Molten minerals in magma crystallize when they have cooled sufficiently to reach their temperature range of crystallization. When all of the minerals have crystallized, the resultant product is an igneous rock. In an igneous rock like granite, the minerals in the magma crystallize at different temperatures and interlock, forming a very durable rock. Minerals in sedimentary rock are a product of sedimentation of particles of other rocks or solutions rich in minerals. These minerals in solution can bridge gaps between particles of rock (which themselves are composed of minerals), and cement the particles together, forming a rock. In metamorphic rocks, heat and pressure can alter the crystal and mineral structures of the parent rock. == Rocks are composedof Minerals, so any bunch of minerals is a rock, even if the rock is made of only one or more types of minerals.
So minerals don't become rocks. They just are (collectively) rocks.
it melts.
When metamorphic rocks are heated, the minerals within the rock may undergo recrystallization, transforming into new minerals. This process can lead to the development of new textures and structures in the rock. However, excessive heat can cause the minerals to melt and reform as igneous rocks.
Sedimentary rock becomes metamorphic rock when subjected to high temperatures and pressures. This process causes the minerals within the sedimentary rock to recrystallize and reorganize, resulting in a new rock with different characteristics.
Metamophic rock came from the volcano and it's part of rocks and minerals.
Metamorphic rocks with a layered or banded look are referred to as foliated.
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.
Metamorphic rock continues to heat and eventually melts and becomes igneous rocks.
Minerals may get changed to other minerals forming a new rock. Mineral grains also become aligned in response to the increased pressure.
I becomes sediments again or becomes igneous or metamorphic rock
In intense heat and pressure, igneous rock can undergo metamorphism, transforming into metamorphic rock. This process involves recrystallization of minerals, and the rock may develop foliation or banding patterns. The original texture and mineral composition of the rock can change as a result of this process.
Metamorphic rocks gain enegry as they are melted by magma and then lose energy as they cool into igneous rocks.
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.
Metamorphic rock becomes igneous rock when it is melted, then solidifies.
it melts.
If the metamorphic rock becomes hot enough it can melt.
heat and pressure is applied to the rock and it becomes a metamorphic rock.