The Mohs scale is a qualitative ordinal scale from 1 to 10 characterizing scratch resistance: a harder material can scratch a softer one. Introduced in 1822 by Friedrich Mohs, it remains widely used for mineral identification in the field, though it is not a precise quantitative measure.
Data available for 55 of 118 elements. Highest: Boron (9.3). Lowest: Cesium (0.2).