* Phaneritic rocks have crystals that are large enough to be seen with the naked eye. These crystals form when magma cools slowly, allowing ample time for the mineral crystals to grow.
* Aphanitic rocks, on the other hand, have very small crystals (microscopic) that form when lava cools quickly.
Examples of phaneritic igneous rocks:
* Granite: A light-colored, coarse-grained rock with large crystals of quartz, feldspar, and mica.
* Gabbro: A dark-colored, coarse-grained rock with large crystals of pyroxene and plagioclase feldspar.
So, the answer is: A phaneritic igneous rock.
