When granite is subjected to high temperatures and pressures over time, it can transform into a type of rock called gneiss. This process occurs through metamorphism, where the minerals within the granite re-crystallize and align, resulting in a banded or foliated texture. Gneiss retains some characteristics of the original granite but exhibits distinct changes in mineral composition and structure.
If granite undergoes high temperatures and high pressures deep within the Earth without melting, it will transform into a metamorphic rock called gneiss. This process, known as metamorphism, alters the mineral composition and texture of the granite, resulting in the characteristic banding and foliation found in gneiss. The high-pressure and high-temperature conditions facilitate the recrystallization of minerals, enhancing the rock's structural integrity.
When granite is subjected to high heat and pressure without melting, it undergoes a metamorphic process, transforming into a rock known as gneiss. This process alters the mineral structure and texture of the granite, often resulting in the formation of new minerals and the alignment of existing ones, creating a banded appearance. The increased temperature and pressure can also enhance the rock's overall density and strength.
If granite undergoes high temperatures and high pressures without melting, it will transform into a metamorphic rock known as gneiss. This process, called metamorphism, alters the mineral composition and texture of the granite, resulting in the formation of bands or foliated textures characteristic of gneiss. The minerals in granite, such as quartz and feldspar, may recrystallize under these conditions, leading to the development of new mineral assemblages.
High pressure = High temperature
Yes, granite can change into gneiss through the process of metamorphism. This transformation typically involves high temperature and pressure conditions, causing the mineral composition and texture of the granite to recrystallize into the banded texture associated with gneiss.
If granite undergoes high temperatures and high pressures deep within the Earth without melting, it will transform into a metamorphic rock called gneiss. This process, known as metamorphism, alters the mineral composition and texture of the granite, resulting in the characteristic banding and foliation found in gneiss. The high-pressure and high-temperature conditions facilitate the recrystallization of minerals, enhancing the rock's structural integrity.
When granite is subjected to high heat and pressure, it undergoes metamorphism and can transform into a metamorphic rock called gneiss. This process involves recrystallization of minerals within the granite, resulting in a new texture and mineral composition.
When granite is subjected to high heat and pressure without melting, it undergoes a metamorphic process, transforming into a rock known as gneiss. This process alters the mineral structure and texture of the granite, often resulting in the formation of new minerals and the alignment of existing ones, creating a banded appearance. The increased temperature and pressure can also enhance the rock's overall density and strength.
If granite were subjected to intense heat and pressure, it would likely change to gneiss, a metamorphic rock. Gneiss forms through the recrystallization of minerals in granite under high temperature and pressure conditions.
Granite subjected to high temperature and pressure deep within the Earth without melting would likely undergo a process called metamorphism, and would form a metamorphic rock known as gneiss. Gneiss is characterized by its banded appearance due to the reorganization of minerals under intense heat and pressure.
If granite undergoes high temperatures and high pressures without melting, it will transform into a metamorphic rock known as gneiss. This process, called metamorphism, alters the mineral composition and texture of the granite, resulting in the formation of bands or foliated textures characteristic of gneiss. The minerals in granite, such as quartz and feldspar, may recrystallize under these conditions, leading to the development of new mineral assemblages.
High pressure = High temperature
Yes, granite can change into gneiss through the process of metamorphism. This transformation typically involves high temperature and pressure conditions, causing the mineral composition and texture of the granite to recrystallize into the banded texture associated with gneiss.
If limestone undergoes contact metamorphism, it will typically turn into marble. Marble forms from the recrystallization of limestone under high temperature and pressure conditions.
No , a high temperature high pressure ( gas )
The most common metamorphic rock derived from granite is gneiss. Gneiss forms through high-grade metamorphism, where granite undergoes intense heat and pressure, resulting in a foliated texture characterized by alternating bands of light and dark minerals. This banding is a key feature that distinguishes gneiss from other metamorphic rocks.
Any rock can become a sedimentary rock (even another sedimentary rock) is it is broken down by erosion, and the resulting sediment is then redeposited, undergoes compaction and consolidation and then lithification (lithification is just the process of becoming a rock)Any rock can become a metamorphic rock if it is subject to sufficient pressure and temperature as a result of deep burial (which will result in both high heat and high pressure) or mostly pressure e.g from the pressure of two continental plates colliding.examples - mudstone under high pressure becomes slateLimestone under moderately high temperature and pressure becomes marble.Granite under intense pressure and Temperature short of actual remelting becomes a gneiss, if the greiss undergoes even greater pressure and temperature it can become a schist.Finally, any rock subject to sufficient temperature as a result of very deep burial will melt, become magma, and ofthe magma them eventually cools enough to crystallise you have a new igneous rock