Skip to content

Pliny on the formation of selenite.

Pliny the Elder, on selenite mined near Segóbriga (Segobriga near modern Saelices, Cuenca in Spain), Naturalis Historia 36.45:

Umorem hunc terræ quadam anima crystalli modo glaciari et in lapidem concrescere manifesto apparet, quod cum feræ decidere in puteos tales, medullæ in ossibus earum post unam hiemem in eandem lapidis naturam figurantur.

It is patently obvious that this is a liquid frozen like quartz by some spirit in the earth and hardened into rock, because when animals fall into their mineshafts, their bone marrow transforms into the same kind of rock after a single winter.

As given it sounds like something of an outlandish hypothesis, but apparently the only difficult part is the post unam hiemem “after a single winter”. Gypsum permineralization of animal remains is not unknown, but the process would certainly have taken longer than a season; it has been suggested that the animals found were prehistoric fossils and the assumption that they had fallen into the mine would just have been the simplest explanation of why animals would be found at such a depth to begin with.

Selenite (<em>lapis specularis</em>)

Selenite (lapis specularis)

As for crystalli modo glaciatur—today, of course, we wouldn’t say that any crystal, except possibly that of ice, would be formed by freezing; the usual explanation is precipitation out of a solution. Ancient Europe, though, was very weak on the chemistry of solutions: Aristotle, for example, asserted (in On Generation and Corruption) a drop of wine could not be mixed into ten thousand gallons of water, but that the mass of water would overpower and transform that wine into water if they came together. (Today we recognize contaminants can have effect even highly diluted; a drop in ten thousand gallons is about one part per billion and, to take a concrete example, 2 parts per billion is the maximum acceptable quantity of mercury in American drinking water.) With that level of understanding, saying that something ‘freezes the way that quartz crystal does’ (crystalli modo glaciatur) is probably as close to saying it ‘crystallizes’ that you’re going to get.

Still, to ‘rescue’ the text to something like:

It is patently obvious that this is a liquid crystallized and petrified by some geological process…

…is probably a task best left to Plinipedia, if that ever happens. (There really ought to be a project devoted to updating and correcting Pliny.)

[For crystallum.]

{ 2 } Comments

  1. Alex | March 25, 2011 at 8:42 am | Permalink

    I read elsewhere (I forget where; probably on Plinipedia :) ) that Pliny regarded quartz as a form of ice that had become “permanent” due to being frozen for a long time. This had been justified by the observation that quartz had been found on glaciers but not on volcanoes.

    It’s my understanding that there’s much confusion as to the identity of “selenite” – as the name has been used for either moonstone or for the crystalline form of Gypsum, two completely different minerals. I’m currently attempting to unravel this one. Can of worms.

  2. Muke | March 25, 2011 at 10:01 am | Permalink

    Pliny does assume quartz is formed this way in this passage; I haven’t seen if he asserts it explicitly elsewhere.

    The word ‘selenite’ may be ambiguous in some authors, but the name Pliny uses in this section is ‘lapis specularis’, which I think is unambiguously the gypsum crystal. He says the original and highest-quality source of it was Segóbriga, and the mines there were gypsum mines.

Post a Comment

Your email is never published nor shared. Required fields are marked *