines produced nuggets, especially of this quality.
In its high-grade form it has always been considered among the top
quality American turquoise. This high blue color has become a “color
standard” in the industry, reflected by the name “Kingman
Blue”.
However, much of the turquoise from Kingman occurs as seams, masses
and veins, rather then in nugget form. Besides the nugget form,
the most desirable Kingman turquoise is a deep blue with molybdenum
pyrite; also, deep blue with pyrite as well as in a “bird's
eye” pattern with “water web” matrix.
The
mine is currently owned & Operated by the Colbaugh family’s
company, Colbaugh Processing. While old natural Kingman turquoise
is rare, they have recently gone back into older sections of the
Kingman mine and are bringing out some new natural Kingman Turquoise.
Although there are quantities of this fine natural deep blue turquoise
available, the largest percentage of turquoise mined at Kingman
is being treated or stabilized. There are several other names for
the turquoise coming out of the Kingman mining district: Ithaca
Peak, Old Man Mine, Kingman Duval, Courtland, The Wall and Turquoise
Mountain, just to mention a few.
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Lone
Mountain Turquoise
The
Lone Mountain turquoise mine near Tonopah, Nevada was one of the
leading producers of fine turquoise in Nevada. It was discovered
by Lee Hand in 1920 and filed under the name of Blue Jay Mining
Lode. At first it was called the Blue Jay Mine on Lone Mountain
and later just Lone Mountain. It is presently closed.
As
with most mines, it was at first a tunnel and shaft project but
when Menless Winfield bought the mine it was made an open pit operation.
The turquoise from this mine is mostly good to high-grade and usually
in the form of nuggets although there is a quantity of vein material.
A very interesting occurrence of turquoise found here is a condition
where the turquoise was deposited in cavities or molds left when
parts of fossil plants were dissolved out of a harder rock. The
turquoise is graded into golden matrix, black matrix and spider
web. At present, most of it is cut and polished or the nuggets drilled
and polished at the mine, making this is a very collectible turquoise,
and rarely available in rough form.
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Morenci
Turquoise is mined in southeastern Arizona, in Greenlee County.
It is light blue to high blue in color. Morenci has an unusual matrix
of irregular black pyrite, or fool’s gold; when polished,
the pyrite often looks like silver. It also is sometimes webbed
in a darker shade of blue, called water webbed. Morenci turquoise
is well known because it was one of the first American turquoises
to come on the modern market, and is often difficult to obtain because
the mine is now depleted, making it an exceedingly collectible turquoise.
Material
coming out in the 1960’s seems to be harder, tending more
to the blue-greens, usually with the pyrite. In the 1970’s,
the material was a much brighter blue, often with quartz along with
the pyrite.
Sources:
Turquoise, The Gem of the Centuries, by Oscar T. Branson, Treasure
Chest Publications
Bob Jones, Senior Editor, Rock & Gem Magazine, Turquoise, Blue
Sky...Blue Stone"
The Turquoise Trail, by Carol Karasik, Harry N. Abrams Publisher
Arizona Highways, January 1974
Silver Sun, 656 Canyon Road, ,Santa Fe, New Mexico 87501, www.silversun-sf.
Return
To Table Of Contents
Located
in the Lynn mining district (no. 19, pl. 1 ) in northern Eureka
County, north of Carlin, Nevada, the Number 8 mine is on the west
side of the Tuscarora Range in the NW 1/4 sec. 4, T. 35 N., R. 50
E., and was at one time a gold and copper mining operation. It was
in a large mining district encompassing ten 20-acre claims and was
active from the 1930’s through the early 1950’s. Host
rocks for the Number 8 deposit consist of intensely altered quartz
monzonite, shale, and thinly bedded black chert, which are complexly
folded, faulted, and much altered. Turquoise is concentrated along
quartz veins in the intrusive rock and along faults in the sedimentary
rocks.
The number 8 mine was presumably discovered about 1925 by a barber
from Carlin whose name has been forgotten, because he made no attempt
to mine the property. The mine was rediscovered by Earl Buffington
and Lawrence Springer in 1929. They filed formal claim to the property
and proceeded to mine turquoise in serious fashion, producing about
1,800 pounds of good stone the first year. In 1930 Ted Johnson bought
Buffington's interest and during the next four years produced about
5,000 pounds of commercial stone. In 1935 Doc Wilson bought the
number 8 mine from Johnson but did nothing with the property and
the claim lapsed. Myron Clark relocated the claim and, after working
it for awhile, sold it to Lee Hand. Hand operated the mine for a
short time, but became dissatisfied with the quality of the stone,
and sold it to the five Edgar brothers who now own it. The Edgars
extended operations and produced a considerable amount of fair-to-good
turquoise.
