A discordant intrusion is known as a dyke. A larger intrusion may also be a pluton or batholith, which both also cut across rock strata. A sill is an intrusion which is concordant, and goes between the strata. This does not necessarily mean that it is horizontal.
The intrusion is younger than the overlying sedimentary rock.
Any igneous dike or intrusion is younger that the surrounding rock layers.
Basically, igneous intrusion involves the solidifying of magma when it cools in the crust of the Earth. When magma rises through the crust, it intrudes into the existing sedimentary rock layers and forms a hill. The surounding rock may be more prone to erosion and wear away leaving the intrusion jutting above the (eroded) surroundings.
A sheet of igneous rock that protrudes into the surrounding layers of rock is called a dike. Dikes are most often horizontal sheets that can form in many layers.
An intrusion is younger than its surrounding rock layers. An intrusion needs another rock to cut through it, which is referred to as a cross-cutting relationship.
A laccolith is an igneous formation between two sedimentary layers
It's called a concordant igneous intrusion, or a sill.
That would be a type of igneous intrusion known as a dike.
The intrusion is younger than the overlying sedimentary rock.
An intrusion is a mass of igneous rock that forms when melted rock moves into cracks in rock layers and then cools.
It is younger than them.
It is younger.
It is younger.
A form of igneous intrusion known as a Sil.
the rock layers were eroded at the interface between the igneous intrusion and the sedimentary rocks.
Any igneous dike or intrusion is younger that the surrounding rock layers.
Intrusive is a term that applies to igneous rocks that form from magma underground such as granite.