Mohs Hardness Scale Testing

Mineral Hardness • Testing Methods • Identification

[Placeholder: Mohs Hardness Scale Diagram]

The Mohs Hardness Scale is one of the most fundamental tools in mineral identification. Developed by German geologist Friedrich Mohs in 1812, this scale measures a mineral's resistance to scratching relative to other common minerals.

Understanding the Mohs Scale

The Mohs scale is a relative scale from 1 (softest) to 10 (hardest), with each number representing a specific mineral. A mineral can scratch any other mineral with a lower number on the scale.

Hardness Mineral Common Objects with Similar Hardness
1 Talc Fingernail (2.5)
2 Gypsum
3 Calcite Copper coin (3.5)
4 Fluorite Iron nail (4.5)
5 Apatite Glass (5.5-6.0)
6 Orthoclase Feldspar Steel file (6.5)
7 Quartz
8 Topaz
9 Corundum Sapphire and ruby (varieties of corundum)
10 Diamond

How to Perform a Hardness Test

1. Gather Your Materials

2. Conduct the Test

To determine a mineral's hardness:

  1. Select a sharp corner of the test object (or known hardness mineral)
  2. Gently but firmly scratch the surface of the unknown mineral
  3. Examine the result: if the unknown mineral is scratched, it has a lower hardness than the test object; if the test object leaves no mark, the unknown mineral has a higher hardness
  4. Repeat with objects of increasing or decreasing hardness to narrow down the range

3. Tips for Accurate Testing

Why Hardness Testing Matters

Hardness is one of the most reliable physical properties for mineral identification. It helps geologists and collectors quickly narrow down the possibilities when examining unknown specimens. In addition, a mineral's hardness provides clues about its atomic structure and can help determine its potential uses in industry.

Limitations of the Mohs Scale

While extremely useful, the Mohs scale has some limitations:

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