The Mohs scale of mineral hardness characterizes the scratch resistance of various
minerals through the ability of a harder material to scratch a softer material. It was created in
1812 by the German
mineralogist Friedrich Mohs and is one of several definitions of
hardness in
materials science.Mohs based the scale on ten minerals that are all readily available. As the hardest known naturally occurring substance, diamond is at the top of the scale. The hardness of a material is measured against the scale by finding the hardest material that the given material can scratch, and/or the softest material that can scratch the given material. For example, if some material is scratched by apatite but not by fluorite, its hardness on the Mohs scale would fall between 4 and 5.
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