Igneous,sedimentry and metamorphic
Dikes: Tabular, discordant intrusive igneous bodies that cut across existing rock layers. Sills: Tabular, concordant intrusive igneous bodies that form parallel to existing rock layers. Laccoliths: Intrusive igneous bodies that are lens-shaped and have uplifted the overlying rock layers. Batholiths: Large intrusive igneous bodies that cover at least 100 square kilometers. Stocks: Small intrusive igneous bodies that are less than 100 square kilometers in size.
Batholiths, laccoliths, and diapirs are intrusive bodies that can break blocks of the intruded rock and cause them to sink due to their size and pressure exerted during the emplacement process. These intrusive bodies have the ability to deform and displace the surrounding rock formations, leading to the sinking of blocks within the intruded rock.
Stock Batholith
The principle you are referring to is the principle of cross-cutting relationships. It states that any feature that cuts across a rock must be younger than the rock it cuts across. This applies to intrusive rock bodies, which are younger than the rocks they intrude into.
Igneous rock that forms below the Earth's surface is intrusive.
Igneous,sedimentry and metamorphic
Dikes: Tabular, discordant intrusive igneous bodies that cut across existing rock layers. Sills: Tabular, concordant intrusive igneous bodies that form parallel to existing rock layers. Laccoliths: Intrusive igneous bodies that are lens-shaped and have uplifted the overlying rock layers. Batholiths: Large intrusive igneous bodies that cover at least 100 square kilometers. Stocks: Small intrusive igneous bodies that are less than 100 square kilometers in size.
Batholiths, laccoliths, and diapirs are intrusive bodies that can break blocks of the intruded rock and cause them to sink due to their size and pressure exerted during the emplacement process. These intrusive bodies have the ability to deform and displace the surrounding rock formations, leading to the sinking of blocks within the intruded rock.
The four basic types of plutons are batholiths, stocks, dikes, and sills. Batholiths are large masses of intrusive igneous rock that form deep underground, while stocks are smaller intrusions. Dikes are tabular bodies of igneous rock that cut across existing rock layers, and sills are tabular bodies that intrude between existing rock layers.
size, shape, and relationship to the surrounding rock layers
The largest individual rock bodies are probably plutons, masses of intrusive igneous rock which may be many miles in diameter.
Granite is an intrusive igneous rock.
It is a coarse grained rock if its intrusive.
It is a coarse grained rock if its intrusive.
It is called an intrusive igneous rock.
I dont know but an intrusive rock is a type of igneos rock
Stock Batholith