What is Chromite?
Chromite is an oxide mineral composed of chromium, iron and oxygen (FeCr2O4). It is a dark gray to black in
color with a metallic to submetallic luster and a high specific gravity. It occurs in basic and ultrabasic
igneous rocks and in the metamorphic and sedimentary rocks that are produced when chromite-bearing rocks are
altered by heat or weathering.
Chromite is important because it is the only economic ore of chromium, an essential element for a wide variety
of metal, chemical and manufactured products. Many other minerals contain chromium, but none of them are found
in deposits that can be economically mined to produce chromium.
Properties of Chromite
Chromite can be challenging to identify. Several properties must be considered to differentiate it from other
metallic ores. Hand specimen identification of chromite requires a consideration of: color, specific gravity,
luster, and a characteristic brown streak. The most important clue to identifying chromite is its association
with ultrabasic igneous rocks and metamorphic rocks such as serpentinite.
Physical Properties of Chromite
||dark gray to black, rarely brownish black
||metallic to submetallic
||5.5 to 6
||4.0 to 5.1 (variable)
||FeCr2O4 with magnesium substituting for iron in significant amounts
||an ore of chromium
Chromite is sometimes slightly magnetic. This can cause it to be confused with magnetite. Chromite and
ilmenite have very similar properties. Careful observations of hardness, streak and specific gravity are
required to distinguish these minerals in hand specimens.
Chromite and Solid Solution
Magnesium frequently substitutes for iron in chromite. A solid solution series exists between the mineral
chromite (FeCr2O4) and the isomorphous mineral magnesiochromite (MgCr2O4).
Intermediate specimens can be rich in iron ((Fe,Mg)Cr2O4) or magnesium ((Mg,Fe)Cr2O4).
For convenience in communication, these minerals are often referred to collectively as "chromite."
Some mineralogists give a generalized chemical composition of (Mg,Fe)(Cr,Al)2O4 for chromite. This
composition recognizes multiple solid solution paths between chromite and hercynite (FeAl2O4),
spinel (MgAl2O4), magnesiochromite (MgCr2O4), magnetite
(Fe3O4), and magnesioferrite (MgFe2O4).
Because of the many different compositions in these solid solution series,
geologists and metallurgists often consider "chromite" to be any member
of the solid solution series that has a significant Cr2O3 content.
Stratiform, Podiform and Beach Sands
Small amounts of chromite are found in many types of rock. However, chromite deposits that are large enough for
mining are generally found in: 1) stratiform deposits (large masses of igneous rock such as norite or peridotite that slowly crystallized from subsurface magma); 2) podiform deposits (serpentines and other metamorphic rocks
derived from the alteration of norite and peridotite); and, 3) beach sands (derived from the weathering of
Stratiform deposits are large masses of igneous rock that cooled very slowly in subsurface magma chambers.
During this slow cooling, chromite and associated minerals crystallized early while the magma was still at a
very high temperature. Their crystals then settled to the bottom of the magma chamber to form a layered deposit. Some
of the layers in these deposits can contain 50% or more chromite on the basis of weight.
Most of the world's known chromite occurs in two stratiform deposits: the Bushveld Complex in South Africa and the
Great Dyke in Zimbabwe. Other important stratiform deposits include: the Stillwater Complex in Montana,
the Kemi Complex of Finland, the Orissa Complex of India, the Goias in Brazil, the Mashaba Complex of Zimbabwe
and small deposits in Madagascar. Nearly all of these are Precambrian in age.
Podiform deposits are large slabs of oceanic lithosphere that have been thrust up onto a continental plate.
These slabs of rock, also known as "ophiolites," can contain significant amounts of chromite. In these deposits
the chromite is disseminated through the rock and not highly concentrated in easy-to-mine layers. Podiform deposits
are known in Kazakhstan, Russia, the Philippines, Zimbabwe, Cyprus and Greece.
The first discoveries of podiform chromite deposits were made near Baltimore, Maryland in the early 1800s. These deposits
supplied nearly all of the world's chromite until about 1850. These deposits were small and are no longer in production.
Chromite is found in beach sands derived from the weathering of chromite-bearing rocks and laterite soils that developed
over peridotite. Beach sand rich in chromite and other heavy minerals is sometimes mined, processed to remove
heavy minerals, and returned to the environment.
Two facts allow these chromite sands to occasionally contain economic deposits of chromite. First, chromite is one of
the more weathering-resistant minerals of peridotite. That causes it to be concentrated in residual soils that form
in the weathering zone above chromite-rich rocks. Second, chromite has a higher specific gravity than other minerals
in peridotite. This causes it to be selectively transported and deposited by wave and current actions, concentrating it in certain locations at streams and
beaches. These deposits are sometimes rich enough and large enough that they can be mined for chromite.
