Green Vitriol

Green Vitriol


Simply put, a vitriol is a metallic sulfate compound, often but not always hydrated. The crystals of most vitriols are glassy and all are soluble in water, making solutions containing sulfuric acid. In fact, the very word vitriol has its origin in the Latin word for glass, vitrum.

Out of the ten or so vitriol compounds, one is common and occurs along faults and oxidized zones in metallic mineral deposits: green vitriol, better known to geologists and miners as the mineral melanterite, or to chemists as iron sulfate heptahydrate, FeSO4·7H2O. Pure green vitriol is a transparent pale green solid. Not surprisingly, it has a glassy luster just like broken glass.

Green Vitriol

On the surface of the earth, green vitriol that is most common form of vitriol. As the mineral melanterite, you can find it at most iron, zinc, lead, copper and other metallic mineral deposits. These mineral deposits bearing melanterite will all have the following properties in common: iron, sulfur in some form and lots of oxidation. You need all three to make melanterite.

Find a fault in a mine or find a place where there is water seepage in or next to a metallic mineral mine and that’s where you’ll probably find melanterite. Why? Well, for three reasons.

  • The first is the presence of the common sulfide minerals which occur in many mineral deposits. Pyrite, also known as iron sulfide, FeS2, or as fool’s gold, is a good example of a common sulfide mineral. Sulfide minerals provide green vitriol with the sulfur it needs to form.
  • The second reason is water, which prefers to travel along joints, fractures and faults in rocks. The thing about water is that it is rich in oxygen and lots of oxygen is required for the iron and sulfur in rocks to be oxidized.
  • The third reason is the abundance of iron. Iron is everywhere waiting to be oxidized.  Iron is the fourth most-abundant element in the earth’s crust. The abundance of iron is the reason that most metallic mineral deposits have a cap or “gossan” of oxidized-iron minerals in the form of limonite, a rust-colored melange of various oxidized iron compounds.  You can often find melanterite in gossans if the climate isn’t too dry. You can also find melanterite in streams with acid mine drainage or on tailings piles rich in limonite or along seeps and faults inside, on top of, or next to old mines.

Another name for green vitriol and one that all of nineteenth or earlier English-speaking ancestors would have known was copperas. Along with alum, copperas was one of the essential raw materials of the pre-industrial world.

The Uses of Green Vitriol

Green vitriol – or copperas, if you prefer – was formerly used for all sorts of things and is still used today. In the Middle Ages, it was the starting material to make early formulations of sulfuric acid. It should not be a surprise that the old pre-industrial name for sulfuric acid was oil of vitriol.

Green vitriol was also used as a leather dye commonly sold as shoemaker’s black. In addition, it was utilized as a mordant to fix dyes for the coloring raw cloth – and it retains that use to this day. It was an ingredient in several black ink recipes from antiquity to the early twentieth century. In leather dye and in oak gall ink, the soluble iron from the green vitriol would react with the tannic and gallic acids in the leather or proto-ink solution, respectively, to form iron tannate and iron gallate, both of which are black.

Modern uses of this chemical compound include as a supplement for treating anemia, as a preventative medicine for constipation, as a water treatment to prevent eutrophication, as a fertilizer and lawn conditioner (often bagged and sold as copperas), and as a reducing agent in environmental remediation to reduce chromium VI to less toxic forms. Because of its ready solubility and its power as a reducing agent, it is widely used in many industrial processes.

Making Green Vitriol

The easiest and most ancient way to make green vitriol is to evaporate naturally-occurring spring water that was saturated with iron sulfate. As unlikely as this may sound, evaporating such saturated waters from springs or from mine drainage waters was described by the first-century AD Roman encyclopedist Pliny the Elder. Such waters still exist today, though I’m not sure anyone is using them for producing modern chemicals for sale. I’ve personally observed such waters precipitating sulfates in the California Coast Ranges.

As an example, here’s a photo I took while working at a Superfund site that shall remain nameless. The tank shown below collected the drainage of an inactive mine before it was piped into a treatment plant. The pH of this saturated solution was less than one. One of the folks I worked with on this project actually had to invent a test to measure pH less than zero in order to test some of the waters at this site. This stuff was acid mine drainage on steroids, the worst of which was later shown to be the most acidic fluid discovered on earth.

