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Rock formed from minerals that precipitate from saturated solutions are called chemical sedimentary rocks, such as rock salt and rock gypsum.In some metamorphic rock processes, the loss of fluid due to heat and pressure can cause the transformation of some minerals into other minerals, but this is a different process than that which is causing precipitation from a saturated solution. In retrograde metamorphism, hydration (the addition of water) can also cause the transformation of some minerals.
Metamorphic rocks are rocks formed from igneous, sedimentary and even other metamorphic rocks. Heat, pressure and chemical action can cause a rock to change into another rock. Pressure from the rocks on top of them squeezes and folds the rock. Their grains come close together and they become less porous. Heat and chemicals may cause changes in the arrangement of mineral particles or new minerals may be formed.
Gneiss is a metamorphic rock formed when intense heat and/or pressure is applied to it's parent rock schist.
chemical weathering
Metamorphic rocks are formed from a protolith, or parent rock, which can be of any rock type (igneous, sedimentary, or metamorphic). The parent rock is exposed to varying degrees of pressure and/or heat either from depth of burial, exposure to a plutonic body of intense heat, or from pressures resulting from the collision of tectonic plates. Exchanges of elements can also occur from hot fluids associated with plutonic intrusions.The heat and/or pressure can transform the minerals inside the parent rock to new minerals, cause recrystallization of existing minerals, or reorganize the existing minerals into bands and layers. All of these processes take place without any melting of the parent rock.
Rock formed from minerals that precipitate from saturated solutions are called chemical sedimentary rocks, such as rock salt and rock gypsum.In some metamorphic rock processes, the loss of fluid due to heat and pressure can cause the transformation of some minerals into other minerals, but this is a different process than that which is causing precipitation from a saturated solution. In retrograde metamorphism, hydration (the addition of water) can also cause the transformation of some minerals.
The changes take place because of recrystallization or realignment of existing minerals, or creation of minerals from existing assemblages that that can only be formed under certain specific ranges of temperature or pressure.
Heat and pressure.
Answer The atoms in rocks rearrange to form denser minerals. The combination of heat and pressure may cause the minerals in the rock to separate into layers.Answer Pressure squeezes out any remaining water that may be left in the metamorphic rock and minerals that have water as part of their structure are changed chemically to minerals that do not require water as part of their structure. The metamorphic rock will then have become a higher grade metamorphic rock possibly containing garnet, a non-hydrous mineral.
Metamorphic rocks are rocks formed from igneous, sedimentary and even other metamorphic rocks. Heat, pressure and chemical action can cause a rock to change into another rock. Pressure from the rocks on top of them squeezes and folds the rock. Their grains come close together and they become less porous. Heat and chemicals may cause changes in the arrangement of mineral particles or new minerals may be formed.
Yes, all storms are formed in low pressure systems, and low pressure systems will frequently cause storms and precipitation.
When you look at a rock and see different colors, those colors are minerals .The pressure and heat causes the minerals in the rock to change into different minerals which cause the different colors in the rocks.
Metamorphic Rocks.
As the temperature of rock rises the individual mineral components begin vibrating and the intermolecular bonds holding minerals together begin to stretch.
Gneiss is a metamorphic rock formed when intense heat and/or pressure is applied to it's parent rock schist.
chemical weathering
Metamorphic rocks are formed from a protolith, or parent rock, which can be of any rock type (igneous, sedimentary, or metamorphic). The parent rock is exposed to varying degrees of pressure and/or heat either from depth of burial, exposure to a plutonic body of intense heat, or from pressures resulting from the collision of tectonic plates. Exchanges of elements can also occur from hot fluids associated with plutonic intrusions.The heat and/or pressure can transform the minerals inside the parent rock to new minerals, cause recrystallization of existing minerals, or reorganize the existing minerals into bands and layers. All of these processes take place without any melting of the parent rock.