Stock
Batholith
No, a stock is not an intrusive igneous body. In the world of finance, a stock refers to ownership in a company and shares of its assets and profits. Intrusive igneous bodies are geological formations formed underground from the cooling and solidification of magma.
A batholith is an example of an intrusive igneous body. Batholiths are large formations of intrusive igneous rocks that form beneath the Earth's surface through the slow cooling and solidification of magma.
The largest discordant body of intrusive igneous rock is the Bushveld Complex in South Africa. It covers an area of about 66,000 square kilometers and is primarily composed of gabbro, an intrusive igneous rock.
Stope
A tabular concordant intrusive structure refers to a type of igneous intrusion where the orientation of the intrusive body is parallel to the existing layering or structures in the surrounding rock. This results in the intrusion appearing as a tabular or sheet-like feature that runs parallel to the rock layers. The intrusive body is typically discordant to the sedimentary or metamorphic layers but its orientation is concordant.
No it is not intrusive because of the difference in body heat and intrusive igneousStope is not an intrusive igneous body. apex
No, a stock is not an intrusive igneous body. In the world of finance, a stock refers to ownership in a company and shares of its assets and profits. Intrusive igneous bodies are geological formations formed underground from the cooling and solidification of magma.
no
yes
Lahar
A batholith is an example of an intrusive igneous body. Batholiths are large formations of intrusive igneous rocks that form beneath the Earth's surface through the slow cooling and solidification of magma.
The largest discordant body of intrusive igneous rock is the Bushveld Complex in South Africa. It covers an area of about 66,000 square kilometers and is primarily composed of gabbro, an intrusive igneous rock.
sill
Stope
The largest type of intrusion is the pluton.
A batholith is a group of intrusive igneous plutons.
Sills, dikes, and volcanic necks are not examples of an intrusive igneous body. These features are formed by igneous activity in the Earth's crust but are not considered intrusive bodies because they are typically narrow and tabular in shape, rather than larger and more massive like intrusive bodies such as batholiths or plutons.