sill
A sill is formed.
if it squeezes into a fault, its a dike, if it squeezes between horizontal layers, its a sill
It forms a sill.
The slab that forms when magma forces itself across rock layers is called a dike.
Yes, a dike forms when magma intrudes into existing rock layers and solidifies. As the magma cools and solidifies underground, it creates a vertical or near-vertical sheet-like body of igneous rock that cuts across the existing rock layers.
The magma forms sills and magma chambers.
feature a and b
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.
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.
Dikes and sills are relatively thin. They both have magma to squeeze or force itself across layers of rock.
A Sill is formed when a fluid rock (usually magma but it can be mud or salt) is squeezed in between the layers (usually horizontal) of older rocks before it solidifies in place. A Dike or Dyke is the opposite, here the fluid rock penetrates across the layering of the older rocks. Logically to get the material to form a Sill there must be an accompanying feeder Dyke.
When magma forces itself across rock layers, it can create igneous intrusions such as dikes (vertical sheet-like intrusions) or sills (horizontal sheet-like intrusions). These intrusions form when magma solidifies as it cools, creating distinctive structures within the surrounding rock layers.