Sedimentary rocks: Metamorphic rocks
Subduction and high pressure.
Sedimentary rocks are ones formed by solidified mud and loose earth. Metamorphic rocks are ones formed by some sort of change, such as melting and re-cooling. So they are similar in some senses (they are both rocks, both of the earth) but in others they are very different (physical properties).
Metamorphic Rocks
That they have undergone some form of change. For more information on metamorphic rocks please see the related question.
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Sedimentary rocks: Metamorphic rocks
because if the metamorphic rocks are big they will shrink
Some questions about metamorphic rocks that could be explored include: How do different types of pressure and temperature affect the formation of metamorphic rocks? What are the key minerals found in metamorphic rocks and how do they indicate the rock's history? How do metamorphic rocks differ from igneous and sedimentary rocks in terms of their formation processes and characteristics?
Metamorphic rocks are formed when igneous or sedimentary rocks undergo change because of exposure to excessive heat and pressure. The properties most often used to distinguish them from other kinds of rocks are: density, banding and the absence of vesicles.
Subduction and high pressure.
Metamorphic rocks are used for building materials like marble and slate. They can also be used as decorative stones in landscaping and architecture. Some metamorphic rocks, like quartzite, are used as abrasive materials in manufacturing.
Sedimentary rocks are ones formed by solidified mud and loose earth. Metamorphic rocks are ones formed by some sort of change, such as melting and re-cooling. So they are similar in some senses (they are both rocks, both of the earth) but in others they are very different (physical properties).
No. Metamorphic rocks can also from front sedimentary rocks and from other metamorphic rocks.
shale
Examples of non-foliated metamorphic rocks are quartzite and marble.
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.