Quartz crystal

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-Quartz (from German Quarz) is the second most abundant mineral in the Earth's continental crust (after feldspar). It is made up of a continuous framework of SiO4 silicon-'''[[oxygen]]''' tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall formula '''SiO2'''.+[[Image:Quartz Crystal Timing.jpg|'''[[Quartz crystal]]''' (from German Quarz) is the second most abundant mineral in the Earth's continental crust (after feldspar). It is made up of a continuous framework of SiO4 silicon-'''[[oxygen]]''' tetrahedra, with each '''[[oxygen]]''' being shared between two tetrahedra, giving an overall formula '''SiO2'''.|thumb|300px]]
-== Also See: ==+'''[[Quartz crystal]]''' (from German Quarz) is the second most abundant mineral in the Earth's continental crust (after feldspar). It is made up of a continuous framework of SiO4 silicon-'''[[oxygen]]''' tetrahedra, with each '''[[oxygen]]''' being shared between two tetrahedra, giving an overall formula '''SiO2'''.
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 +== '''Also See:''' ==
*'''[[Freestyle Timing Booklet]]''' *'''[[Freestyle Timing Booklet]]'''

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Quartz crystal (from German  Quarz) is the second most abundant mineral in the Earth's continental crust (after feldspar). It is made up of a continuous framework of SiO4 silicon-oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall formula SiO2.
Quartz crystal (from German Quarz) is the second most abundant mineral in the Earth's continental crust (after feldspar). It is made up of a continuous framework of SiO4 silicon-oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall formula SiO2.


Quartz crystal (from German Quarz) is the second most abundant mineral in the Earth's continental crust (after feldspar). It is made up of a continuous framework of SiO4 silicon-oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall formula SiO2.


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