They rarely have pores. But sometimes they get them from all the heat and pressure their put under.
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the metamorphic rocks are formed by heat and extreme pressure from other rocks
Slate and marble are examples of metamorphic rocks. Other metamorphic rocks include gneiss, schist, and quartzite. All metamorphic rocks are formed from other rock types.
Metamorphic rocks have been changed by heat or pressure. This can be a change in size, shape, or arrangement of minerals.
Foliation is a descriptive term applied to certain types of metamorphic rocks, so, by definition, Yes, a folate rock is metamorphic.
Metamorphic rocks can sometimes have spaces or voids called vesicles, but these are not common in all metamorphic rocks. Holes or voids can also form in metamorphic rocks through the dissolution of minerals or inclusions during the rock's formation process. Overall, metamorphic rocks are more likely to have a solid, dense structure compared to sedimentary rocks, which are more prone to having visible pores or holes.
No. Metamorphic rocks can also from front sedimentary rocks and from other metamorphic rocks.
Metamorphic Rocks
Metamorphic rocks
It is a type of Metamorphic rock
igneous, sedimentary, metamorphic
Metamorphic rocks can form from both igneous and sedimentary rocks through the process of heat and pressure, but they are more commonly associated with forming from existing metamorphic or sedimentary rocks. Igneous rocks can indirectly contribute to the formation of metamorphic rocks by heating up and altering surrounding rocks, leading to the formation of new metamorphic rocks.
Metamorphic rocks can form from both igneous and sedimentary rocks
Metamorphic rocks can form from both igneous and sedimentary rocks
Rocks formed from high temperature and pressure include metamorphic rocks such as marble, schist, and gneiss. These rocks are created deep within the Earth's crust through the transformation of existing rock types under intense heat and pressure conditions.
Porous rocks.
Unakite rocks are metamorphic rocks formed from the alteration of igneous rocks. They are typically composed of pink feldspar, green epidote, and clear quartz.