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Lesson 06 · Ore Bodies

Laterites — what's left after the rock rots

What you’ll getUnderstand a family defined by how it formed (weathering), the metals it gives, and why it's cheap to dig but costly to refine.

Here's a twist. Up to now, families were named after the partner element. This one is named after how it formed instead.

The definition: a laterite is soil and rock left behind after millions of years of intense weathering — that's rain, heat, and time slowly rotting the rock — in hot, wet, tropical climates. The rain washes away the parts that dissolve and leaves certain metals concentrated near the surface, mostly as oxides.

What they give us

  • Nickel laterites — a huge share of the world's nickel, with cobalt alongside it.
  • Bauxite — the ore of aluminium. Here's a useful fact to lock in: bauxite is itself a laterite, just one where aluminium got concentrated instead of nickel.

The trade-off that defines this family

Because laterites sit right at the surface, they're cheap and easy to dig — no deep underground tunnels. But the metal is locked up in oxide form, so freeing it is expensive. The go-to method is HPAL — High-Pressure Acid Leach — where sulfuric acid, under high heat and pressure, dissolves the nickel and cobalt out.

A tale of two nickelsNickel can come from a sulfide (deep, float-and-smelt) or a laterite (surface, dig-and-leach). Same metal, two totally different deposits and methods. If you understand why, you understand this whole course.
← Lesson 5 · Oxides — metal joined to oxygen
Lesson 7 · Mineral sands & placers — when nature does the sorting →