Many pure substances in the laboratory are either dull, white powders or dull, coloured powders. If they are dissolved and allowed to crystallize slowly, their geometry becomes apparent to the naked eye, and light interacts with crystals far more elaborately. In nature's laboratory, impurities, heat, and pressure help convert compounds and elements into minerals. These new forms retain their basic ratios of bonded atoms, but as the philosopher Santayana would say, minerals now objectify pleasure---in other words, they become beautiful.
Scroll down to see a few examples:
| Mineral | Main Chemical Compound | |
![]() Pic from http://www.mineralatlas.com/mineral%20photos/M/marcasite2.jpg |
Marcasite(FeS2) | FeS2 |
Pic from Wikipedia. |
Bornite(Cu5FeS4) | Cu5FeS4 |
Pic from http://gwydir.demon.co.uk/jo/minerals/calcite.htm |
Calcite | CaCO3 |
Pic from http://www.gc.maricopa.edu/earthsci/imagearchive/realgar.jpg |
Realgar | AsS |
Pic from author. |
Amethyst | SiO2 |
Pic from http://www.sedgwickmuseum.org/education/gallery.html |
Sulfur | S |
Pic from author. |
Sucrose (not really a mineral but I formed this crystal of a common organic compound by forgetting about a saturated solution in the fridge.) |
C12H22O11 |





