MINERALS
Hardness
Click here to go back to the main page
Hardness is a measure of a mineral's resistant to abrasion. This property is easily determined and is used widely for field identification of minerals. More than a century ago. Friedrich Mohs (1773-1839), a German mineralogist, assigned arbitrary relative numbers to ten common minerals in order of their hardness.
|
Hardness
|
Mineral
|
Test
|
| 1 | Talc | Fingernail (2.5) |
| 2 | Gypsum | |
| 3 | Calcite | Cooper coin (3) |
| 4 | Flourite | Knife blade (5.5) |
| 5 | Apatite |
Glass plate (5.5+) |
| 6 | K-feldspar | |
| 7 | Quartz | Streak plate (7) |
| 8 | Topaz | |
| 9 | Corundum | |
| 10 | Diamond |
A simpler version of the Moh's scale can be established using three types of hardness:
SOFT - Minerals that can be scratched with a fingernail
INTERMEDIATE - Minerals that cannot be scratched with a fingernail but can be scratched with a steel nail.
HARD - Minerals that cannot be scratched with a steel nail.

|
Mineral
|
Hardness
|
|
Calcite
|
|
|
|
INTERMEDIATE Mineral cannot be scratched with a fingernail but can be scratched with a steel nail. |
|
Gypsum
|
|
|
|
SOFT Mineral can be scratched with a fingernail |
|
Pink
Feldspar
|
|
|
|
HARD Mineral cannot be scratched with a steel nail. |
|
White
Feldspar
|
|
|
|
HARD Mineral cannot be scratched with a steel nail. |
|
Gray
Feldspar
|
|
|
|
HARD Mineral cannot be scratched with a steel nail. |
|
Quartz
|
|
|
|
HARD Mineral cannot be scratched with a steel nail. |
Click here to go back to the main page
©David Leveson and David Seidemann - Brooklyn College - Earth and Environmental Sciences