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Ferromagnesian silicates, which include minerals like olivine and pyroxene, contain significant amounts of iron and magnesium. These elements contribute to the minerals' darker colors and higher densities due to their heavier atomic weights. The presence of iron also imparts magnetic properties, as iron is a ferromagnetic element. Consequently, the combination of these factors leads to the characteristic dark, dense, and often magnetic nature of ferromagnesian silicates.

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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 characteristics do ferromagnesian minerals have in common?

Ferromagnesian minerals are rich in iron and magnesium, which give them dark colors like black, dark green, or brown. They are typically heavy, dense minerals with a high specific gravity. Additionally, ferromagnesian minerals often exhibit a distinct cleavage and are common in mafic igneous rocks like basalt and gabbro.


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