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Silicate minerals are those composed of silicon and oxygen atoms. Some of these minerals are quartz, feldspar, mica and olivine.

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Laurence Aufderhar

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2y ago
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10y ago

Igneous rocks high in silica are usually light-colored

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14y ago

silicates contain silicon and oxygen

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Q: What are the silicates made of?
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Related questions

Are Most rocks made from silicates?

no


Are Most rocks are made from silicates.?

no


What is a name of a group of silicates made of a chalcedony?

Agate


What are the 2 man-made silicates?

The two main man-made silicates are glass and cement. Glass is made by melting sand and other ingredients together, while cement is produced by heating a mixture of limestone and clay to high temperatures.


What are the three classifications of sponges?

calcispongia----composed of calcium hyalospongia.....made of silicates demospongia....made of protein


What has the author I A Voinovitch written?

I. A. Voinovitch has written: 'L' analyse des silicates' -- subject(s): Silicates 'The analysis of silicates' -- subject(s): Silicates


What are the two major mineral grouped?

Silicates and non-silicates.


Is pumice inorganic?

Yes. Pumice is inorganic. It is a glassy volcanic rock made mostly of silicates.


What are the two most common kinds of minerals?

Silicates and non-silicates.


What is the difference ferromagnesian and non-ferromagnesian silicates?

Ferromagnesian silicates contain iron and magnesium in their composition, which gives them a dark color and high density. Non-ferromagnesian silicates do not contain iron and magnesium, resulting in lighter colors and lower densities. Ferromagnesian silicates tend to be denser and have higher melting points compared to non-ferromagnesian silicates.


What are Compound minerals made up of oxygen and silicon are called?

Compound minerals made up of oxygen and silicon are called silicates. Silicates are the most abundant group of minerals in the Earth's crust and are composed of silicon and oxygen tetrahedra. Examples of silicate minerals include quartz, feldspar, and mica.


How do sheet silicates differ from framework silicates?

Sheet silicates have a layered structure where silica tetrahedra are arranged in sheets with cations between the layers, while framework silicates have a three-dimensional network of silica tetrahedra connected in all directions. Sheet silicates have weaker bonds between layers, allowing for easier cleavage and flexibility, while framework silicates have stronger bonds, resulting in a more rigid structure.