The magma slowly cools over time into intrusive igneous rock. Later, often because the land is uplifted, the surrounding rock is eroded. Intrusive igneous rock, however, is often quite resistant to erosion, and so remains in place.
The magma slowly cools over time into intrusive igneous rock. Later, often because the land is uplifted, the surrounding rock is eroded. Intrusive igneous rock, however, is often quite resistant to erosion, and so remains in place.
If magma is solidified it will form
Volcanic neck
Magma forms from heated rock--it cools--minerals form--when totally solidified it is a rock.
The lava would form pillow basalts.
The lava would form pillow basalts.
Magma is basicaly the same as lava, except magma is still in the volcano, when magma has come out of the volcano, it has become lava.
They are formed when either a sedimentary rock or a metamorphic rock are exposed to high heat and turn into magma and then cool quickly.
A volcanic plug. Frequently when glacially eroded these plugs form crag and tail feature.
All the three existing rock families/types/classes (ie, igneous, sedimentary and metamorphic rocks) can form magma, if they become hot enough to melt and change to molten form.
Igneous rock, if heated sufficiently by subduction processes will melt to form magma.
A loooooooong time ago it was classified as a Stratovolcano. When it erupted, the magma cooled and hardened in the volcano. Eventually, the outer part eroded away, causing the cooled magma to be exposed. After that, it was then classified as an extinct volcano, and to this day it is a popular tourist attraction.