Metamorphic foliation is layering in metamorphic rock. The layers can be very thin, or they can be a meter thick,
presence of platy mineral and orientation stress can give foliation to a metamorphic rocks.
The thin flat layering found in most metamorphic rocks is called foliation
a rock with metamorphic minerals but no foliation or lineation
The main way metamorphic rocks are classified is by the presence or absence of foliation. Foliated metamorphic rocks are distinguished by the type of foliation they exhibit. Types of foliation textures, include: slaty, phyllitic, schistose, and gneissi.
Not exactly. Some metamorphic rocks have foliation, which can appear similar to the layers of sedimentary rock. Foliation develops from mineral grains being oriented by pressure, rather than the deposition of layers.
presence of platy mineral and orientation stress can give foliation to a metamorphic rocks.
Metamorphic rocks often have foliation. Schist is a common example.
The thin flat layering found in most metamorphic rocks is called foliation
Metamorphic rocks that do not exhibit foliation.
Foliation
Foliation is the layering of metamorphic rock. An example of foliation would be a rock called a Gneiss. On this rock, it is easily apparent to see the layers of rock that have formed.
A metamorphic rock will display foliation or bands around the rock.
No. Non-foliated metamorphic rocks include quartzite and marble.
No. The layering or foliation only occurs when there is a variation in the composition of the original rock. If the rock is homogeneous, then there will be no foliation.
The foliation in metamorphic minerals is always perpendicular to the direction of pressure. E.g. Vertical pressure is applied, the foliation will be horizontal, and vice-versa, the pressure is horizontal you get vertical foliation. From yahoo answers
a rock with metamorphic minerals but no foliation or lineation
Schists are metamorphic rocks with parallel alignment of minerals.