contact metamorphism
Magma reaches the Earth's surface through a process called volcanic eruption. This occurs when pressure builds up underground and forces the magma to flow and eventually break through the Earth's surface. Once the magma reaches the surface, it is then called lava.
When hot magma forces its way into rocks, it can cause contact metamorphism. This process involves the high temperatures and pressure of the magma altering the surrounding rocks, changing their mineral composition and creating new rocks like marble or quartzite. Additionally, the rocks affected by the intrusion of magma may exhibit new textures and structures from the heat and chemical reactions.
Magma that forces its way into rocks and hardens is called intrusion.
contact metamorphism
When heat from nearby magma causes changes in surrounding rocks, a process called contact metamorphism occurs. This process includes changes in rock texture and mineral composition due to the high temperature and pressure from the magma. This usually results in the formation of new minerals and textures within the rocks.
When metamorphism occurs due to heat generated by magma, it is called "contact metamorphism." This process typically happens when surrounding rocks are heated by the proximity of molten magma, leading to changes in mineral composition and texture. The effects are usually localized around the intrusion of magma, resulting in the formation of metamorphic rocks such as hornfels.
Igneous rock is formed when magma forces itself into surrounding underground rock and cools and solidifies. The surrounding rock is heated and metamorphosed but does not fully melt in this process.
An intruding magma body makes room for itself during emplacement by causing the surrounding rocks to deform and fracture. This process occurs through processes such as dilation, where the pressure of the magma forces the surrounding material to expand, and brittle failure, where the rocks break apart to accommodate the incoming magma. As the magma rises, it can also create a network of cracks and fissures, allowing it to move upwards more easily. Ultimately, this creates a space for the magma to occupy as it solidifies into igneous rock.
The process through which single parent magma can form rocks with different compositions is known as fractional crystallization. It occurs as the magma cools and solidifies, with different minerals crystallizing at different temperatures. As these minerals crystallize and settle out of the magma, they can form different rock compositions depending on the minerals that have formed. This process can produce a range of rock compositions from a single parent magma.
I could be wrong. But crystalization is what I would say.
SubductionThe Magma Forms And Makes A Volcano
Magma can change form when it cools and solidifies to become igneous rock. This process typically occurs underground, allowing the magma to cool slowly and crystallize into different types of igneous rocks such as granite or basalt.