Actually, quartz is one of the last minerals to cool under the surface. Because of this, the quartz tends to fill in all of the empty spaces in the solidfying magma, causing it to often come out in flakes, or oddly shaped chunks. Not all igneous rocks cool slowly, and this factor is just dependent on whether or not the rock is intrusive (still under ground) or extrusive (above or near the surface). Because obviously if a rock is underground, with all of the hot magma, it is going to take thousands of years for it to cool completely. While the air of the atmosphere that humans live in is way cooler than underground, so obviously it is going to take less time to cool it. So in closing, it just depends where the quartz is at in the Earth's crust. But, if it is in the Earth's crust, it usually is one of the last minerals to cool, making quartz unique.
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Quartz forms over thousands to millions of years, depending on the geological conditions present during its formation. In some cases, quartz can form relatively quickly in hydrothermal environments, while in other cases, it may take much longer in pegmatites or granite formations.
That depends on the rate of cooling, which depends on temperature. This also affects crystal size. Also note that relative to other minerals, Quartz cools first on average, hence the large crystals in Granite.
it depends on what type it is and the structure and the way you make it grow all crystals never have the same growing time line
Quartz and feldspar are two common minerals that form rocks. Quartz is often found in granite while feldspar is found in both granite and basalt.
Quartz crystals range in size from cryptocrystalline (difficulty in observing even with microscopes) to gigantic. The largest individual quartz crystal recorded weighed more than 96,000 pounds and was roughly 20 feet in length.
Quartz can be present in igneous rocks if it crystallizes from magma during the cooling process. In sedimentary rocks, quartz can be derived from the weathering and erosion of pre-existing rocks rich in quartz, transported and deposited as sediment, and then cemented together to form the sedimentary rock.
Oxygen is found in the Earth's atmosphere, in water, and in the Earth's crust in the form of minerals like quartz and oxides. Silicon is commonly found in the Earth's crust in the form of silicate minerals, sand, and rocks like granite and quartz.
The most common end product of the chemical weathering of quartz is clay minerals. Clay minerals form due to the breakdown of the silicon and oxygen in quartz when exposed to water and carbon dioxide, leading to the transformation of quartz into the softer clay minerals.