Volcanic necks, Batholiths and Dome Mountains are the features formed when magma cools beneath the Earth’s surface.
Step-by-step explanation:
- Volcanic neck is the hard deposited magma after the cooling process beneath the earth surface.
- Batholiths are the mass of rock formed when magma cools beneath the earth crust.
- Dome Mountains are formed when cooling down process of magma leads to cold and hard rock.
Magma chambers correspond to the surface in reservoirs below which Magma is stored. “Stocks, laccoliths, sills” are some of the Intrusive features that are formed as a result. The type of volcanic landforms is decided by the cooling of magma either within the crust or above the crust.
This may result in either extrusive or intrusive landforms. The feature is also known as dynic volcano. The final stage is the formation of the magma, cooling of it, and then becoming hard.