Yes, the other type is a foliate rock with bands of minerals.
The Texture term for metamorphic rock which are not banded or layered is non-foliated metamorphic rock. Good examples are marble and quartzite.
Lack of banding
Marble is a metamorphic rock that is massive and lacks banding. It forms from the recrystallization of limestone and is composed mostly of the mineral calcite. Marbles are often used in architecture and sculpture due to their aesthetic qualities.
Soapstone is a nonfoliated metamorphic rock. It forms from the metamorphism of protoliths such as dolomite or steatite and does not exhibit the characteristic layering or banding of foliated rocks like slate or schist.
Quartzite
The Texture term for metamorphic rock which are not banded or layered is non-foliated metamorphic rock. Good examples are marble and quartzite.
Lack of banding
nonfoliated rocks
Marble is a metamorphic rock that is massive and lacks banding. It forms from the recrystallization of limestone and is composed mostly of the mineral calcite. Marbles are often used in architecture and sculpture due to their aesthetic qualities.
Soapstone is a nonfoliated metamorphic rock. It forms from the metamorphism of protoliths such as dolomite or steatite and does not exhibit the characteristic layering or banding of foliated rocks like slate or schist.
Quartzite
Metamorphic rock displaying banding is referred to as foliated metamorphic rock.
Slate is a foliated metamorphic rock.
Quartzite, Marble, and Soapstone are three examples of nonfoliated rock.
No banding or alignment of a metamorphic rock's minerals would be consider non-foliated.
Quartzite is a nonfoliated metamorphic rock that is granular and composed mainly of quartz. It forms from the metamorphism of quartz-rich sandstone.
The two groups of metamorphic rock are foliated and nonfoliated. Metamorphic rocks can also be classified as contact and regional.