Because the surrounding materials are nearly the same temperature as the molten rock material.
Gabbro cooled slowly underground, resulting in the formation of coarse-grained crystals in the rock. This slow cooling process allows large crystals to grow and develop in the molten rock.
Quartz
Intrusive
No. Molten rock under the surface is called magma. Molten rock above the surface is referred to as lava.
They are insulated by the surrounding rock and are in close proximity or part of a hot, molten, or partially molten igneous intrusion.
Gabbro cooled slowly underground, resulting in the formation of coarse-grained crystals in the rock. This slow cooling process allows large crystals to grow and develop in the molten rock.
Quartz
igneous rock.
slowly
Intrusive
Quartz
It is mineral
No. Molten rock under the surface is called magma. Molten rock above the surface is referred to as lava.
They are insulated by the surrounding rock and are in close proximity or part of a hot, molten, or partially molten igneous intrusion.
The texture is determined by the rate it takes the molten to cool to form the rock.
Rock is an excellent insulator, meaning that it loses heat slowly and gains it slowly, so an intrusion loses its heat slowly to the country rock, and the country rock absorbs it slowly (some of it undergoing metamorphosis). This means that the rock under the surface cools very slowly. On the surface, water and air cause the heat on the surface of the rock to cool very quickly, forming an noticeable chilled margin. This means that in a lava flow, for example, the surface cools to form something that looks solid, whereas underneath it can still be flowing. Inevitably the lava underneath will cool too, and more quickly than underground, as it is nearer to the cool atmosphere.
The texture of a rock is determined by the rate it takes the molten to cool to form the rock.