Rhyolite is an igneous rock that is high in silica content, typically greater than 70%, and is characterized by its light color and fine-grained texture. It forms from the rapid cooling of lava at or near the Earth's surface, leading to the formation of glassy and volcanic textures. Rhyolite is closely linked to explosive volcanic eruptions, where gas-rich magma generates powerful outbursts, producing significant pyroclastic materials.