I grabbed a sample of the mine drainage in the tank and took it home with me, where I allowed it to evaporate. I got lovely green crystals of green vitriol as a result. I then used my green vitriol to dye some leather black for some reenactment stuff that I do as a hobby.

A collection tank of iron sulfate saturated waters from mine drainage.
A collection tank of iron sulfate saturated waters from mine drainage. Note the lovely green color. Evaporating this mine drainage “water” resulted in crystals of green vitriol.

The next method for making green vitriol is to collect rocks rich in both iron and sulfur, like pyrite which is FeS2. The starting rocks are broken up and soaked, and the solutions are drawn off and allowed to evaporate, thus congealing vitriol crystals. Up into the nineteenth century, it was common to lower strips of iron into the sulfate-saturated solutions. As you may recall from the chemistry of the electromotive series from high school chemistry, the insertion of the metallic iron will force the precipitation of any copper out of the solution and provides a preferential site on the iron strips for the precipitation of the iron sulfate heptahydrate crystals. Using iron strips was necessary since copper was and is a common contaminant in metallic mineral deposits.

Agricola mentions this method in his classic sixteenth century opus on mining and minerals, De Re Metallica. The problem here is that Agricola plagiarized this method from Biringuccio’s Pirotechnia, published a few years before De Re Metallica. Maybe Agricola stole it from Biringuccio because a few years before Agricola published De Re Metallica, Biringuccio has previously plagiarized his earlier work, De Re Fossilium. So one plagiarized the other, who then plagiarized the first in return, which just goes to show you that two wrongs can make a write…

Interesting Vitriolic Trivia

We get the word vitriolic from vitriol’s former association with the production of sulfuric acid.

In the later half of the sixteenth century, most green vitriol was made and sold by the Holy See. Newly Protestant England with its huge cloth trade was in trouble because it couldn’t get vitriol to fix cloth dyes in the textile trade that was its life blood. Queen Elizabeth the First supported and encouraged the creation of copperas houses for the manufacture of green vitriol using the exposed rocks method. The starting material was raw copperas – the mineral pyrite – that washed out of the London Clay along beaches in Kent and Essex.


  • Allen, T., Cotterill, M., and Pike, G., 2004, Copperas: An account of the Whitstable Works and the first industrial-scale chemical production in England, Canterbury Archaeological Trust Occasional Paper No. 2., ISBN 1-870545-08-7.
  • Alpers, C.N., J.L. Jambor and D.K. Nordstrom, 2000, Sulfate Minerals, Rev. Min 40, Mineralogical
    Society of America, ISBN 0-939950-52-9.
  • Agricola, G., De Re Metallica, trans. by Hoover, L., and Hoover, H., 1950, Dover Publications,
    ISBN 0486600068.
  • Biringuccio, V., The Pirotechnia, trans. by Smith, C., and Gnudi, M., 1990, Dover Publications, 477
    pp., ISBN 0486261344.
  • Hoover, H., and Hoover, L., 1912, Translators’ Annotations to Agricola’s De Re Metallica, in:
    Agricola, G., De Re Metallica, Dover Publications, ISBN 0486600068.
  • Pliny the Elder, Natural History, Volume 9 (Books 33-35), trans. By H. Rackham, 1958, Loeb
    Classical Library/Harvard University Press, 430 pp., ISBN 0-674-99433-7.
  • Rosetti, G., The Plictho, trans. by Edelstein, S., and Borghetty, H., 1969, MIT Press.
  • J.C. Shenstone, J. C., 1907, “Copperas Industry,” in W. Page and J.H. Round (eds), The Victoria Historyof the County of Essex, Vol. II, pp. 411-13.

Today’s banner image is iron (II) sulfate heptahydrate, by Benjah-bmm27 (2007),  in the public domain, via Wikimedia Commons

4 thoughts on “Green Vitriol

    1. Yes. that’s Iron Mountain – the place with pH negative two fluids inside the old mine workings.

    1. I don’t know of any off the top of my head. In general, one tends not to find any of the hydrated sulfate minerals on any of the mineral auction or sale sites because they are not stable outside of the moist high-fugacity environments of acid mine drainage, underground mines and geologic water-saturated faults.
      I personally have found melanterite at the base of tailings piles of sulfide-bearing deposits and along streams below old mines. That green color is characteristic of the mineral. But as to websites where one might actually procure some, try checking the mineral auctions sites. It’s not common, but sometime a good piece of melanterite will come up for sale.

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