Excerpts from ROCKTALK vol. 2 no. 3
Colorado Geological Survey
Diamonds
Diamonds are formed from pure carbon, one of the most abundant elements on planet
Earth. Diamonds, even from ancient times, have been sought for their extraordinary
hardness (they are the hardest substance known) and their brilliance, especially in the
colorless transparent gemstone variety. Ironically the other form of pure carbon is
graphite, which is very soft with a soapy feel and a dull gray color. Graphite is commonly
the "lead" in a pencil.
Mohs Hardness Scale of minerals starts at 1 (talc) and ranges to 10 (diamond). That does
not mean that diamonds are ten times harder than talc; mineral number 9 on the Mohs
scale is corundum, a class of minerals which includes rubies and sapphires. Diamonds
can be from ten to hundreds times harder than corundum. Diamonds themselves vary in
hardness; for example, stones from Australia are harder than those found in South Africa.
The four main optical characteristics of diamonds are transparency, luster, dispersion of
light, and color. In its pure carbon form, diamond is completely clear and transparent. As
in all natural substances, perfection is nearly impossible to find. Inclusions of other
minerals and elements cause varying degrees of opacity. The surface of a diamond can be
clouded by natural processes, such as the constant tumbling and scraping in the bed of a
river.
Luster is the general appearance of a crystal surface in reflected light. Luster of a smooth
crystal face of diamond is strong and brilliant. It is intermediate between glass and metal
and has its own special term--adamantine.
The process of white light breaking up into its constituent colors is called dispersion.
Diamonds have strong dispersion, which along with their strong luster, causes the
beautiful play of colors so often referred to as the "fire" of a diamond.
Gemstone varieties of diamond are usually clear and colorless, often containing minor
inclusions and imperfections. Yellow or yellowish-brown and even brilliant yellow
diamonds have been found. Very rarely, diamonds are blue, black, pale green, pink,
violet, and even reddish.
The most famous blue diamond, the Hope Diamond, is intertwined with Colorado's
mining history. Thomas Walsh, discoverer of the rich Camp Bird Mine near Ouray,
purchased the Hope Diamond for his wife in the early 1900s; it was later given to his
daughter, Evelyn Walsh McLean who wore it almost continuously until the 1940s. The
45.5-carat Hope Diamond now resides at the National Museum of Natural History in
Washington, D.C.
Diamonds, in their perfect cubic crystal form, occur as isolated octahedral (eight-sided)
crystals (see figure below). Many variations on the cubic form are found in nature,
including twelve-sided crystals and a flattened triangular shape known as a macle.
Gemologists recognize three main varieties of diamonds: ordinary, bort, and carbonado.
Excerpts from ROCKTALK vol. 2 no. 3
Colorado Geological Survey
Ordinary diamonds occur as crystals often with rounded faces, from colorless and free
from flaws ("the first water"*) to stones of variable color and full of flaws. Bort
diamonds occur in rounded forms without a good crystal structure. They are generally of
inferior quality as a gemstone. Carbonados are black opaque diamonds usually from the
Bahia Province of Brazil. They are crystalline but do not possess the mineral cleavage
found in ordinary diamonds.
* An expression which refers to the highest quality diamonds and has come to mean the
highest quality of just about anything.
Size comparison of octahedral diamond crystal
for 1 to 500 carats.
Excerpts from ROCKTALK vol. 2 no. 3
Colorado Geological Survey
Diamonds form in nature only under the extreme conditions found in the upper mantle at
depths of 150 to 200 kilometers (possibly down to 300 kilometers): pressures of greater
than 50 kilobars (50,000 x normal atmospheric pressure) and temperatures of 900 to
1,300øC and possibly higher. The diamonds form as minerals within rocks of the upper
mantle called eclogite and peridotite. Eclogite is a coarse-grained rock consisting of red
garnet (almandine-pyrope) and a green pyroxene (omphacite). Peridotite is believed to be
the most common rock of the upper mantle; it contains varying amounts of three
minerals, olivine, orthopyroxene and clinopyroxene. The olivine rich peridotite is called
dunite, and the pyroxene rich rock is called websterite. The rock harzburgite contains up
to 40 percent orthopyroxene and 60 to 90 percent olivine and is thought to be the most
common host rock for diamonds.
