How do minerals change without melting?

1 Answer
Dec 4, 2015

Pseudomorphism!

Explanation:

Cool word isn't it?

This is a really cool way that a mineral can change its atomic structure without melting. But note that the mineral doesn't change its chemical composition in this case.

An example, a mineral such as Kyanite ("Al"_2"SiO"_5Al2SiO5) has three forms which it can exist in depending on the pressure and temperature conditions.

At low pressure (a few kilobars, roughly a few kilometres into earths crust) andalusite is the stable structure and then at higher temperature moderate pressure sillimanite is the stable structure.

So as we change pressure and temperature a different atomic structure becomes stable and the mineral changes.

Another example is diamond. Diamond is simply carbon ("C"C) but expose it to pressures of around 40 kilobars or more (> 100 km into the mantle) then you get diamond!

Though, I wouldn't recommend putting your pencil in the oven for a few weeks to try and make diamond! But expose diamond to some high temperature and pressure (below its stability field) and it might just transform back to graphite!

![http://serc.carleton.edu](https://useruploads.socratic.org/LKUEDx5Q2S2GATFIP9rA_fields.jpg)

Above is the stability ranges for the three guys I mentioned above, diamond occurs four times higher than this diagram (more than 120km into our mantle)!

NB: "0.1 GPa " = " 1 kilobar"0.1 GPa = 1 kilobar