Rocks differ in hardness, due to differing compounds that make up the rock.In 1822 an Austrian geologist, Frederick Mohs, devised a scale that ranked different mineral samples for their hardness, therefore standardising the field tests done by miners across the world.
Mohs chose the following samples as standards due to their abundance and different hardness.
1 = Talc, 2 = Gypsum, 3 = Calcite, 4 = Fluorite, 5 = Apatite, 6 = Orthoclase, 7 = Quartz
8 = Topaz, 9 = Corundum, 10 = Diamond.
By having a standard scale, prospectors can begin to classify the materials they are finding.