The Batholith would be the larger feature.
When magma is pushed into a thick sill, it solidifies underground to form a layer of igneous rock called a dike. Dikes typically cut across existing rock layers, creating a discordant intrusion. The rock that forms from the cooling magma in a dike is usually fine-grained due to the rapid cooling process underground.
Igneous Rocks - Rocks formed by crystallization from a melt (magma) types are: # Extrusive (volcanic) - produced when magma flows on the earth's surface # Intrusive (plutonic) - produced when magma solidifies at depth beneath the earth. eg.s are: 1)pumice. 2)Laccolith 3)Batholith 4)Dike 5)Sill
A vertical wall of intrusive rock is more likely to be a dike or a sill, rather than a batholith. Batholiths are large masses of intrusive igneous rock that typically form large underground plutons or domes. They are usually associated with extensive geological processes and are formed at depth in the Earth's crust.
AnswerA dike is an intrusive body of magma that pushes its way across layers of sediments.A sill is an intrusive body of magma that pushes its way between layers of sediments.
A sill is a horizontal sheet of igneous rock that is intruded between existing rock layers, while a laccolith is a dome-shaped intrusion that causes the overlying rock layers to arch upwards. Sills are flat and parallel to existing rock layers, while laccoliths are typically lens-shaped and create bulges in the rock layers above them.
When magma is pushed into a thick sill, it solidifies underground to form a layer of igneous rock called a dike. Dikes typically cut across existing rock layers, creating a discordant intrusion. The rock that forms from the cooling magma in a dike is usually fine-grained due to the rapid cooling process underground.
batholith
Igneous Rocks - Rocks formed by crystallization from a melt (magma) types are: # Extrusive (volcanic) - produced when magma flows on the earth's surface # Intrusive (plutonic) - produced when magma solidifies at depth beneath the earth. eg.s are: 1)pumice. 2)Laccolith 3)Batholith 4)Dike 5)Sill
The four main intrusive igneous features are dikes (tabular intrusions that cut across rock layers), sills (tabular intrusions that run parallel to rock layers), laccoliths (mushroom-shaped intrusions with a flat base), and batholiths (large, dome-shaped intrusions that form the core of mountain ranges).
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.
A vertical wall of intrusive rock is more likely to be a dike or a sill, rather than a batholith. Batholiths are large masses of intrusive igneous rock that typically form large underground plutons or domes. They are usually associated with extensive geological processes and are formed at depth in the Earth's crust.
you would want to have a batholith, becaus it is much bigger than a sill. your goal when mining is to get a much of the minerl as possible and a batholith has more granite becuse it is bigger.
It's sill or batholith.
the chemical and physical particles
The slab of volcanic rock that is formed when magma forces itself across rock layers is called a dike. This will eventually build into mountains.
AnswerA dike is an intrusive body of magma that pushes its way across layers of sediments.A sill is an intrusive body of magma that pushes its way between layers of sediments.
This is known as a laccolith.