The existing minerals are re-formed by the heat and pressure into a new assembly of minerals, at least in part to minimize the volume. The new minerals will crystallize out at their natural freezing points, and some of the micas are the last to crystallize out.
The time of this terminal event is taken as the age of the rock or of that metamorphic event.
minerals are lined up
Metamophic rock came from the volcano and it's part of rocks and minerals.
Minerals may get changed to other minerals forming a new rock. Mineral grains also become aligned in response to the increased pressure.
Minerals may get changed to other minerals forming a new rock. Mineral grains also become aligned in response to the increased pressure.
Minerals may get changed to other minerals forming a new rock. Mineral grains also become aligned in response to the increased pressure.
Sandstone is a sedimentary rock
foliations and lineations
If the percentage of felsic minerals in a rock increases, the rock will become lighter in color and less dense. Felsic minerals are rich in silica and aluminum, so the rock may also become more viscous when melted. Additionally, the rock's melting temperature may decrease.
melt (magma or lava)
boob
boob
I becomes sediments again or becomes igneous or metamorphic rock