When limestone, a sedimentary rock, gets buried deep in the planet for numerous years, the heat and pressure can change it right into a metamorphic rock referred to as marble. Marble is strong and can be polished to a beautiful luster. The is widely supplied for buildings and statues. Together you have the right to see from the picture, marble has actually a very sparkly luster. It wake up in plenty of different colors such together white, pink, gray, red, yellow or black.

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Basalt is a hard, black color volcanic rock. Basalt is the most common rock form in the Earth's crust.Depending on how it is erupted, basalt have the right to be hard and also massive (Figure 1) or crumbly and also full of bubbles (Figure 2).
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Slate

Slate is a metamorphic rock the is created when shales and also clays are placed under great pressure and heated within the earth for numerous years. Prefer shale, that splits apart into sheets, which way that the has an excellent cleavage. Slate is normally gray or black and is provided to make blackboards and also roofing tiles.
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Limestone

Limestone is a sedimentary rock. That is created by layers of little pieces that rock and also stones pressed tough together.The stoneformsin wet areas which typical it willalso containof shells and also waste issue from organisms the live in water.Limestone caves are developed when rainwater seeps with cracks in limestone rock and dissolves it.Limestone turns right into the metamorphic absent marble once it is subjected to high quantities of pressure and heat.
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Limestone is vital to make cement.It is offered in glass making.Layers of crushed limestone are placedunderneath roads and also underneath railroad tracks.Ithelps clean drinking water and treat sewage.Fertilizer supplied by farmers includes ground increase limestone. The is a food because that theplants and also is good for the soil.Animal feed likewise contains part limestone.

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Gneiss is a type of metamorphic rock that develops when a sedimentary or igneous rock is exposed to extreme temperatures and also pressure. Once this happens, virtually no traces of the original rock remain. Gneiss rocks are identified by their plan of minerals into long bands.Gneiss is distinctive among other rocks that have actually bands because its minerals are not evenly dispersed so the bands are assorted widths.