because rholite forms outside a volcano and granite forms inside the volcano
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The texture of rhyolite is fine-grained due to its rapid cooling at the Earth's surface, whereas granite has a coarse-grained texture because it cools slowly deep underground. The different cooling rates lead to variations in crystal size and arrangement, giving each rock its distinctive texture.
The volcanic equivalent of granite is rhyolite. Both granite and rhyolite are composed mainly of light-colored minerals such as quartz and feldspar, but rhyolite forms from volcanic magma that cools quickly at the Earth's surface, resulting in a fine-grained texture.
Rhyolite is a fine-grained, extrusive igneous rock with high silica content, while granite is a coarse-grained, intrusive igneous rock also rich in silica but with larger crystals. Rhyolite forms from cooled lava flows on the Earth's surface, while granite forms from slowly cooling magma beneath the surface.
Diorite is a rock that has a composition similar to granite, but with a different texture. Both rocks are composed mainly of quartz, feldspar, and mica minerals. Diorite is typically darker in color and has a coarser grain size compared to granite.
Rhyolite has a finer-grained texture compared to granite because it cools relatively quickly at or near the Earth's surface, forming smaller crystals. Granite, on the other hand, cools slowly deep underground, allowing larger crystals to form. This difference in cooling rates results in distinct textures for each rock type.
The extrusive counterpart of granite is rhyolite. Rhyolite is an igneous rock that forms from the rapid cooling of magma at the surface of the Earth, just like granite does below the surface.