In
1950, as most of the visible turquoise had been taken from the workings,
the Edgars hired a contractor with bulldozer equipment to remove
overburden from another part of the claim. A deposit of copper had
been found on the property, and the Edgars thought they might mine
copper if they did not find more turquoise. The bulldozer, after
digging a pit about eight feet deep and 80 feet long, uncovered
a deposit of some of the finest spider-web turquoise ever found
in Nevada. The deposit was mostly in nodules, some of gigantic size.
One
of the largest pieces of turquoise and matrix in the modern world,
perhaps the largest nodule ever uncovered, was discovered at the
Number 8 mine on June 23, 1954, by T. G. Edgar, J. M. Edgar, and
Marvin Symes. This specimen was 33 inches long, 18.5 inches wide,
and seven inches thick. Cleaned and polished it weighed 150 pounds.
The nodule was of excellent texture, good color and hardness, and
ranked with any turquoise of good commercial grade. Another nodule,
of excellent quality, weighed more than nine pounds. It was sold
to C. G. Wallace, of Zuni, New Mexico, for $1,600. The discovery
proved to be a rather large-pocket and produced more than 1,600
pounds of the very highest grade turquoise before being worked out.
Spurred by this find, the Edgars further explored the property,
without finding any more spider-web turquoise of notable quantity.
Other turquoise was discovered, however, of good commercial grade,
sufficient to keep the mine in operation.
Of
the ten claims in this 20-acre area, the Number 8, first claimed
by the Blue Star Company in Lander County, is considered the finest
example of the gold-webbed turquoise.. The mine has produced one
of the most prized spider web turquoise deposits in the world. In
its prime, enormous nodules were found, including one that weighed
150 pounds. Number 8 turquoise is famous for its black, golden-red
and brown spider web matrix background, which is set off by the
soft blue to blue green turquoise. Only rarely does gem material
appear: a very dark blue turquoise with black spider web matrix.
The mine is now depleted and Number 8 turquoise is extremely rare
and valuable.
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Orvil
Jack discovered and developed the mine in the northern Nevada, known
as Crescent Valley, that bears his name. This claim is actually
made up of two mines: when the blue turquoise is mined, it is called
the "Blue Ridge Turquoise Mine." When the yellow-green
“faustiet”' is mined, it is referred to as "Orvil
Jack Turquoise." The rare yellow-green color of the turquoise
comes from the zinc content.
Mr.
Jack is now deceased, but his daughter Grace Jack Wintle continues
to manage and work the mine, although it is now operated primarily
as a gold mine. Only a very small amount of the yellow-green variety
is now being produced, and is considered very collectible due to
its rare color and scarcity.
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The
Pilot Mountain mine is located in northern Nevada. It is still producing
and is worked by one family. The stone is highly admired for its
deep blue-green colors. In addition, it can show light blue to dark
green colors on the same stone. This graduation in color is unusual
and makes the turquoise very collectible. The matrix is black to
golden brown. Although sometimes a little porous, or pithy, Pilot
Mountain is a hard stone and takes a good polish.
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Royston
is a district in Nevada consisting of three turquoise mines: Bunker
Hill, Oscar Wehrend, and the main producer, The Royal Blue. Royston
is known for its beautiful colors ranging from deep green to rich,
light blues which are set off by a heavy brown matrix. The Royston
mine is producing a little high grade turquoise today, operated
by the Ottison family. They process most of their material into
finished cabs and allow very little rough to come onto the market.
This controlled output has raised the price of this material considerably
in recent years.
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The
Sleeping Beauty, mine located in Globe, Arizona is an active mine
producing a wide range of turquoise that is highly prized for it's
solid soft blue color, with little or no matrix. The color of the
turquoise ranges from a deep royal blue to a light sky blue. The
mine originally was worked for copper and gold but during the last
four decades it has produced gemstone quality turquoise in quantities
to satisfy the commercial market. In general, the miners lease portions
of the “dumps” and sort turquoise from there.
There
is a small town in south central Italy, near Naples, famous for
its cameos. Their needs for huge quantities of this material over
the years have always kept the supply down and demand high. The
clear blue is reminiscent of old Persian turquoise, and is without
doubt the most preferred and prized by Europeans, both for cameos
as well as in bead or jewelry form.
There
is a sister mine nearby, called the Bluebird, that produces some
of the world’s most beautiful azurite. This material is a
copper oxide and also contains malachite, crysacolla as well as
a mineralized copper or cuprite. This is a rare and undervalued
gem stone that has all but disappeared from the marketplace.
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