The magma that forms an intrusion or feeds a volcano provides the heat that drives hydrothermal activity.
Igneous Intrusions
Contact metamorphism occurs locally, next to igneous intrusions and along fractures that were in contact with hydrothermal fluids. Regional metamorphism occurs over very large areas, such as deep within the cores of rising mountain ranges, and generally occurs with the folding of rock layers. Both result in the formation of metamorphic rocks.
plutons
GranitesDioritesGabbrosPegmatitesDykesSillsLayered Igneous intrusions
metamorphism is when a Igneous and sedimentary rocks turn into metamorphic rock.
Igneous Intrusions
Contact metamorphism occurs locally, next to igneous intrusions and along fractures that were in contact with hydrothermal fluids. Regional metamorphism occurs over very large areas, such as deep within the cores of rising mountain ranges, and generally occurs with the folding of rock layers. Both result in the formation of metamorphic rocks.
Names given to the different types of igneous intrusions are attributed to their
Igneous rocks can be changed to sedimentary rocks outside of igneous intrusions. This is due to silt built up and weathering.
plutons
GranitesDioritesGabbrosPegmatitesDykesSillsLayered Igneous intrusions
metamorphism is when a Igneous and sedimentary rocks turn into metamorphic rock.
The largest of all igneous intrusions is called a batholith. Batholiths are formed by the massive invasion of hot magma into country rock.
When magma reaches the earth's surface, it is called lava. when it solidifies, it forms new crust, or rock.
Igneous intrusions form when magma cools and solidifies before it reaches the surface. Three common types of intrusion are sills, dykes, and batholiths
Igneous processes and hydrothermal solutions
Regional metamorphism is a widespread precess involving both heat and directed pressure, and is involved in things like mountain building and activity deep with in the core. Contact metamorphism is local processes involving low to moderate pressure and high temperature. This type is adjacent to igneous intrusion and along fractures in contact with hydrothermal (hot!) fluids at mid-ocean ridges.