magma pushed into a thick sill can form what
It can form laccolith. Your welcome!
Laccolith
laccolith
No. A sill forms when magma hardens parallel to the rock layers, which is usually horizontal. When magam hardens vertically, it forms a dike.
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.
A form of igneous intrusion known as a Sil.
Sill (D)
Simple terms- Chemical and Physical particles
A magma sill is a planar sheet of magma which is parallel to the surrounding rock.
Laccolith
No. A sill forms when magma hardens parallel to the rock layers, which is usually horizontal. When magam hardens vertically, it forms a dike.
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.
Sill (D)
A form of igneous intrusion known as a Sil.
the chemical and physical particles
Sill (D)
Simple terms- Chemical and Physical particles
A sill is an intrusive body of magma that pushes its way between layers of sediments.
No, when magma forces itself BETWEEN rock layers it is called a sill. When the magma cuts THROUGH rock layers it is called a dike.
A Sill.