Zircon
A tough silicate that traps uranium and refuses lead — which is how the age of the Earth is known, and the only real source of zirconium.
Zircon's importance rests on a quirk of its chemistry. When it crystallises it accepts uranium into the site zirconium would occupy, and rejects lead almost completely. So any lead found inside a zircon crystal arrived there by the decay of uranium after the crystal formed, and the ratio between them is a clock that started when the mineral did.
Zircon is also extraordinarily durable — hard, chemically resistant, and surviving erosion, transport and burial intact. Grains have been dated to more than four billion years, older than any surviving rock, and they are the principal physical evidence for what the early Earth was like.
How to identify it
Zircon is hard, heavy and brilliant, with an adamantine lustre and strong dispersion that made it the traditional diamond substitute before synthetic stones. Crystals are stubby tetragonal prisms with pyramidal ends.
Some specimens are partly metamict — their structure damaged by the radiation of their own uranium — which lowers the hardness and density and makes the mineral cloudy.
Uses
Most zircon is used as sand rather than as a metal source: in foundry moulds, refractory linings and ceramic glazes, where its heat resistance and low thermal expansion matter.
It is also the ore of zirconium and, inseparably, of hafnium — the two are chemically so alike that separating them is among the more difficult operations in industrial chemistry, and the separation matters because zirconium is nearly transparent to neutrons and hafnium absorbs them, which makes one a reactor cladding and the other a control rod.
How we know: checked recently · only one source, so there is nothing to cross-check it against · stated directly by the source.
How this connects
Where a connection has been confirmed by an outside reference, that reference is named beside it.
is an ore of
is an alternative to
- Diamond — mineral · as a gemstone only: zircon's dispersion and adamantine lustre made it the traditional diamond substitute, long before synthetic stones. It is nowhere near as hard
is commonly confused with
- Xenotime — mineral · both tetragonal phosphate-like prisms in the same heavy mineral sands; zircon is harder and denser
is a component of
is a source for
- Hafnium — element · always with zirconium in zircon, from which it is separated only because reactor-grade zirconium must be free of it — hafnium absorbs the neutrons zirconium lets through
Sources
- Material WorldOur own writing
- Wikimedia Foundation · Creative Commons CC0 1.0 Universal (public domain dedication)
- COD Advisory Board / Vilnius University · CC0 — contributors place data in the public domain