Copper Uses, Resources, Supply, Demand and Production Information
Republished from USGS Fact Sheets released in June, 2009
and January 2014
Copper - A Metal Used Through The Ages
Copper was one of the first metals ever extracted and used by humans, and it has made vital contributions to sustaining and improving society since the dawn of civilization. Copper was first used in coins and ornaments starting about 8000 B.C., and at about 5500 B.C., copper tools helped civilization emerge from the Stone Age. The discovery that copper alloyed with tin produces bronze marked the beginning of the Bronze Age at about 3000 B.C.
Copper is easily stretched, molded, and shaped; is resistant to corrosion; and conducts heat and electricity efficiently. As a result, copper was important to early humans and continues to be a material of choice for a variety of domestic, industrial, and high-technology applications today.
How Do We Use Copper Today?
Presently, copper is used in building construction, power generation and transmission, electronic product manufacturing, and the production of industrial machinery and transportation vehicles. Copper wiring and plumbing are integral to the appliances, heating and cooling systems, and telecommunications links used every day in homes and businesses. Copper is an essential component in the motors, wiring, radiators, connectors, brakes, and bearings used in cars and trucks. The average car contains 1.5 kilometers (0.9 mile) of copper wire, and the total amount of copper ranges from 20 kilograms (44 pounds) in small cars to 45 kilograms (99 pounds) in luxury and hybrid vehicles.
Ancient Uses of Copper
As in ancient times, copper remains a component of coinage used in many countries, but many new uses have been identified. One of copper's more recent applications includes its use in frequently touched surfaces (such as brass doorknobs), where copper's antimicrobial properties reduce the transfer of germs and disease. Semiconductor manufacturers have also begun using copper for circuitry in silicon chips, which enables microprocessors to operate faster and use less energy. Copper rotors have also recently been found to increase the efficiency of electric motors, which are a major consumer of electric power.
What Properties Make Copper Useful?
The excellent alloying properties of copper have made it invaluable when combined with other metals, such as zinc (to form brass), tin (to form bronze), or nickel. These alloys have desirable characteristics and, depending on their composition, are developed for highly specialized applications. For example, copper-nickel alloy is applied to the hulls of ships because it does not corrode in seawater and reduces the adhesion of marine life, such as barnacles, thereby reducing drag and increasing fuel efficiency. Brass is more malleable and has better acoustic properties than pure copper or zinc; consequently, it is used in a variety of musical instruments, including trumpets, trombones, bells, and cymbals.
Types of Copper Deposits
Copper occurs in many forms, but the circumstances that control how, when, and where it is deposited are highly variable. As a result, copper occurs in many different minerals. Chalcopyrite is the most abundant and economically significant of the copper minerals.
Research designed to better understand the geologic processes that produce mineral deposits, including copper deposits, is an important component of the USGS Mineral Resources Program. Copper deposits are broadly classified on the basis of how the deposits formed. Porphyry copper deposits, which are associated with igneous intrusions, yield about two-thirds of the world's copper and are therefore the world's most important type of copper deposit. Large copper deposits of this type are found in mountainous regions of western North and South America.
Another important type of copper deposit-the type contained in sedimentary rocks-accounts for approximately one-fourth of the world's identified copper resources. These deposits occur in such areas as the central African copper belt and the Zechstein basin of Eastern Europe.
Individual copper deposits may contain hundreds of millions of tons of copper-bearing rock and commonly are developed by using open-pit mining methods. Mining operations, which usually follow ore discovery by many years, often last for decades. Although many historic mining operations were not required to conduct their mining activities in ways that would reduce their impact on the environment, current Federal and State regulations do require that mining operations use environmentally sound practices to minimize the effects of mineral development on human and ecosystem health.
USGS mineral environmental research helps characterize the natural and human interactions between copper deposits and the surrounding aquatic and terrestrial ecosystems. Research helps define the natural baseline conditions before mining begins and after mine closure. USGS scientists are investigating climatic, geologic, and hydrologic variables to better understand the resource-environment interactions.
Copper Supply, Demand and Recycling
The world's production (supply) and consumption (demand) of copper have increased dramatically in the past 25 years. As large developing countries have entered the global market, demand for mineral commodities, including copper, has increased. In the past 20 years, the Andean region of South America has emerged as the world's most productive copper region. In 2007, about 45 percent of the world's copper was produced from the Andes Mountains; the United States produced 8 percent. Virtually all copper produced in the United States comes from, in decreasing order of production, Arizona, Utah, New Mexico, Nevada, or Montana.
The risk of disruption to the global copper supply is considered to be low because copper production is globally dispersed and is not limited to a single country or region. Because of its importance in construction and power transmission, however, the impact of any copper supply disruption would be high.
Copper is one of the most widely recycled of all metals; approximately one-third of all copper consumed worldwide is recycled. Recycled copper and its alloys can be remelted and used directly or further reprocessed to refined copper without losing any of the metal's chemical or physical properties.
How Do We Ensure Adequate Supplies of Copper for the Future?
