Mohs Hardness Scale Converter

Use this Mohs hardness scale converter to translate between the classic 1–10 Mohs scale and a more quantitative relative (absolute) hardness scale. Explore how hard common minerals and gemstones are, and compare their scratch resistance for geology, gemology and materials science applications.

This tool is designed for quick, educational conversions and field work. For critical engineering design, always rely on standardized hardness tests (Vickers, Rockwell, Brinell) performed on the actual material.

Interactive Mohs hardness converter

Conversion mode

You can enter decimal values (e.g. 6.5) to represent materials between two reference minerals.

Results

Mohs hardness (approx.):
Absolute hardness (approx.):
Classification:
Closest reference mineral:

Enter a value and click “Convert” to see the approximate hardness and closest Mohs reference mineral.

Important: This converter uses a reference table and simple interpolation. Values are indicative only and should not replace standardized hardness testing for critical design or certification.

Mohs hardness scale reference table

The table below lists the ten classic Mohs reference minerals, their hardness level and an approximate absolute hardness value used in this converter.

Mohs Reference mineral Approx. absolute hardness Typical use / notes
1 Talc 1 Very soft; marks easily with a fingernail.
2 Gypsum 2 Soft; can be scratched with a fingernail.
3 Calcite 14 Scratched by a copper coin; common in limestones.
4 Fluorite 21 Medium hardness; used in industry and optics.
5 Apatite 48 Benchmark for medium-hard minerals.
6 Orthoclase feldspar 72 Scratches glass; common rock-forming mineral.
7 Quartz 100 Very common; reference point for many abrasives.
8 Topaz 200 Hard gemstone; suitable for jewellery.
9 Corundum 400 Includes ruby and sapphire; used as an abrasive.
10 Diamond 1500 Extremely hard; cutting tools, high-wear applications.

Absolute hardness numbers are dimensionless values that reflect the relative gaps between Mohs levels. They are not a substitute for standardized indentation hardness tests but help visualize how hardness increases along the Mohs scale.

How the Mohs hardness scale works

The Mohs scale is an ordinal scratch scale from 1 (very soft) to 10 (very hard). A mineral with a higher Mohs number can visibly scratch one with a lower number. For example, quartz (7) can scratch orthoclase (6), but not corundum (9) or diamond (10).

Because the scale is ordinal, the gap between 9 and 10 is much larger than the gap between 3 and 4. In other words, diamond is far harder than corundum, even though their Mohs values differ by only one step.

Key idea:

If mineral A scratches mineral B, A is harder than B on the Mohs scale. If neither scratches the other, they have similar hardness.

Mohs hardness vs. engineering hardness tests

In materials science and mechanical design, hardness is usually measured with indentation tests such as Vickers, Rockwell or Brinell. These methods use a controlled load and an indenter geometry to measure how deeply a material is penetrated.

  • Mohs hardness: scratch test, quick and simple, qualitative and ordinal.
  • Vickers, Rockwell, Brinell: indentation tests, quantitative, tied to specific standards.

Because the test methods are very different, there is no single exact formula that converts Mohs hardness into engineering hardness numbers. The best you can do is use approximate correlations for a given class of materials (for example, steels or specific minerals).

Classification of materials by Mohs hardness

A very rough rule of thumb often used in geology and mineralogy is:

  • Soft: Mohs 1–2 (talc, gypsum)
  • Medium: Mohs 3–5 (calcite, fluorite, apatite)
  • Hard: Mohs 6–7 (orthoclase, quartz)
  • Very hard: Mohs 8–10 (topaz, corundum, diamond)

Our converter uses these ranges to display a plain-language classification for any entered value.

How to use this Mohs hardness converter in practice

1. Identifying unknown minerals

In the field, geologists often use a scratch kit or simple objects (fingernail, copper coin, steel knife, glass plate) to estimate Mohs hardness by trial and error. Once you have an approximate Mohs value, you can use this converter to:

  • see the closest reference mineral,
  • compare its absolute hardness with other minerals,
  • decide whether a sample is likely to scratch or be scratched by common materials.

2. Gemstone durability and jewellery design

Gemologists and jewellers use the Mohs scale to evaluate whether a gemstone is suitable for daily wear. As a very broad guideline:

  • Everyday rings and bracelets usually require gemstones around Mohs 7 or higher.
  • Softer stones (Mohs 5–6) may still be acceptable in protected settings such as earrings and pendants.
  • Very soft stones (Mohs < 5) are generally best reserved for occasional wear or collectors.

3. Abrasives and surface finishing

When selecting abrasives, coatings or cutting tools, you need a material that is harder than the workpiece. A quick Mohs comparison can help you decide whether a given mineral abrasive is appropriate before checking more precise data in engineering hardness scales.

Limitations and good practice

  • Mohs hardness is measured on ideal, pure crystals. Real-world rocks and industrial materials may behave very differently because they are mixtures or contain defects.
  • The converter’s absolute hardness numbers are approximate and should be used for comparison only, not for design calculations.
  • For critical applications (structural components, high-speed cutting tools, safety-relevant parts), always rely on certified hardness tests performed on the actual material grade.

Frequently asked questions about the Mohs hardness scale

What is the Mohs hardness scale?
The Mohs hardness scale is a simple ranking of minerals from 1 (very soft) to 10 (very hard) based on scratch tests. A harder mineral can scratch a softer one. It was introduced in the early 19th century and is still widely used in mineralogy and gemology.
Is Mohs hardness the same as Vickers or Rockwell hardness?
No. Mohs hardness is a qualitative scratch test, while Vickers, Rockwell and Brinell are quantitative indentation tests. They use different methods, units and scales. You can use charts and converters like this one to get approximate comparisons, but there is no single exact formula to go from Mohs to other hardness scales.
Why are the gaps between Mohs levels so uneven?
The Mohs scale is ordinal, not linear. The difference in hardness between 9 (corundum) and 10 (diamond) is much larger than between 3 (calcite) and 4 (fluorite). Absolute hardness numbers help visualize these uneven gaps.
Can I enter decimal Mohs values?
Yes. Many practical materials fall between two reference minerals. For example, a hardness around 6.5 is between orthoclase and quartz. The converter interpolates between the closest reference levels to provide an approximate absolute hardness.
Can this tool replace laboratory hardness testing?
No. This is an educational and quick-reference tool. For engineering or quality-critical applications, you should always rely on standardized hardness tests (Vickers, Rockwell, Brinell, Knoop, etc.) performed under controlled conditions on the actual material.