A rock can undergo metamorphism through contact metamorphism, where it is altered by heat and pressure from nearby magma, or through regional metamorphism, which is caused by deep burial and tectonic forces within the Earth's crust. In both cases, the mineral composition, texture, and structure of the rock can be changed.
The wild can be described in many ways, hear is one of them... The wild is full of many problems and many answers such as survival, all living things have to adapt to there new enviorment, like us on our first day are school. There are many ways of survival in the wild.
they are vicious, can't be trained to act in specific ways because they are not our robots! They bite you for running does that make sense No!!
Yes, barred rock chickens lay brown eggs that are edible, like eggs from other chicken breeds. Barred rock hens are known for being reliable layers of large brown eggs. These eggs are nutritious and safe to eat when properly handled and cooked.
There are many ways! 100s!
Sometimes, activities of some animals include scratching the soil or digging, some small rocks may break into smaller particles. Thus making it fine and become a part of the soil.
one way is the heat and pressure.
Foliated rocks form through regional metamorphism where intense heat and pressure create a banded or layered texture. They can also form through dynamic metamorphism, where deformation causes mineral alignment and banding in the rock.
Metamorphic rocks, such as marble, slate, and gneiss, are formed by changes in heat and pressure or the pressure of hot watery fluids. These rocks undergo a process called metamorphism, which causes the mineral composition and texture of the original rock to change.
Metamorphic rocks are formed through either heat and pressure from deep within the Earth (contact metamorphism), or from the tectonic forces of plate movements (regional metamorphism). These processes can cause existing rocks to change their mineral composition and texture, resulting in the formation of metamorphic rocks.
Metamorphic rocks form from existing rocks that undergo a change in temperature, pressure, or chemical environment. This process, called metamorphism, causes the minerals in the original rock to recrystallize and align in new ways, resulting in the formation of a metamorphic rock. Heat and pressure are the main driving forces behind this transformation.
The high temperatures required for metamorphism ultimately are derived from Earth's eternal heat, either through deep burial or from nearby igneous intrusions. The high pressures required for metamorphism can be generated in two ways: from vertical pressure caused by the weight of overlying rock, or from the compressive forces generated as rocks are deformed during mountain building.
Two ways in which metamorphic rocks are 1) contact metamorphism (thermal) where magma comes in direct contact with surrounding igneous rock and changes it due to high temperatures and usually low pressure. 2) Regional metamorphism (dynamothermal) ,high pressures and low temperature eg mountain ranges. or 3) Cataclastic metamorphism, heat as a result of friction due to two plate meeting or passing each other.
The mineral composition and texture of the parent rock can influence the resulting minerals and texture of the metamorphic rock formed. Additionally, the temperature and pressure conditions experienced by the parent rock will determine the extent of metamorphism and the types of minerals formed.
Everything. There is so many ways to change rocks. Erosion by Wind and Water. Earthquakes/Plate Tectonics, Subduction leading to metamorphism and ultimately melting and becoming Igneous. Man.
Metamorphism can occur through contact metamorphism, where rocks are altered by heat from nearby magma; regional metamorphism, where rocks are subjected to high pressure and temperature over a large area; burial metamorphism, where rocks are subjected to increased pressure from being buried deep underground; and dynamic metamorphism, where rocks are deformed under high pressure but low temperature conditions along faults or shear zones.
The minerals in the rock have been realigned into parallel bands in response to pressures exerted on the rock from a particular direction. The banding forms perpendicularly to the direction of the force.
i dont know, do u? what kind of question is THAT anyways? (get a life, geez)