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The Mohs scale is a scale of mineral hardness that was devised by Friedrich Mohs in 1812. It categorizes minerals based on their ability to scratch one another, with each mineral assigned a value from 1 to 10. The scale is ordinal, meaning that the numbers indicate a relative hardness but do not convey precise differences in hardness.

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  1. Materials science
  2. Applied and interdisciplinary physics
  3. Subfields of physics
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