magma squeezed into a vertical crack is called a dike.
A hardened layer of magma is called a lava flow or volcanic rock.
batholiths
dike
When magma flows horizontally, it can form igneous rock formations called dikes or sills. Dikes are vertical intrusions, while sills are horizontal intrusions. These structures are formed when magma solidifies within preexisting rock layers.
A dike is formed when magma intrudes and solidifies in a vertical or near-vertical orientation within pre-existing rock layers. Lava flows, on the other hand, occur when magma erupts onto the surface and flows horizontally along the ground.
An intrusion.
No, actually the volcanic pipe is horizontal.
Commonly referred to as a sill.
No.
It forms a sill.
If vertical, a dyke; if horizontal, a sill.
A hardened layer of magma is called a lava flow or volcanic rock.
when magma is squeezed into horizontals craks are called sill
horizontal
False. A pipe of a volcano is a vertical conduit that allows magma to rise from depth to the surface. It is typically a narrow, tube-like structure that connects the magma chamber to the surface vent of the volcano.
batholiths
A dome mountains forms when rising magma is blocked by horizontal layers of rock. The magma forces the layers of rock to bend upward into a dome shape. Eventually, the rock above the dome mountain wears away, living it exposed.