The global copper supply chain begins with the extraction of copper from porphyry deposits—vast, low-grade hydrothermal ore bodies formed by the cooling of magma-rich fluids deep within the Earth's crust. These deposits are characterized by a network of veinlets and disseminated minerals, where the most prevalent species is chalcopyrite ($\text{CuFeS}_2$), a copper-iron sulfide.
Extraction is dominated by massive open-pit mining, exemplified by the Chuquicamata mine in Chile and the Bingham Canyon Mine in the United States. These operations are monuments to industrial scale, moving millions of tons of overburden to access ore containing as little as 0.4% to 1.0% copper. In addition to these primary sulfide deposits, the industry utilizes solvent extraction and electrowinning (SX-EW) to recover copper from oxide ores, where the metal is leached using sulfuric acid—a process that allows for the exploitation of lower-grade surface deposits that would otherwise be economically invisible.
The transition from raw ore to high-purity conductive metal involves a sequence of energy-intensive thermal and chemical stages:
Copper production is highly concentrated. Chile remains the world's largest producer, followed by Peru, Indonesia, and the United States. The demand is increasingly driven by the global energy transition; copper's superior electrical and thermal conductivity makes it indispensable for electric vehicle (EV) motors, wind turbines, and the expansion of the global electrical grid. China currently accounts for over half of the global demand, acting as the primary hub for the refinement and application of the metal.
The infrastructure of the copper chain is one of extreme scale: from the deep pits of the Atacama Desert to the massive electrolytic refineries and the global network of shipping lanes that transport refined cathodes to industrial centers. The metal's role as the "nervous system" of modern electrification ensures that its supply chain is a critical bottleneck in the transition to a low-carbon economy.