If diamonds are formed at depths of 150 to 200 kilometers in the upper mantle, how do
they get to the surface of the earth? They are brought to the surface in a peculiar igneous
rock called kimberlite (named after the diamond-bearing region of Kimberly, South
Africa where these rocks were first identified.) Kimberlites are intrusive bodies that
originate in the upper mantle and are injected upward through the upper mantle and the
lower and upper crust, eventually reaching the earth's surface as a small volcanic
complex (see figure on p. 3). Kimberlites have three facies correlative to their position in
the mantle and crust: the root facies, the diatreme facies, and the crater facies. The shape
of the kimberlite shown in the figure is similar to that of a carrot or a pipe; a
comparatively wide upper zone, up to several hundred meters in diameter, in the diatreme
and crater facies; to a lower zone, which narrows into a thin intrusive dike, possibly only
a meter thick, in the root facies. The forceful intrusion of the kimberlite brecciates* the
surrounding rocks of the upper mantle and crust and incorporates them as xenoliths
(xenolith literally means "foreign rock"). Often these xenoliths of the upper mantle
peridotites or eclogites contain diamonds.
* Means to break apart into smaller angular fragments. A rock composed of angular
fragments is referred to as a breccia.
Diamonds, being mostly pure carbon, are not amenable to modern methods of age-dating
rocks (Carbon 14 dating methods are useful with materials less than about 50,000 years.
Most rocks are millions to billions of years old. With recently developed age-dating
techniques, the small inclusions of other minerals in diamonds (such as garnet) can be
dated. Recent dating of inclusions in diamonds from kimberlite pipes, mainly in South
Africa and Australia, indicate that diamonds formed as early as 3,300 million years ago to
as late a 990 million years ago, an extended period of the earth's history. The kimberlite,
which carried the diamonds to the surface and is the present host rock, was intruded only
about 100 million years ago.
Kimberlites ascend rapidly to the earth's surface at rates thought to be on the order of 10
to 30 kilometers per hour. There is usually no evidence of any substantial thermal
reaction with the surrounding country rock. In the near surface environment, velocities
may increase to several hundreds of kilometers per hour because of gas expansion in the
Excerpts from ROCKTALK vol. 2 no. 3
Colorado Geological Survey
ascending magma and reaction with water. Craters, tuff rings, and maars form as the
highly charged kimberlite magma erupts at the surface.
Kimberlites, though rare, are widespread throughout the surface of the earth. Most well
known diamond producing pipes are small, 12 to 75 acres, and they generally occur in
clusters of six to forty pipes. Almost all diamond bearing kimberlites are found in the
ancient stable cratons of the continents, never in oceanic crust or in younger mountain
belts, like the Alps or the Sierra Nevada in California.
Diagram of an idealized kimberlite intrusion.
Colorado Geological Survey
Diamonds
Earth. Diamonds, even from ancient times, have been sought for their extraordinary
hardness (they are the hardest substance known) and their brilliance, especially in the
colorless transparent gemstone variety. Ironically the other form of pure carbon is
graphite, which is very soft with a soapy feel and a dull gray color. Graphite is commonly
the "lead" in a pencil.
Mohs Hardness Scale of minerals starts at 1 (talc) and ranges to 10 (diamond). That does
not mean that diamonds are ten times harder than talc; mineral number 9 on the Mohs
scale is corundum, a class of minerals which includes rubies and sapphires. Diamonds
can be from ten to hundreds times harder than corundum. Diamonds themselves vary in
hardness; for example, stones from Australia are harder than those found in South Africa.
The four main optical characteristics of diamonds are transparency, luster, dispersion of
light, and color. In its pure carbon form, diamond is completely clear and transparent. As
in all natural substances, perfection is nearly impossible to find. Inclusions of other
minerals and elements cause varying degrees of opacity. The surface of a diamond can be
clouded by natural processes, such as the constant tumbling and scraping in the bed of a
river.
Luster is the general appearance of a crystal surface in reflected light. Luster of a smooth
crystal face of diamond is strong and brilliant. It is intermediate between glass and metal
and has its own special term--adamantine.
The process of white light breaking up into its constituent colors is called dispersion.
Diamonds have strong dispersion, which along with their strong luster, causes the
beautiful play of colors so often referred to as the "fire" of a diamond.
Gemstone varieties of diamond are usually clear and colorless, often containing minor
inclusions and imperfections. Yellow or yellowish-brown and even brilliant yellow
diamonds have been found. Very rarely, diamonds are blue, black, pale green, pink,
violet, and even reddish.
The most famous blue diamond, the Hope Diamond, is intertwined with Colorado's
mining history. Thomas Walsh, discoverer of the rich Camp Bird Mine near Ouray,
purchased the Hope Diamond for his wife in the early 1900s; it was later given to his
daughter, Evelyn Walsh McLean who wore it almost continuously until the 1940s. The
45.5-carat Hope Diamond now resides at the National Museum of Natural History in
Washington, D.C.