To help predict where future copper resources might be located, USGS scientists study how and where known copper resources are concentrated in the Earth's crust and use that knowledge to assess the potential for undiscovered copper resources. Techniques to assess mineral resource potential have been developed and refined by the USGS to support the stewardship of Federal lands and to better evaluate mineral resource availability in a global context.
In the 1990s, the USGS conducted an assessment of U.S. copper resources and concluded that nearly as much copper remained to be found as had already been discovered. Specifically, the USGS found that about 350 million tons of copper had been discovered and estimated that about 290 million tons of copper remained undiscovered in the United States.
Global Copper Resource Assessment
The USGS assessed undiscovered copper in two deposit types that account for about 80 percent of the
world’s copper supply. Porphyry copper deposits account for about 60 percent of the world’s copper.
In porphyry copper deposits, copper ore minerals are disseminated in igneous intrusions. Sediment-hosted
stratabound copper deposits, in which copper is concentrated in layers in sedimentary rocks, account for
about 20 percent of the world’s identified copper resources. Globally, mines in these two deposit types
produce about 12 million tons of copper per year.
This study considered potential for exposed and concealed deposits within 1 kilometer of the surface for
porphyry deposits and up to 2.5 kilometers of the surface for sediment-hosted stratabound deposits. For
porphyry deposits, 175 tracts were delineated; 114 tracts contain 1 or more identified deposits. Fifty
tracts were delineated for sediment-hosted stratabound copper deposits; 27 contain 1 or more identified
Results of the assessment are provided by deposit type for 11 regions (table 1). The mean total undiscovered
resource for porphyry deposits is 3,100 million tons, and the mean total undiscovered resource for
sediment-hosted deposits is 400 million tons, for a global total of 3,500 million tons of copper. The
ranges of resource estimates (between the 90th and 10th percentiles) reflect the geologic uncertainty in the
assessment process. Approximately 50 percent of the global total occurs in South America, South Central Asia
and Indochina, and North America combined.
South America has the largest identified and undiscovered copper resources (about 20 percent
of the total undiscovered amount). The world’s largest porphyry deposits are mined in this region.
Central America and the Caribbean host two undeveloped giant (>2 million ton copper) porphyry
copper deposits in Panama. Most of the undiscovered resources are in a belt that extends from Panama to southwestern Mexico.
North America hosts highly mineralized porphyry copper tracts that include supergiant (>25 million tons copper)
porphyry deposits in northern Mexico, the western United States, and Alaska, as well as giant deposits in western Canada.
The estimated undiscovered porphyry copper resources are approximately equal to the identified resources. In the United
States, undiscovered sediment-hosted stratabound copper deposits in Michigan, Montana, and Texas are estimated to contain
about three times as much copper as has been identified. Two giant deposits are known, in Michigan and Montana.
Northeast Asia is relatively underexplored, with modest identified porphyry copper resources and only one
identified giant porphyry copper deposit. However, the mean undiscovered resources are estimated to be quite large.
This region has the largest ratio of undiscovered to identified resources in the study.
North Central Asia has 35 porphyry copper deposits, including a supergiant deposit in Mongolia and a
giant deposit in Kazakhstan. The tract area is estimated to contain about three times the amount of identified porphyry
copper resource. This region also hosts three giant sediment-hosted stratabound copper deposits, in Kazakhstan and Russia.
The USGS estimates that as much sediment-hosted stratabound copper as has already been discovered may be present.
South Central Asia and Indochina are less thoroughly explored than many other parts of the world; however,
four giant porphyry copper deposits have been identified to date in the Tibetan Plateau. Undiscovered porphyry copper deposits
may contain eight times the identified amount of copper.
Southeast Asia Archipelagos host world-class, gold-rich porphyry copper deposits such as a supergiant in Indonesia and
about 16 giant deposits in Indonesia, Papua New Guinea, and the Philippines. Although parts of the region are well explored,
undiscovered porphyry resources are likely to exceed identified resources.
Eastern Australia has one giant porphyry copper deposit and several small porphyry deposits. Modest undiscovered
resources are expected under cover.
Eastern Europe and Southwestern Asia have been mined for copper since ancient times, and giant porphyry copper
deposits have recently been identified. Undiscovered copper is predicted to be about twice the identified resources, both for
porphyry deposits along a belt from Romania through Turkey and Iran and for sediment-hosted stratabound deposits in Afghanistan.
Western Europe has the largest sediment-hosted stratabound copper deposit in the world, in Poland.
Undiscovered sediment-hosted stratabound copper resources in southwestern Poland are estimated to exceed identified
resources by about 30 percent.
Africa and the Middle East have the world’s largest accumulation of sediment-hosted stratabound copper deposits,
with 19 giant deposits in the Central African Copperbelt in the Democratic Republic of Congo and Zambia. Significant
undiscovered copper resources remain to be discovered.
The information in these USGS Fact Sheets was prepared by Jeff Doebrich, Kathleen Johnson, Jane Hammarstrom, Michael Zientek, and Connie Dicken.
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