Foliated or nonfilated
crystals
Metamorphic rocks in which the minerals show no alignment are called non-foliated metamorphic rocks.
its foliated
Schists are metamorphic rocks with parallel alignment of minerals.
foliated metamorphic rocks. The alternating layers are caused by the alignment and segregation of minerals during the metamorphic process, resulting in a banded or layered appearance. Examples of foliated metamorphic rocks include gneiss, schist, and slate.
crystals
Metamorphic rocks in which the minerals show no alignment are called non-foliated metamorphic rocks.
A mineral alignment is a layered arrangement of firmly joined crystals of minerals; the minerals are aligned in layers or bands.
its foliated
its foliated
No banding or alignment of a metamorphic rock's minerals would be consider non-foliated.
Schists are metamorphic rocks with parallel alignment of minerals.
Heat is one condition that is required to form parallel alignment of minerals sometimes found in a metamorphic rock. The other condition is pressure.
The rate at which magma cools determines the size of the mineral crystal.
foliated metamorphic rocks. The alternating layers are caused by the alignment and segregation of minerals during the metamorphic process, resulting in a banded or layered appearance. Examples of foliated metamorphic rocks include gneiss, schist, and slate.
Crystals are the form that minerals take upon solidification. Metamorphic is a term used to describe a rock that undergoes a chemical or mineral transformation from heat or pressure. New crystals can form in rock undergoing metamorphosis, but the crystals themselves are not considered metamorphic.
If by particles you mean the size of the crystals, then the crystals in metamorphic rock are often larger than in the sedimentary rock. High heat and pressure can cause the minerals to recrystallize. This would be the case in the metamorphosis of limestone (sedimentary) to marble (metamorphic).