At this point, we started to suspect that the material we were seeing simply wasn’t quartzite at all. We had now worked on true quartzite, and the difference in the way these other “quartzites” cut, polished and reacted to acids was becoming difficult to ignore.
Marble and quartzite are both metamorphic stones, formed when existing rock is transformed by heat and pressure. What separates them is largely their mineral composition. Traditional marble is composed primarily of calcite, a form of calcium carbonate. Quartzite, on the other hand, is composed predominantly of quartz. That difference is enormous from a restoration standpoint: calcite is relatively soft and reacts readily with common acids, while quartz is much harder and far more chemically resistant.
Then there is dolomitic marble. Instead of being composed primarily of calcite, it contains a high proportion of the mineral dolomite—calcium magnesium carbonate. Dolomite is somewhat harder and generally reacts more slowly with weak acids than calcite, so dolomitic marble can behave noticeably differently from conventional marble. It is still an acid-sensitive carbonate stone, however, and it is nowhere near quartzite in hardness.
This explained much of what we had been seeing. Some materials being sold commercially as “quartzite” were actually dolomitic marbles: harder and sometimes more etch-resistant than typical marble, but still capable of developing the rings and dull spots our clients were calling us about. To complicate things further, marble, dolomitic marble and quartzite can have remarkably similar colours, veining and movement.
Appearance alone is not a reliable way to tell them apart.
The first image shows a dolomitic marble that was sold as “quartzite.” While somewhat harder than conventional calcitic marble, it remains susceptible to etching and other forms of wear. The second image shows true quartzite, a highly durable material composed predominantly of quartz and generally much harder than marble. Note how similar the two stones can appear despite behaving very differently in use.