Olivine would weather faster than quartz
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).
Quartz would be able to scratch fluorite, galena, and pyroxene as it is harder than these minerals on the Mohs scale of hardness.
feldspars. feldspars.
Quartz, with a hardness of 7, will scratch calcite, with a hardness of 3.
A non-metallic mineral such as quartz or calcite.
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).
They would include olivine, quartz, the feldspars, and the micas.
Quartz and olivine typically do not occur together in the same igneous rock. Quartz is commonly found in felsic rocks, which are rich in silica, while olivine is prevalent in mafic and ultramafic rocks, which have lower silica content and are rich in magnesium and iron. The contrasting mineral compositions reflect different cooling histories and magma compositions. Therefore, while both minerals can be found in igneous rocks, they are usually indicative of different rock types.
Igneous rocks typically form from the crystallization of magma, which has specific chemical compositions. Quartz, a silica-rich mineral, is usually found in felsic rocks, while olivine is a magnesium-iron silicate typically found in mafic rocks. The presence of both minerals in the same rock would indicate a divergent composition, as quartz forms at lower temperatures and olivine at higher temperatures. Consequently, the coexistence of these minerals suggests an unlikely cooling history, making such a rock rare or non-existent in nature.
One mineral that is not typically found in granite is olivine. Granite is primarily composed of quartz, feldspar, and mica, while olivine is more commonly associated with mafic and ultramafic igneous rocks, such as basalt and peridotite. Thus, olivine's presence in granite would be unusual.
Quartz would be able to scratch fluorite, galena, and pyroxene as it is harder than these minerals on the Mohs scale of hardness.
Chalk would weather fastest, followed by limestone.
feldspars. feldspars.
This would be quartz.
They would weather slower than on earth due to different amts of wind and rain than on earth.
Quartz is a mineral not a rock. Fossils can be found associated with quartz in sedimentary rock not inside the quartz.
Quartz