Where is Quartz in host rock found?
SiO2 in igneous or metamorphic rock
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Open the appQuartz in host rock occurs in specific geological environments. Knowing where to look, and in what kind of rock, is the difference between going home empty-handed and finding a great specimen.
Where to find Quartz in host rock
Worldwide
Quartz is one of the most abundant minerals in the Earth's crust and is found in igneous and metamorphic rocks on every continent. Significant occurrences include the Appalachian Mountains (USA), Rocky Mountains (USA), Brazilian Shield, Scandinavian Shield, Himalayas, and various mountain ranges and cratons globally.
Collecting tips
- Look for glassy grains. In igneous and metamorphic rocks, quartz often stands out as glassy, colorless to gray grains that lack cleavage and exhibit a conchoidal fracture when broken.
- Test hardness. Quartz has a Mohs hardness of 7, meaning it will scratch glass and most common minerals. This is a key diagnostic property.
- Observe crystal habit. While often anhedral in host rocks, look for hexagonal crystal forms in vugs or pegmatitic environments within igneous rocks, or elongated lenses in highly deformed metamorphic rocks.
- Consider the host rock type. Quartz is a primary component of felsic igneous rocks (e.g., granite) and a major constituent of many metamorphic rocks (e.g., quartzite, gneiss). Its presence helps classify the host rock.
Quick Check
- Color:
- Colorless, white, gray, or various other colors due to impurities.
- Luster:
- Vitreous (glassy) to greasy.
- Streak:
- White (as it is harder than the streak plate).
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