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Mineral · SrCO3

Strontianite

Strontium carbonate, named after the Scottish village it was found in — and the reason a firework burns red.

Ore

Strontianite is strontium carbonate, and it carries one of the few mineral names taken from a specific village — Strontian in the Scottish Highlands, where it was identified in the 1790s and where the element was subsequently found and named after it.

Its familiar consequence is colour. Strontium salts burn an intense crimson, and that is the red in fireworks, distress flares and signal lights. No other element gives quite that red cheaply, which is why a nineteenth-century discovery in a lead mine is still visible on every bonfire night.

How to identify it

Colourless to pale green or yellow, vitreous, and effervescing in acid like any carbonate. It is very close to aragonite in structure and habit, and the reliable distinction is the flame: strontianite colours a flame crimson where aragonite gives the orange of calcium.

Medium confidence Weak evidence

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

  • Strontium element · a source, though celestine supplies more of it Wikidata

is commonly confused with

  • Aragonite mineral · near-identical structure and habit; the distinction is the flame, crimson against calcium's orange

is a component of

  • Limestone rock · in nodules and cavities, strontium substituting for calcium and then separating out — the mineral's commonest sedimentary occurrence

contains

Sources

  • Material World
    Our 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

Questions this page answers

Where it comes from, and what it becomes

Follow Strontianite back to what it starts as, and forward into what it becomes. Each step is a documented one — a real route material takes, not a chain of inference.

Downstream — what it becomes

  • Strontianite → is a component of (in nodules and cavities, strontium substituting for calcium and then separating out — the mineral's commonest sedimentary occurrence) → Limestone → is an input to (heated until the carbonate decomposes to lime and carbon dioxide) → Calcination → produces (the solid residue once carbon dioxide has been driven off) → Quicklime → is a component of (as calcium oxide within the clinker phases, not as free lime) → Portland cement → is used in → Construction
  • Strontianite → is an ore of (a source, though celestine supplies more of it) → Strontium → is used as → Pigment
  • Strontianite → is a component of (in nodules and cavities, strontium substituting for calcium and then separating out — the mineral's commonest sedimentary occurrence) → Limestone → is an input to (heated until the carbonate decomposes to lime and carbon dioxide) → Calcination → produces (the solid residue once carbon dioxide has been driven off) → Quicklime → is an input to (forms a basic slag that strips phosphorus and sulfur out of the melt) → Basic oxygen steelmaking → produces (most of the world's primary steel) → Steel
  • Strontianite → is a component of (in nodules and cavities, strontium substituting for calcium and then separating out — the mineral's commonest sedimentary occurrence) → Limestone → is an input to (heated until the carbonate decomposes to lime and carbon dioxide) → Calcination → produces (the solid residue once carbon dioxide has been driven off) → Quicklime → is a source for (slaked to hydroxide, then setting by reabsorbing carbon dioxide from the air) → Lime mortar → is used in (in conservation, where it is a requirement rather than a preference — a cement mortar harder than a soft historic brick destroys the brick) → Construction
  • Strontianite → is a component of (in nodules and cavities, strontium substituting for calcium and then separating out — the mineral's commonest sedimentary occurrence) → Limestone → is an input to (heated until the carbonate decomposes to lime and carbon dioxide) → Calcination → produces (the solid residue once carbon dioxide has been driven off) → Quicklime → is an input to (slaked with water to make the lime putty that mortar and plaster are mixed from) → Hydration → produces (it does not dry — the calcium silicates react with the mix water and grow an interlocking hydrate gel, which is why it sets under water and must be kept wet to reach strength) → Concrete
  • Strontianite → is a component of (in nodules and cavities, strontium substituting for calcium and then separating out — the mineral's commonest sedimentary occurrence) → Limestone → is an input to (heated until the carbonate decomposes to lime and carbon dioxide) → Calcination → produces (the solid residue once carbon dioxide has been driven off) → Quicklime → is a component of (as calcium oxide within the clinker phases, not as free lime) → Portland cement → is a component of (the binder — the expensive, energy-intensive, chemically active part) → Concrete

These are the most distinct paths onward. Strontianite ends up in others besides.