IN SUMMARY
Platinum is almost never discussed alone. It comes as a sextet with palladium, rhodium, iridium, osmium and ruthenium, collectively the platinum group metals (PGM), whose geology, processing and applications are so intertwined that they are treated as a single family. They are by far the rarest metals in the Earth's crust, present at parts-per-billion levels, and that scarcity, combined with extraordinarily complex processing, makes their per-kilogram environmental impact orders of magnitude higher than common metals. As demand shifts from catalytic converters toward hydrogen fuel cells, this guide, part of Minviro's "Explore the Elements" series, introduces PGM geology, processing routes, markets and the role of LCA.
PGM are the rarest metals in the crust. Found at parts-per-billion levels, most of Earth's platinum group metals sank into the core during planetary formation, leaving only scarce, highly refractory deposits at the surface, always alongside nickel, copper and gold.
Supply is extraordinarily concentrated. South Africa's vast Bushveld Complex holds around 70% of global PGM mineral wealth, with Russia, Zimbabwe and Canada (notably the Sudbury meteorite-impact deposit) making up most of the rest.
Their carbon footprint is exceptionally high. Because so little is mined and processing is so complex, platinum can emit tens of thousands of kg CO₂e per kg, compared with roughly ten per kg for nickel, which makes LCA essential for the sector.



