Silver Ag · 47

The best electrical conductor there is, and the metal that has been used as money for longer than almost anything else.

Why does it matter?

Half of silver demand is industrial, and the fastest-growing piece is the paste that carries current off a solar cell.

Where it is in the Earth

Silver is a rare element, and the geological processes that concentrate it into mineable deposits are varied and often indirect. The most important of these is hydrothermal activity: hot, mineral-laden water moving through fractures in the crust, cooling as it rises, and depositing its dissolved metals in veins and replacement bodies. Silver frequently travels with lead, zinc, copper and gold in these fluids, which is why the ore minerals listed in the table — galena (lead sulfide), acanthite (silver sulfide) and native gold alloyed with silver as electrum — so often occur together in the same deposit. When those hydrothermal fluids encounter reactive carbonate rocks such as limestone, they can replace large volumes of the host rock entirely, creating the massive sulfide bodies that carry much of the world's silver.

The geological term for the most productive silver-bearing district type in history is epithermal, meaning the deposit formed at shallow depth and relatively low temperature. The volcanic belts that ring the Pacific Ocean — through Mexico, Peru, Bolivia and down into Chile — provided exactly the right conditions: recent volcanism supplying the heat, faulted and fractured rock providing the pathways, and thick sequences of sedimentary rock providing the reactive hosts. This is why Latin America dominates the production table so completely. A second, older deposit type is the sediment-hosted or Broken Hill-type orebody, formed when seafloor sediments were buried and metamorphosed, concentrating silver alongside lead and zinc. Australia's Cannington mine is a textbook example of this style. Poland's KGHM deposits belong to a third family: stratiform copper-silver mineralisation in Permian sedimentary rocks, where silver is intimately bound up with copper sulfides rather than lead.

Because silver follows these base metals so closely through geological history, truly primary silver deposits — where silver is the dominant metal rather than a companion — are the exception rather than the rule. The great Comstock Lode in Nevada, Cerro Rico in Bolivia and a handful of Mexican districts qualify, but most silver in the ground exists because lead, zinc, copper or gold happened to be there first. That geological reality has profound consequences for how silver is mined and priced, which the sections below address.

Getting it out

The method used to extract silver from the ground depends almost entirely on the primary metal the mine is really chasing. Because most silver is a by-product, it follows whatever extraction approach makes sense for lead, zinc, copper or gold. Large porphyry copper mines such as Escondida in Chile, Grasberg in Indonesia and Bingham Canyon in the United States operate as open-pit operations, moving enormous quantities of low-grade rock. The silver content in the ore at these mines is small per tonne, but the sheer scale of material processed means that collectively they contribute a significant portion of world supply. Open-pit mining suits these deposits because the ore is disseminated — spread through a large volume of rock — and stripping away the overlying waste to expose it is economically worthwhile only when the volumes mined are very large.

Underground mining is the right approach where ore is higher grade, narrower in geometry, or buried too deeply for an open pit to be practical. Cannington in Australia, which exploits a Broken Hill-type silver-lead-zinc orebody, operates underground. So does Olympic Dam, another Australian mine where silver appears alongside copper, uranium and gold in an iron-oxide copper-gold system. Underground methods recover less total rock but concentrate effort on the ore itself, which is why they suit richer or more complex deposits. Grade — the amount of silver per tonne of ore — is the number that determines which approach makes economic sense, and for a primary silver operation the threshold differs considerably from what a copper mine needs to find silver worth noting in its accounts at all.

What this means in practice is that the volume of waste rock moved per unit of silver produced varies enormously across the industry. A bulk open-pit copper mine produces silver almost as an afterthought, incurring no incremental mining cost for it. A primary silver underground mine must justify each metre of development entirely on the silver (and any associated lead or zinc). The by-product mines dominate total supply, and because their silver output is largely governed by decisions about copper, lead or zinc production, global silver mining volumes do not respond to silver prices in the straightforward way that a purely primary metal's supply would.

What pulls on it

Silver sits at an unusual intersection of monetary history and modern industry. For most of recorded history it functioned as currency, store of value and jewellery metal, and those uses persist: jewellery, silverware and investment (bars and coins) still account for a meaningful share of annual consumption. But the tables on this page show that industrial demand now accounts for roughly half of total use, and within that industrial share the fastest-growing application is the conductive paste printed onto the front face of crystalline silicon solar cells. That paste is the electrical pathway that carries current generated by the cell to the external circuit, and it is made from very fine silver powder. The intensity figure in the table — between 8 and 20 kilogrammes per megawatt of capacity — captures how much silver goes into a solar module, though the range is wide because cell designs differ and because the industry has been steadily reducing silver content per cell for years.

Beyond solar, silver's combination of the highest electrical conductivity of any element and good resistance to the formation of insulating oxides on its surface makes it the preferred contact material wherever reliable electrical switching matters: power-grid contactors and switchgear, automotive relays, consumer electronics. These applications tend to be mature and relatively stable in volume, contracting slowly as engineers find ways to use thinner layers or smaller contact areas. Medicine is a smaller but persistent market: silver's well-documented antimicrobial effect — bacteria cannot readily develop resistance to it in the way they do to antibiotics — keeps it in use in wound dressings and coatings for medical instruments. Nuclear power plants using pressurised-water reactor designs use a silver-indium-cadmium alloy in their control rods, a low-volume but highly specific application where substitution is tightly constrained by reactor licensing.

The direction of demand is therefore being pulled in two directions at once. Investment and jewellery demand fluctuates with economic sentiment and price expectations, and can swing sharply. Industrial demand is growing in aggregate because solar deployment is growing, but the solar industry is also systematically engineering silver out of each individual cell. Whether total solar-related silver consumption rises or falls over the coming years depends on which of those two forces — more modules installed versus less silver per module — runs faster. That tension is one of the genuinely unresolved questions in the silver market.