Igneous,sedimentry and metamorphic
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.
No, small intrusive bodies are not called stocks; they are referred to as "stocks" in a geological context when discussing larger, more significant bodies of intrusive igneous rock. In geology, smaller intrusive bodies are typically called "dikes," "sills," or "plutons," depending on their shape and orientation. Stocks specifically refer to smaller plutons that are less than 100 square kilometers in area.
size, shape, and relationship to the surrounding rock layers
It is called an intrusive igneous rock.
Intrusive igneous rock is formed from solidified magma below the surface of the Earth. Intrusive rock exhibits a phaneritic texture, where the individual crystal grains are visible without magnification. Examples of intrusive igneous rocks are granite, diorite, and gabbro.
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.
No, small intrusive bodies are not called stocks; they are referred to as "stocks" in a geological context when discussing larger, more significant bodies of intrusive igneous rock. In geology, smaller intrusive bodies are typically called "dikes," "sills," or "plutons," depending on their shape and orientation. Stocks specifically refer to smaller plutons that are less than 100 square kilometers in area.
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