Diamonds, in their perfect cubic crystal form, occur as isolated octahedral (eight-sided)
crystals (see figure below). Many variations on the cubic form are found in nature,
including twelve-sided crystals and a flattened triangular shape known as a macle.
Gemologists recognize three main varieties of diamonds: ordinary, bort, and carbonado.
Excerpts from ROCKTALK vol. 2 no. 3
Colorado Geological Survey
Ordinary diamonds occur as crystals often with rounded faces, from colorless and free
from flaws ("the first water"*) to stones of variable color and full of flaws. Bort
inferior quality as a gemstone. Carbonados are black opaque diamonds usually from the
Bahia Province of Brazil. They are crystalline but do not possess the mineral cleavage
found in ordinary diamonds.
* An expression which refers to the highest quality diamonds and has come to mean the
highest quality of just about anything.
Size comparison of octahedral diamond crystal
for 1 to 500 carats.
Excerpts from ROCKTALK vol. 2 no. 3
Colorado Geological Survey
Diamonds form in nature only under the extreme conditions found in the upper mantle at
depths of 150 to 200 kilometers (possibly down to 300 kilometers): pressures of greater
than 50 kilobars (50,000 x normal atmospheric pressure) and temperatures of 900 to
1,300øC and possibly higher. The diamonds form as minerals within rocks of the upper
mantle called eclogite and peridotite. Eclogite is a coarse-grained rock consisting of red
garnet (almandine-pyrope) and a green pyroxene (omphacite). Peridotite is believed to be
the most common rock of the upper mantle; it contains varying amounts of three
minerals, olivine, orthopyroxene and clinopyroxene. The olivine rich peridotite is called
dunite, and the pyroxene rich rock is called websterite. The rock harzburgite contains up
to 40 percent orthopyroxene and 60 to 90 percent olivine and is thought to be the most
common host rock for diamonds.
If diamonds are formed at depths of 150 to 200 kilometers in the upper mantle, how do
they get to the surface of the earth? They are brought to the surface in a peculiar igneous
rock called kimberlite (named after the diamond-bearing region of Kimberly, South
Africa where these rocks were first identified.) Kimberlites are intrusive bodies that
originate in the upper mantle and are injected upward through the upper mantle and the
lower and upper crust, eventually reaching the earth's surface as a small volcanic
complex (see figure on p. 3). Kimberlites have three facies correlative to their position in
the mantle and crust: the root facies, the diatreme facies, and the crater facies. The shape
of the kimberlite shown in the figure is similar to that of a carrot or a pipe; a
comparatively wide upper zone, up to several hundred meters in diameter, in the diatreme
and crater facies; to a lower zone, which narrows into a thin intrusive dike, possibly only
a meter thick, in the root facies. The forceful intrusion of the kimberlite brecciates* the
surrounding rocks of the upper mantle and crust and incorporates them as xenoliths
(xenolith literally means "foreign rock"). Often these xenoliths of the upper mantle
peridotites or eclogites contain diamonds.
* Means to break apart into smaller angular fragments. A rock composed of angular
fragments is referred to as a breccia.
Diamonds, being mostly pure carbon, are not amenable to modern methods of age-dating
rocks (Carbon 14 dating methods are useful with materials less than about 50,000 years.
Most rocks are millions to billions of years old. With recently developed age-dating
techniques, the small inclusions of other minerals in diamonds (such as garnet) can be
dated. Recent dating of inclusions in diamonds from kimberlite pipes, mainly in South
Africa and Australia, indicate that diamonds formed as early as 3,300 million years ago to
as late a 990 million years ago, an extended period of the earth's history. The kimberlite,
which carried the diamonds to the surface and is the present host rock, was intruded only
about 100 million years ago.
Kimberlites ascend rapidly to the earth's surface at rates thought to be on the order of 10
to 30 kilometers per hour. There is usually no evidence of any substantial thermal
reaction with the surrounding country rock. In the near surface environment, velocities
may increase to several hundreds of kilometers per hour because of gas expansion in the
Excerpts from ROCKTALK vol. 2 no. 3
Colorado Geological Survey
ascending magma and reaction with water. Craters, tuff rings, and maars form as the
highly charged kimberlite magma erupts at the surface.
Kimberlites, though rare, are widespread throughout the surface of the earth. Most well
known diamond producing pipes are small, 12 to 75 acres, and they generally occur in
clusters of six to forty pipes. Almost all diamond bearing kimberlites are found in the
ancient stable cratons of the continents, never in oceanic crust or in younger mountain
belts, like the Alps or the Sierra Nevada in California.
Diagram of an idealized kimberlite intrusion.
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