Here's why:
* Porphyritic texture: This texture is characterized by the presence of large crystals (called phenocrysts) embedded in a matrix of smaller crystals (called groundmass).
* Formation: Porphyritic rocks form when magma cools slowly, allowing large crystals to grow. Then, the magma cools more rapidly, resulting in the formation of smaller crystals in the groundmass.
Example: Granite is a common example of a porphyritic igneous rock. It often features large quartz and feldspar crystals embedded in a finer-grained matrix of other minerals.