Uses of Chromite and Chromium
Chromium is a metal used to induce hardness, toughness and chemical resistance in steel. The alloy produced is
known as "stainless steel." When alloyed with iron and nickel, it produces an alloy known as "nichrome" which is
resistant to high temperatures and used to make heating units, ovens and other appliances. Thin coatings of
chromium alloys are used as platings on auto parts, appliances and other products. These are given the name "chrome plated."
It is also used to make superalloys that can perform well in the hot, corrosive, and high-stress environment of jet engines.
Chromium's name comes from the Greek word "chroma" which means "color." Chromium is used as a pigment in paint.
The familiar yellow lines painted down the center of highways and the yellow paint used on school buses are often
"chrome yellow" - a color produced from chromium pigment. Chromium is an important pigment in many types of paint,
ink, dye and cosmetics. Trace amounts of chromium produce the color in many minerals and gemstones. The red color
of ruby, the pink of some sapphires and the green color of emerald are caused by tiny amounts of chromium.
Chromium Production and Recycling in the United States
Chromium is not mined in the United States. The chromium consumed by United States industry comes from: A) other
countries in the form of chromite ore, ferrochromium or chromium metal; or, B) chromium recovered from recycled metals.
Over half of the chromium used in the United States today is from recycling.
Because chromium is essential for the defense and prosperity of the United States, the federal government maintains
a stockpile of chromite ore, ferrochromium and chromium metal for use in a national emergency. This type of emergency
could occur if the United States was involved in a war and the enemy prevented the delivery of chromite and chromium products
by sea transport. In addition, small chromite deposits have been located in the United States which could be mined
if they are needed.
Chromite and Diamond Exploration
Kimberlite, the type of rock that holds many of the world's most important diamond deposits, usually contains small amounts
of chromite, ilmenite and certain types of garnet. Although these minerals occur in very small amounts, they are much more
common in the rock than diamonds. Because these minerals do not occur together in most other types of rocks, they can be a
valuable indicator of a nearby kimberlite body if they are found in stream sediments, glacial tills, residual soils,
core samples or well cuttings. Some of the greatest diamond deposits on Earth were discovered using the geology of indicator minerals.
|How do diamonds form?
A detailed article that explains the four sources of diamonds found at Earth's surface.
Contributor: Hobart King
Find it on Geology.com
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|Ant Hill Garnets are tiny garnets that ants haul to the surface and discard on their anthill. Honest!
|Emerald is the most popular green gemstone in the United States and most of the world.
|Jet is a black organic gem material that forms from well-preserved woody material.
|Chromite from the Transvaal area of South Africa. Specimen is approximately 4 inches (10 centimeters) across. |
|A field photo of the Bushveld LG6 chromite seam. This clearly shows the stratiform nature of the deposit. USGS photo by Klaus Schulz. |
||Did You Know? School buses and yellow lines on highways are often painted with "chrome yellow" paint. The "chrome" means chromium was used as an ingredient. Image © iStockphoto / 2windspa.
|Chromite from the Transvaal area of South Africa. This specimen is approximately 3.5 inches (9 centimeters) across. |
|Chromite from Shurugwi, Zimbabwe. Specimen is approximately 4 inches (10 centimeters) across.|
||Did You Know? The color of many gemstones is derived from trace amounts of chromium. The red color of rubies, the pink of some sapphires and the green color of emeralds are derived from chromium. Image © iStockphoto / ProArtWork.
|Chromite Production and Reserves
||2011 Mine Production
||2012 Mine Production (estimated)
The values above are estimated chromite production and reserves in thousands of metric tons. Data from USGS Mineral Commodity Summaries. 
 Stratiform Chromite Deposit Model: Ruth F. Schulte, Ryan D. Taylor, Nadine M. Piatak, and Robert R. Seal II; Chapter E of Mineral Deposit Model for Resource Assessment; Scientific Investigations Report 2010-5070-E; 131 pages; November 2012.
 Chromium: John F. Papp, United States Geological Survey, Mineral Commodity Summaries, January 2013.
 Chromium: John F. Papp, United States Geological Survey, 2011 Minerals Yearbook, April 2013.
 Chromium Makes Stainless Steel Stainless: S. J. Kropschot and Jeff Doebrich, United States Geological Survey, Fact Sheet 2010-3089, September 2010.
 How a Rogue Geologist Discovered a Diamond Trove in the Canadian Arctic: Carl Hoffman, Wired Magazine, Issue 16.12, accessed July 2013.