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
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.
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.
horizontal
batholiths