Commonly referred to as a sill.
Magma that hardens in a horizontal crack typically forms a thin, sheet-like intrusion called a sill. Sills are created when magma is injected parallel to the existing rock layers. As the magma cools and solidifies, it forms a horizontal layer of igneous rock within the crack.
It forms a sill.
A crack that has been filled in by magma and hardens parallel to existing rock layers is known as a "sill." Sills are formed when magma intrudes between pre-existing rock layers and solidifies, resulting in a horizontal or nearly horizontal sheet of igneous rock. This process can create distinctive geological features and is an important aspect of igneous rock formation.
It is called a dike.
Magma that hardens after being forced into a crack across rock is called a dike.
No, actually the volcanic pipe is horizontal.
Sill (D)
A concordant intrusive igneous feature like a sill can form when magma hardens between horizontal layers of rock. Sills are tabular bodies that are parallel to the surrounding rock layers.
When magma hardens inside the Earth's crust, it can form vertical columns known as dikes, and horizontal layers called sills. Dikes form when magma cuts through pre-existing rock layers, while sills are formed when magma intrudes between existing rock layers.
Yes, that's correct. Sills are igneous rock formations that form when magma is intruded horizontally between rock layers and then solidifies underground. If the magma solidifies vertically underneath the surface, it will create a sill structure.
Igneous rock is what forms when magma cools and hardens.
That would be a type of igneous intrusion known as a dike.