The rock material melts
physical
METAMORPHISM.
It is called contact metamorphism.
Metamorphism can cause basalt to undergo changes in mineral composition and texture, forming new minerals like chlorite, epidote, or amphibole. The original basalt can recrystallize into a denser, harder rock known as greenstone due to metamorphic heat and pressure. The degree of metamorphism can vary, with low-grade metamorphism likely resulting in minor changes, while high-grade metamorphism can drastically alter the basalt's appearance.
metamorphism
recrystallization
metamorphicregional metamorphism
grade
Contact metamorphism occurs next to an intrusion of molten magma. This type of metamorphism happens when hot magma comes into contact with existing rock, causing the rock to undergo changes in mineralogy and texture due to the heat and pressure.
Metamorphism typically involves three stages: prograde metamorphism, in which rocks are subjected to increasing temperature and pressure causing mineral changes; peak metamorphism, where rocks reach their maximum temperature and pressure conditions; and retrograde metamorphism, where rocks begin to cool and the minerals may change back to their original forms.
Contact metamorphism occurs when rocks are subjected to high temperatures and pressures due to being in close proximity to an igneous intrusion, leading to localized changes in mineralogy and texture. In contrast, regional metamorphism affects large areas of rocks over a wide region due to tectonic forces such as mountain building or subduction, resulting in widespread changes in mineralogy and texture. Contact metamorphism is therefore more localized and less intense compared to regional metamorphism.
The three main types of metamorphism are contact metamorphism, regional metamorphism, and dynamic (or shear) metamorphism. Contact metamorphism occurs when rocks are heated by nearby molten magma, leading to localized changes in mineralogy and texture. Regional metamorphism happens over larger areas under high pressures and temperatures, typically associated with tectonic forces, resulting in more widespread and pronounced metamorphic changes. Dynamic metamorphism involves the alteration of rocks due to intense pressure, often during fault movements, which primarily affects the rock's texture without significant heat influence.