no it doesnt
Olivine and quartz are rarely found together in igneous rocks due to their differing crystallization conditions and compositions. Olivine typically forms at higher temperatures in mafic and ultramafic magmas, while quartz crystallizes at lower temperatures in more silica-rich, felsic magmas. The presence of olivine usually indicates a more magnesium- and iron-rich environment, whereas quartz is associated with more silicon-rich compositions, making their coexistence in the same rock highly unlikely.
Olivine does not contain Gabbro. Gabbro can contain olivine. Usually no more than a few percent.
As igneous rocks become more felsic, their density generally decreases. Felsic rocks, which are rich in silica and contain lighter minerals such as quartz and feldspar, tend to have lower specific gravities compared to mafic rocks that are richer in heavier minerals like olivine and pyroxene. Consequently, the overall density of the rock diminishes as the composition shifts towards more felsic minerals.
No. Silicon is the element. Silica is the compound silicon dioxide.
No, olivine and pyroxene are more commonly found in mafic rocks due to their high iron and magnesium content. Felsic rocks, on the other hand, typically contain minerals like quartz, feldspar, and mica, which have lower iron and magnesium content.
Quartz and olivine have different crystallization temperatures, with olivine forming at higher temperatures than quartz. This means that in most cases, olivine and quartz are not typically found together in the same igneous rock as they would have crystallized at different stages in the cooling process. Olivine is a common mineral in mafic rocks (rich in magnesium and iron) while quartz is more common in felsic rocks (rich in silica).
Olivine and quartz are rarely found together in igneous rocks due to their differing crystallization conditions and compositions. Olivine typically forms at higher temperatures in mafic and ultramafic magmas, while quartz crystallizes at lower temperatures in more silica-rich, felsic magmas. The presence of olivine usually indicates a more magnesium- and iron-rich environment, whereas quartz is associated with more silicon-rich compositions, making their coexistence in the same rock highly unlikely.
Following Goldich Dissolution Series (Or going backwards by Bowen's Reaction Series), olivine weathers before Quartz. Quartz has a framework silicate structure and olivine has a isolated silicate structure.
Olivine would weather faster than quartz because it is less stable chemically and more prone to reactions with water and acids from the environment. Quartz, being a more resistant mineral, is more durable and less susceptible to weathering processes.
Olivine does not contain Gabbro. Gabbro can contain olivine. Usually no more than a few percent.
Olivine weathers faster than quartz because it is less chemically stable when exposed to water and carbon dioxide in the atmosphere, leading to faster breakdown and weathering processes. Olivine is also more susceptible to chemical reactions and alteration compared to quartz, which is a more inert and resistant mineral.
If lava contains quartz that means the silica content is high. A high silica content makes lava more viscous, and gives it the tendency to erupt explosively.
They are classified as silicates, one of the more common being the mineral quartz which is composed only of the elements silicon and oxygen (SiO2). Other silicate minerals may include one or more other elements as well in their chemical formula.
No because, Like fossil fuels, silica (found in the world's sands and quartz) is a non-renewable, finite resource. However, silica is a far more plentiful resource.
No. Silicon is the element. Silica is the compound silicon dioxide.
A rock with more silica is likely to be lighter in color, such as light gray or white, due to the presence of minerals like quartz. In contrast, a rock with less silica tends to be darker, as it is typically composed of minerals like mafic minerals (e.g., biotite, amphibole) that give it a darker hue.
No, olivine and pyroxene are more commonly found in mafic rocks due to their high iron and magnesium content. Felsic rocks, on the other hand, typically contain minerals like quartz, feldspar, and mica, which have lower iron and magnesium content.