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Metamorphic rocks are formed the heat and pressure underground.

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Sedimentary rocks seem rocky as well. Let's explore them too!

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Now let's explore the metamorphic rocks!

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Let's explore the igneous rocks first!

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The Rock Cycle is the process where rocks can change and be made under different conditions. Heat, pressure, cooling, or weathering

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The melting of Sedimentary rocks, followed by cooling. For example, shale can turn into diorite.

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Erosion, deposition, compaction, and cementation of metamorphic rocks.
For example, quartzite can turn into sandstone.

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Heat and Pressure of Igneous rocks.
For example, granite can turn into gneiss through this process.

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Erosion, deposition, compaction, and cementation of sediment. For example, basalt can turn into chert.

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The heat and pressure of Sedimentary rocks. For example, shale(sedimentary) can turn into slate(metamorphic) through this process.

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The melting of the metamorphic rock, followed by cooling.
For example, slate can turn into granite.

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Pressure on rocks is how much force is acted upon it.

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Nonfoliated Metamorphic Rocks are rocks that are formed near igneous intrusions. The pressures there are relatively low, and are equal in all directions. This causes the rocks to become denser.
Examples: Quartzite, and marble.

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Foliated Metamorphic Rocks are rocks formed under the Earth's surface, under unequal, extreme high pressures: when there is more pressure applied to one direction than in the others. This causes the rocks to reorient themselves with the long and flat minerals, and gives the rock a stripped look.
Examples: Slate, phyllite, , schist, and gneiss.

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Hi! My name is Rockie, and I will be showing you the rock cycle, and igneous, sedimentary, and metamorphic rocks.

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Links:
http://www.mineralogy4kids.org/?q=rock-cycle
Igneous Rocks: http://www.mineralogy4kids.org/rock-cycle/igneous-rocks
Extrusive: http://www.mineralogy4kids.org/rock-cycle/extrusive-igneous-rocks
Intrusive: http://www.mineralogy4kids.org/rock-cycle/intrusive-igneous-rocks
Sedimentary Rocks: http://www.mineralogy4kids.org/rock-cycle/sedimentary-rocks
Clastic: http://www.mineralogy4kids.org/rock-cycle/clastic-sedimentary-rocks
Non-clastic: http://www.mineralogy4kids.org/rock-cycle/nonclastic-sedimentary-rocks
Metamorphic Rocks: http://www.mineralogy4kids.org/rock-cycle/metamorphic-rocks
Foliated: http://www.mineralogy4kids.org/rock-cycle/foliated-metamorphic-rocks
Non-foliated: http://www.mineralogy4kids.org/rock-cycle/nonfoliated-metamorphic-rocks
* http://www.kids-fun-science.com/organic-rocks.html
*https://www.geolsoc.org.uk/ks3/gsl/education/resources/rockcycle/page3559.html
* https://www.nationalgeographic.org/encyclopedia/sediment/
Images:
* https://requestreduce.org/images/compaction-examples-clipart-kids-science-19.jpg
* https://www.buzzle.com/img/articleImages/557359-9027-35.jpg
* https://media.nationalgeographic.org/assets/photos/000/269/26930.jpg
*https://researchpedia.info/wp-content/uploads/2014/03/Difference-between-Magma-and-Lava.jpg
*https://upload.wikimedia.org/wikipedia/commons/thumb/6/63/Wavecut_platform_southerndown_pano.jpg/500px-Wavecut_platform_southerndown_pano.jpg
*https://www.chesapeakebay.net/images/issues/06.17_sediment_issues_image.jpg
*https://i.pinimg.com/originals/f3/5a/9c/f35a9c4d60700985984205ee64159fdf.gif
* https://lh5.googleusercontent.com/TpSFQ3ZCzSe2PlNrTUHAXmpAjHHZ9wnAeBCjX6GpiBESoLyBT-kZOH8hrIdxzdCnyzNB2TNTQsDiznS9y9M__pVuiQz_8nD3=w480-h480

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Chemical rocks are formed from chemical reactions, mainly in the sea. Clastic and chemical rocks are the only rocks that contains fossils and the climate that was present when the rock formed.
Examples: Limestone, rock salt, rock gypsum, chert.

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Organic rocks are rocks made up of fossils, such as remains of plants and animals. It is formed from varying degrees of pressure and temperature over long periods of time.

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Clastic sedimentary rocks are formed by weather processes. The exposure to wind, ice, and water breaks rocks down into pebbles, sand, or clay particles.
Examples: Conglomerate, breccia, sandstone, and shale.

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The process in which sediments are stuck together by minerals that are deposited by water.

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Compaction is the process in which sediment is tightly squeezed, resulting in the reduction of the pore space between sediment grains.

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Deposition is the dropping of sediments, or soil and rocks in a new location. Deposition changes the shape of the land.

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Erosion is the movement in which sediment is transported to a new location on Earth's surface by natural forces, like wind or rain.

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Sediment can consist of rocks, minerals, and remains of plants and animals. It is often moved and deposited in a new location.

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Magma is the molten rock stored inside the Earth's crust.
Lava is magma that has reached Earth's surface through a volcano vent.

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Intrusive igneous rocks are rocks formed below the Earth's surface. Magma is slowly cooled below the Earth's surface; resulting in larger crystals.
Examples: Dunite, diorite, gabbro, granite.

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Extrusive igneous rocks are formed above the Earth's surface. When magma from a volcano reaches the surface, it will cool quickly, and form the igneous rock. They usually have small crystals.
Examples: Basalt,  andesite, rhyolite, and obsidian.