The texture of an igneous rock, specifically its crystal size and arrangement, provides crucial information about the environment in which it solidified. Coarse-grained textures indicate slow cooling, typically occurring in intrusive environments beneath the Earth's surface, while fine-grained textures suggest rapid cooling, often associated with extrusive environments like volcanic eruptions. Additionally, the presence of certain minerals can hint at the chemical composition of the magma and the conditions under which it formed.
igneous rock
igneous rocks are made of solidified lava.
Igneous rocks are formed from melted rock that has cooled and solidified. Examples include granite, basalt, and obsidian.
Such rock is referred to as plutonic igneous rock if it is part of a large solidified mass of magma at large depths in the crust, or as intrusive igneous rock if simply solidified at some depth within the crust. Plutonic igneous rock is therefore a type of intrusive igneous rock.
Uplift and solidification
Solidified magma or lava is igneous rock.
igneous rock
Igneous rock is formed from solidified and cooled magma or lava.
igneous rocks are made of solidified lava.
Solidified magma or lava.
Igneous rocks are formed from melted rock that has cooled and solidified. Examples include granite, basalt, and obsidian.
It's called extrusive igneous rock--rapidly solidified lava.
Intrusive igneous rock.
The igneous rock is formed when a rock that is solidified from molten or partly molten matierial.
Igneous rocks, which come in many different forms.
Basalt, the extrusive igneous rock that comprises most of the oceanic crust, is the most common type of solidified lava.
Hot lava, when cooled and solidified, forms igneous rocks. Examples include basalt, granite, and obsidian.