The two metamorphic rocks that typically exhibit the largest crystals are gneiss and schist. Gneiss often features large, visible grains of quartz and feldspar, while schist is characterized by its shiny, platy minerals like mica that can form significant crystal sizes. These large crystals usually develop in environments with high temperatures and pressures, allowing minerals to grow and recrystallize.
Crystals can have different sizes due to differences in their growth conditions, such as temperature, pressure, and rate of crystal growth. Factors like nucleation sites, impurities, and crystal lattice structure can also influence crystal size. These variations in growth conditions can lead to crystals with different sizes within the same sample.
Such rocks are porphyritic.
Porphyritic
Gneiss usually consists of visible crystals of aligned mineral assemblages.
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The two metamorphic rocks that typically exhibit the largest crystals are gneiss and schist. Gneiss often features large, visible grains of quartz and feldspar, while schist is characterized by its shiny, platy minerals like mica that can form significant crystal sizes. These large crystals usually develop in environments with high temperatures and pressures, allowing minerals to grow and recrystallize.
Fine, crystals less than 1mm
Crystals can have different sizes due to differences in their growth conditions, such as temperature, pressure, and rate of crystal growth. Factors like nucleation sites, impurities, and crystal lattice structure can also influence crystal size. These variations in growth conditions can lead to crystals with different sizes within the same sample.
A Gneiss is a Metamorphic rock
Gneiss is foliated.
Such rocks are porphyritic.
Gneiss is foliated and coarse grained
Gneiss is a rock, not a mineral.
No, gneiss is metamorphic.
Gneiss is a part of the earths lower crust. No matter where you drill you will eventually uncover gneiss.
Yes, rocks can contain a variety of crystal sizes.