The salt crystals that we were trying to grow in our experiment attempted to simulate: biomineralization precipitation from solution solid state diffusion hardening from melt
The salt crystals that we were trying to grow in our experiment attempted to simulate: biomineralization precipitation from solution solid state diffusion hardening from melt
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
Problem 1LR
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Answer mutiple choice question below
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Step 1: Hardness of minerals
The Mohs mineral hardness scale, which gives different minerals a relative hardness value, is commonly used to measure the hardness of minerals. Friedrich Mohs created the scale in 1812, and its foundation is the idea that a tougher mineral can abrasively erode a softer mineral.
Here are the common minerals and their respective hardness values on the Mohs scale:
- Talc: Hardness of 1 - It can be easily scratched by a fingernail.
- Gypsum: Hardness of 2 - It can be scratched by a fingernail.
- Calcite: Hardness of 3 - It can be scratched by a copper penny.
- Fluorite: Hardness of 4 - It can be scratched by a knife blade.
- Apatite: Hardness of 5 - It can be scratched by a knife blade but not by a penny.
- Orthoclase Feldspar: Hardness of 6 - It can scratch glass.
- Quartz: Hardness of 7 - It can scratch glass.
- Topaz: Hardness of 8 - It can scratch quartz.
- Corundum: Hardness of 9 - It can scratch topaz.
- Diamond: Hardness of 10 - It is the hardest naturally occurring mineral and can scratch all other minerals.
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