Heat is one condition that is required to form parallel alignment of minerals sometimes found in a metamorphic rock. The other condition is pressure.
They form when layers of minerals lay on top of each other
Minerals can form in metamorphic rock from the loss of water during compression. Hydrous minerals are replaced with non-hydrous minerals.
A mineral alignment is a layered arrangement of firmly joined crystals of minerals; the minerals are aligned in layers or bands.
It is more likely that igneous and metamorphic, or igneous and sedimentary rocks would have something in common than sedimentary and metamorphic. The reason is because the processes involved in making metamorphic rocks is completely different than the processes needed to make sedimentary rocks. Only high temperature, high pressure minerals such as olivine, pyroxene, amphibole can withstand these kinds of conditions. Take quartz and feldspar, two of the most abundant minerals found in sedimentary rocks, these minerals would not be found in abundance in metamorphic rocks because they are not high temperature, high pressure rocks. But the most simple answer is that all the major groups of rocks are made of minerals. Metamorphic has high pressure and Igneous does to and both made from a particle called magma.
The answer is Foliation.
Metamorphic rocks in which the minerals show no alignment are called non-foliated metamorphic rocks.
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.
Foliated or nonfilated
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.
They form when layers of minerals lay on top of each other
They form when layers of minerals lay on top of each other
They form when layers of minerals lay on top of each other
Earth movements form metamorphic rocks by pressing, squeezing, and folding. Sometimes minerals are destroyed and new minerals are created
parallel alignment of minerals that have been subjected to stress