* Intrusive Nature of Granite: Granite is an igneous rock that forms when magma cools and solidifies beneath the Earth's surface. This process often involves the intrusion of hot magma into existing rock layers.

* Heat from Granite: The hot magma within granite provides a significant source of heat to surrounding rocks. This heat can cause existing minerals within these rocks to recrystallize and change their texture, forming metamorphic rocks.

* Pressure from Granite: The intrusion of granite also applies pressure to surrounding rocks. This pressure, along with the heat, can cause existing minerals to rearrange and form new minerals, further contributing to the formation of metamorphic rocks.

In summary: The heat and pressure associated with the intrusion of granite create the perfect conditions for the transformation of existing rocks into metamorphic rocks. This is why metamorphic rocks are frequently found near granite formations.

Here are some examples of metamorphic rocks commonly found near granite:

* Schist: A metamorphic rock with a layered or foliated texture formed under high pressure and moderate temperature.

* Gneiss: A metamorphic rock with a banded texture formed under high pressure and high temperature.

* Marble: A metamorphic rock formed from limestone under heat and pressure, often found near granite intrusions.

The specific type of metamorphic rock that forms depends on the original rock type, the intensity of heat and pressure, and the time involved in the metamorphic process.