Sedimentary rock is changed to metamorphic rock using:
1. High pressure
2. High heat
3. A large amount of time
During a mountain building phase, the sedimentary rocks may be buried deeply and subjected to heat and pressure causing certain minerals to form which were not present in the original rock. Also, an igneous intrusion may cause adjoining sediments to be altered in a contact metamorphism leading minerals such as garnets to form.
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.
High pressure can cause the formation of the metamorphic rock slate from the sedimentary rock shale.
Protolith is a term used to describe the parent rock of a metamorphic rock. Conglomerate is a sedimentary rock that can be composed of clasts of sedimentary, igneous, or metamorphic rocks, or any number of combinations of all.
Quick Answer: temperature and/or pressure applied to any type of rock (sedimentary, igneous, and even metamorphic) can cause said rock to become metamorphosed. For example, marble is the metamorphosed equivalent of a carbonate rock.
sedimentary rocks
Heat and pressure changes sedimantary rock (limestone) into metemorphic rock(gnesis).
If by particles you mean the size of the crystals, then the crystals in metamorphic rock are often larger than in the sedimentary rock. High heat and pressure can cause the minerals to recrystallize. This would be the case in the metamorphosis of limestone (sedimentary) to marble (metamorphic).
the main things that cause metamorphic rocks to form is heat, pressure and chemical fluids.
Metamorphic rocks are created by the physical or chemical alteration by heat and pressure of an existing igneous or sedimentary material into a denser form. This rock was compressed into an metamorphic by the tons and tons of pressure causing it to overheat and cause a change which can be chemical or physical.
Pressure and heat from being buried under mountains.
The difference of metamorphic rocks from igneous and sedimentary rocks is on the way these rocks are formed. Igneous rocks form when magma cools down and becomes solid while sedimentary rocks form due to erosion and weathering of the Earthâ??s material, whereas, metamorphic rocks are formed as a result of rock transformation called metamorphism.
Marble is classified as a metamorphic rock. 'Metamorphic' means that the rock has undergone a change in from. In the case of marble, it starts out as some kind of sedimentary carbonate rock (sedimentary rocks are formed by sediments and remains of plant life, etc. that have been compacted together over time) and then that rock material is transformed by a combination of heat and pressure to become marble. The changes may be a development of a chrystalline formation, or a texture or color change. Sometimes the metamorphic changes in rock may include the involvement of minerals, in additon to the heat and pressure combination. Different minerals cause the different color varieties of marble that are available.
By applying increasing pressures or temperatures which cause mineralogical and structural changes to the rock.
The metamorphic or igneous rock would have to be weathered and eroded until it is only particulates. Those particulates must then be forced together as a layer under gravitational pressure. These particulates will then become sedimentary rocks.
The presence of intrusive magma in an area (known as contact metamorphism), or of tectonic plate interactions on a larger scale (known as regional metamorphism) puts the igneous and sedimentary rocks and minerals under heat or pressure which may cause changes in their chemistry and crystal structure. The result is the creation of metamorphic rocks. Gemstones associated with metamorphic rock include the beryls, jade, lapis lazuli, turquoise, spinel, ruby, sapphire and zircon.
During a mountain building phase, the sedimentary rocks may be buried deeply and subjected to heat and pressure causing certain minerals to form which were not present in the original rock. Also, an igneous intrusion may cause adjoining sediments to be altered in a contact metamorphism leading minerals such as garnets to form.