Final answer:
The statement is false; granite is indeed more common than rhyolite, which shares similar chemical and mineral properties but has a finer texture and different formation process.
Step-by-step explanation:
False. Granite is more common than rhyolite which is a type of felsic, extrusive igneous rock. Rhyolite has a similar chemical composition and mineralogy to granite, but presents a very fine crystalline texture, known as an aphanitic texture, due to the rapid cooling of high-viscosity lava. This contrasts with granite, which is an intrusive igneous rock with a coarser, phaneritic texture that cools slowly beneath the Earth's surface. Rhyolites are typically light gray, pinkish, or reddish in color and are characterized by their high viscosity, which can cause them to flow in a thick and slow-moving manner.
Granite, on the other hand, is one of the most abundant rocks in the Earth's continental crust. It forms from the slow cooling and solidification of magma deep beneath the Earth's surface, which results in its large visible crystals. As a fundamental component of continental crust, granite outcrops are common and widely utilized in construction and monuments, making it more frequently encountered than rhyolite.