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Hardness of Minerals

 Hardness of Minerals In the category gold discovery more articles and learn more information about Hardness of Minerals Reviews Price Specifications Features Image manuals videos Accessories All this in metal detectors for gold.


Hardness of Minerals



Hardness of Minerals

In terms of reliability, hardness is one of the better physical properties for

minerals. Specimens of the same mineral may vary slightly from one to

another, but generally they are quite consistent. Inconsistencies occur when

the specimen is impure, poorly crystallized, or actually an aggregate and not

an individual crystal.


Hardness is one measure of the strength of the structure of the mineral

relative to the strength of its chemical bonds. Minerals with small atoms,

packed tightly together with strong covalent bonds throughout tend to be the

hardest minerals. The softest minerals have metallic bonds or even weaker

van der Waals bonds as important components of their structure. Hardness is

generally consistent because the chemistry of minerals is generally consistent.

Hardness can be tested through scratching. A scratch on a mineral is actually

a groove produced by microfractures on the surface of the mineral. A mineral

can only be scratched by a harder substance. A hard mineral can scratch a

softer mineral, but a soft mineral can not scratch a harder mineral (no matter

how hard you try). Therefore, a relative scale can be established to account

for the differences in hardness simply by seeing which mineral scratches

another. That is exactly what French mineralogist Friedrich Mohs proposed

almost one hundred and seventy years ago. The Mohs Hardness Scale starting

with Talc at 1 and ending with Diamond at 10, is universally used around the

world as a way of distinguishing minerals. Simply put; the higher the number, the

harder the mineral.


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