horizontal
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 is called a dike.
when magma is squeezed into horizontals craks are called sill
Magma that hardens after being forced into a crack across rock is called a dike.
No, actually the volcanic pipe is horizontal.
yes
That would be a type of igneous intrusion known as a dike.
dike
AnswerA dike is an intrusive body of magma that pushes its way across layers of sediments.A sill is an intrusive body of magma that pushes its way between layers of sediments.
Vertical is up and horizontal is across
Vertical and horizontal
vertical and horizontal