Mohs Hardness Relative Scaling
Estimates absolute harness based on the non-linear Mohs scale.
This public page keeps the free explanation visible and leaves premium worked solving, advanced walkthroughs, and saved study tools inside the app.
Core idea
Overview
This empirical formula provides a mathematical approximation for converting the qualitative Mohs scale of mineral hardness into a quantitative absolute value. It illustrates that mineral hardness increases exponentially rather than linearly as the scale rank progresses.
When to use: Apply this formula when you need to estimate relative quantitative hardness from a qualitative Mohs rank. It is useful for material science comparisons where precise laboratory testing like Vickers or Knoop is unavailable.
Why it matters: The Mohs scale is not linear; for example, the hardness gap between Corundum (9) and Diamond (10) is much larger than between Talc (1) and Gypsum (2). This formula helps engineers understand the exponential energy and wear requirements for processing harder minerals.
Symbols
Variables
= Approx Absolute Hardness, M = Mohs Scale Rank
Walkthrough
Derivation
Understanding the Mohs Hardness Scale
The Mohs scale ranks mineral hardness from 1 (talc) to 10 (diamond), but the scale is non-linear in terms of absolute hardness.
- The empirical approximation bs ≈ 2^(M/2) estimates relative absolute hardness.
- Scratch resistance is used as the test.
The Mohs scale is ordinal, not linear:
Each step means one mineral can scratch the one below, but the hardness jumps are unequal.
Approximate absolute hardness:
This exponential approximation captures the non-linear spacing. Diamond (M = 10) is vastly harder than corundum (M = 9) in absolute terms.
Note: Practical tests: fingernail ≈ 2.5, copper coin ≈ 3.5, glass ≈ 5.5, steel file ≈ 6.5.
Result
Source: A-Level Geology — Mineralogy
Visual intuition
Graph
Graph unavailable for this formula.
The graph displays an exponential curve where the independent variable is plotted on the X-axis and the approximate hardness (HABS) on the Y-axis. Because the variable appears in the exponent, the curve rises at an increasing rate as the X-axis value grows. The function has a positive Y-intercept at 1 and no horizontal asymptotes.
Graph type: exponential
Why it behaves this way
Intuition
A staircase where each step is significantly taller than the one before it, representing how the physical resistance to scratching accelerates as you move toward diamond.
Signs and relationships
- M/2: The positive exponent indicates that absolute hardness grows exponentially with the Mohs rank, reflecting that the physical effort to scratch a mineral increases drastically at higher levels.
Free study cues
Insight
Canonical usage
This equation converts a dimensionless Mohs hardness rank into a dimensionless relative absolute hardness value.
Common confusion
A common mistake is to assume the Mohs scale is linear or to mistake the dimensionless output of this formula for a physical hardness value with units (e.g., Vickers or Knoop hardness in MPa or kgf/mm2).
Dimension note
Both the input Mohs hardness (M) and the output estimated absolute hardness () are dimensionless quantities in this formula, representing relative indices rather than physical units.
Unit systems
Ballpark figures
- Quantity:
One free problem
Practice Problem
Quartz has a Mohs hardness of 7. Using the relative scaling formula, calculate its approximate absolute hardness (HABS).
Solve for: HABS
Hint: Divide the Mohs rank by 2 and then use that result as the exponent for the base 2.
The full worked solution stays in the interactive walkthrough.
Where it shows up
Real-World Context
In a chemistry investigation involving Mohs Hardness Relative Scaling, Mohs Hardness Relative Scaling is used to calculate Approx. Hardness from Mohs Scale Rank. The result matters because it helps connect measured amounts to reaction yield, concentration, energy change, rate, or equilibrium.
Study smarter
Tips
- Divide the Mohs rank by two before calculating the exponent.
- Use the base-2 logarithm to reverse the formula when starting with absolute hardness.
- Treat results as approximations, as the Mohs scale is inherently an ordinal ranking system.
Avoid these traps
Common Mistakes
- Assuming Mohs 8 is 'twice as hard' as Mohs 4. It's an ordinal rank, not a linear scale.
- Convert units and scales before substituting, especially percentages, time units, or powers of ten.
- Interpret the answer with its unit and context; a percentage, rate, ratio, and physical quantity do not mean the same thing.
Common questions
Frequently Asked Questions
The Mohs scale ranks mineral hardness from 1 (talc) to 10 (diamond), but the scale is non-linear in terms of absolute hardness.
Apply this formula when you need to estimate relative quantitative hardness from a qualitative Mohs rank. It is useful for material science comparisons where precise laboratory testing like Vickers or Knoop is unavailable.
The Mohs scale is not linear; for example, the hardness gap between Corundum (9) and Diamond (10) is much larger than between Talc (1) and Gypsum (2). This formula helps engineers understand the exponential energy and wear requirements for processing harder minerals.
Assuming Mohs 8 is 'twice as hard' as Mohs 4. It's an ordinal rank, not a linear scale. Convert units and scales before substituting, especially percentages, time units, or powers of ten. Interpret the answer with its unit and context; a percentage, rate, ratio, and physical quantity do not mean the same thing.
In a chemistry investigation involving Mohs Hardness Relative Scaling, Mohs Hardness Relative Scaling is used to calculate Approx. Hardness from Mohs Scale Rank. The result matters because it helps connect measured amounts to reaction yield, concentration, energy change, rate, or equilibrium.
Divide the Mohs rank by two before calculating the exponent. Use the base-2 logarithm to reverse the formula when starting with absolute hardness. Treat results as approximations, as the Mohs scale is inherently an ordinal ranking system.
References
Sources
- Britannica: Mohs scale
- Wikipedia: Mohs scale of mineral hardness
- Klein & Hurlbut: Manual of Mineralogy
- Manual of Mineralogy by Cornelis Klein and Barbara Dutrow (23rd Edition)
- Earth Materials: Introduction to Mineralogy and Petrology by Cornelis Klein and Anthony Philpotts (2nd Edition)
- A-Level Geology — Mineralogy