because the magma does not have as much time for crystals to form inside the igneous rock therefor it is a fine-grained rock
They may be smooth and others may be rough. Smoothness/roughness is not a defining characteristic for igneous rocks.
Igneous rocks that form above the earth's surface are called extrusive igneous rocks. These rocks cool and solidify quickly due to the rapid cooling environment of the Earth's surface, resulting in fine-grained textures. Examples include basalt and rhyolite.
in geology
Igneous rocks that form from magma that reaches the surface of the Earth are called extrusive or volcanic rocks. Examples include basalt, andesite, and rhyolite. These rocks cool quickly and have fine-grained textures due to rapid solidification.
Igneous rocks form when magma cools and solidifies either beneath the Earth's surface (intrusive igneous rocks) or on the surface after a volcanic eruption (extrusive igneous rocks). This cooling process can occur slowly, resulting in larger crystals (coarse-grained rocks), or quickly, which produces smaller crystals or glassy textures (fine-grained rocks).
They may be smooth and others may be rough. Smoothness/roughness is not a defining characteristic for igneous rocks.
hard rough and not smooth
Igneous rocks that cool quickly on the Earth's surface are called extrusive or volcanic rocks. Examples include basalt, obsidian, and pumice. These rocks have fine-grained textures due to their rapid cooling.
Igneous rocks formed at the Earth's surface are called extrusive igneous rocks. They form when magma cools and solidifies quickly on the Earth's surface, resulting in fine-grained or glassy textures. Examples include basalt and rhyolite.
Igneous rocks that form above the earth's surface are called extrusive igneous rocks. These rocks cool and solidify quickly due to the rapid cooling environment of the Earth's surface, resulting in fine-grained textures. Examples include basalt and rhyolite.
in geology
Igneous rocks that form from magma that reaches the surface of the Earth are called extrusive or volcanic rocks. Examples include basalt, andesite, and rhyolite. These rocks cool quickly and have fine-grained textures due to rapid solidification.
Igneous rocks form when magma cools and solidifies either beneath the Earth's surface (intrusive igneous rocks) or on the surface after a volcanic eruption (extrusive igneous rocks). This cooling process can occur slowly, resulting in larger crystals (coarse-grained rocks), or quickly, which produces smaller crystals or glassy textures (fine-grained rocks).
Extrusive igneous rocks are formed from lava that cools quickly on the Earth's surface, resulting in fine-grained textures. Intrusive igneous rocks are formed from magma that cools slowly beneath the Earth's surface, resulting in coarse-grained textures.
Igneous rocks that cool quickly below the Earth's surface are known as extrusive rocks or volcanic rocks. Examples include basalt, andesite, and rhyolite. These rocks typically have fine-grained textures due to rapid cooling.
Even in the most generalized classification, more than two igneous rocks have phaneritic textures. In that generalized classification, they are granite, diorite, gabbro, and peridotite.
Igneous rocks that cool quickly on the surface are known as extrusive or volcanic rocks. Examples include basalt, andesite, and rhyolite. These rocks have fine-grained textures due to their rapid cooling process.