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The cooling rate of the rock.
Cooling rate of molten rock
The cooling rate of magma plays a significant role in determining the size of crystals.
The slower the rate of cooling the larger the size of the crystals that can develop.
factors include: saturation, rate of cooling, temperature, and the crystal itself...
The slower the rate of cooling the larger the size of the crystals that can develop.
The cooling rate of the rock.
Primarily the cooling rate of the mineral compound.The faster the rate cooling smaller the crystal size of the mineral.Consequently, large crystal specimins are derived from igneous bodies with a very slow rate of cooling.
that means like when somthing is in a own properties
larger crystals
fast cooling rate forms smaller crystals eg Andesiteslow cooling rate forms large crystals eg.Pegmatite
The size of the crystals that do form are smaller/microscopic in that the time an temperature for crystals to grow is cut. The type of mineral that crystallizes is also effected,
Exposure, Particle size, mineral composition, & climate.
Temperature doesn't really affect the crystal size; the rate of cooling is the major factor. The faster the mineral, rock, etc. (whatever has the crystals) cools, the smaller the crystals- the slower the larger. If you were "growing" crystals with a set, the warmer the temperature generally means the larger the crystals.
The rate at which magma cools determines the size of the mineral crystal.
Grain size depends upon the cooling rate as written below: 1. longer the time it takes to cool, larger will be the grain size and vice versa
When igneous rocks cool quickly, they have small crystals and have a texture that may be described as aphanitic. When igneous rocks cool slowly, they have much larger crystals and have a texture that may be described as phaneritic or pegmatitic.