Rocks composed of minerals of widely different hardness, and rocks that wear by the pulling out of mineral grains from a relatively soft matrix, had relatively high resistance to polishing. Conversely rocks consisting of minerals having nearly the same hardness wore uniformly and tended to have a low resistance to polishing.
The gritstone group is excellent, with resistance to polishing being always high, whereas the lime stone and flint groups yield the lowest resistance. Other groups, basalt, granite and quartzite, yield intermediate results.
Resistance to polishing of samples from the basalt group show a wide range. Resistance is higher when minerals of different hardness are present, and when the ground-mass is foliated or fluxioned. The resistance is also influenced by the proportion and hardness of secondary minerals, softer minerals giving higher resistance.
In groups of igneous rocks the petrological characteristics which most readily affect resistance to polishing are variation in hardness between the minerals and the proportion of soft minerals. Rocks with cracks and fractured minerals are of higher resistance, whereas finer- grained allotriomorphic rocks tend to polish more readily.