It forms a dome.
The inside of the earth (Mantle) pushes the hot magma liquid and makes the magma move toward the surface.
As magma pushes upward, it can raise the overlaying rock layers into a geological feature known as a dome or a laccolith. This occurs when the magma accumulates and exerts pressure, causing the surrounding rock to bulge. Over time, such formations can lead to the development of distinct topographical features on the Earth's surface.
It cools and solidifies into a sedimentary rock.
A dome formed by thick magma that pushes upward rather than horizontally.
When magma pushes upward, it raises overlying rock layers into dome-like structures called volcanic domes or volcanic plugs. These features are formed as the magma forces its way through the Earth's crust and solidifies before reaching the surface.
Magma pushes its way upward due to buoyancy, caused by its low density compared to the surrounding rock. Additionally, increasing pressure from beneath and the presence of fractures or weak spots in the crust can also facilitate magma ascent.
The magma in a sill that pushes up to form a dome-shaped rock structure is called laccolith. Laccoliths form when magma intrudes between layers of sedimentary rock and causes the overlying rocks to arch upwards, resulting in a dome-like structure.
The landform is called a laccolith. It forms when magma is injected between layers of sedimentary rock, causing the overlying layers to arch upward. As the magma cools and solidifies, it creates a dome-shaped uplift in the Earth's crust.
A laccolith intrusion feature may start as a sill, where magma is injected parallel to the rock layers. As more magma accumulates, it can create a bulge that pushes the overlying layers upward, creating a dome-shaped structure resembling a lens. This process is characteristic of the formation of laccoliths in geology.
An igneous intrusive feature that forms from a lens-shaped mass of magma that arches the overlying strata upward is called a laccolith. Laccoliths typically create a dome-like structure as the magma pushes the surrounding rock layers upward. They are often associated with volcanic activity and can vary in size.
The force that pushes rock upward is typically uplift caused by tectonic plate movements. This can occur when tectonic plates collide, causing one plate to be pushed up over the other, or when magma rises towards the surface, creating pressure that lifts the overlying rock.
Volcanic eruptions are caused by the release of pressure from molten rock, or magma, that rises to the surface through weak spots in the Earth's crust. As the magma pushes upward, it can create volcanic activity, such as lava flows, ash emissions, and explosive eruptions.