Final answer:
A pegmatitic texture in igneous rocks, which features very large crystals, is formed when magma cools slowly underground, resulting in intrusive or plutonic rocks like granite.
Step-by-step explanation:
The scenario that will most likely result in the formation of an igneous rock with a pegmatitic texture is magma taking an extremely long time to cool underground. A pegmatitic texture is characterized by very large crystals, indicating that the magma had enough time to cool slowly and allow the crystal grains to grow to a substantial size. This slow cooling process occurs when magma is trapped beneath the Earth's surface, leading to the formation of intrusive or plutonic igneous rocks, such as granite.