Metamorphic rocks

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Can you solve these questions please with clear explanation Describe the main difference between Kaolinite and Montmorillonite clay minerals Differentiate between Sedimentary, Igneous and metamorphic Rocks. Identify the main Transportation agents for the following types of soil. Wind Sea (salt water) Lake (fresh water) River\" Ice Solution Minerals-Montmorillonite Minerals-Kaolinite The main difference between Igneous, Sedimentary and Metamorphic rocks, is the way that they are formed, and their various textures. Igneous Rocks Igneous rocks are formed when magma (or molten rocks) cool down, and become solid. High temperatures inside the crust of the Earth cause rocks to melt, and this substance is known as magma. Magma is the molten material that erupts during a volcano. This substance cools down slowly, and causes mineralization to take place. Gradually, the size of the minerals increase until they are large enough to be visible to the naked eye. Igneous rocks are mostly formed beneath the Earth’s surface. The texture of Igneous rocks can be referred to as Phaneritic, Aphaneritic, Glassy (or vitreous), Pyroclastic or Pegmatitic. Examples of Igneous Rocks include granite, basalt and diorite. Sedimentary Rocks Sedimentary rocks are usually formed by sedimentation of the Earth’s material, and this normally occurs inside water bodies. The Earth’s material is constantly exposed to erosion and weathering, and the resulting accumulated loose particles eventually settle, and form Sedimentary rocks. Therefore, one can say, that these types of rocks are formed slowly from the sediments, dust and dirt of other rocks. Erosion takes place due to wind and water. After thousands of years, the eroded pieces of sand and rock settle, and become compacted to form a rock of their own. Sedimentary rocks range from small clay-size rocks to huge boulder-size rocks. The textures of Sedimentary rocks are mainly dependent on the parameters of the clast, or the fragments of the original rock. These parameters can be of various types, such as surface texture, round, spherical or in the form of grain. The most common type of Sedimentary rock is the Conglomerate, which is caused by the accumulation of small pebbles and cobbles. Other types include shale, sandstone and limestone, which is formed from clastic rocks and the deposition of fossils and minerals. Metamorphic Rocks Metamorphic rocks are the result of the transformation of other rocks. Rocks that are subjected to intense heat and pressure change their original shape and form, and become Metamorphic rocks. This change in shape is referred to as metamorphism. These rocks are commonly formed by the partial melting of minerals, and re-crystallization. Gneiss is a commonly found Metamorphic rock, and it is formed by high pressure, and the partial melting of the minerals contained in the original rock. Metamorphic rocks have textures like slaty, schistose, gneissose, granoblastic or hornfelsic. Examples of these types .

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Rocks on Earth can be classified into three categories based on the way they were formed. Igneous rocks are formed through volcanic action. Sedimentary recks are formed by deposition. Metamorphic rocks are formed when existing rocks undergo a change due to extreme heat and pressure. Rocks that have a volcanic origin are classifed as igneous and form when magma or lwa cook and hardens. As the magma or lava cook; crystals begin to form. The size of the crystals depends upon how fast the magma or lawa cools. If magma cools quickly, small crystals form and can be observed on the rock surface, such as in basalt, for example. Lava can cool so quickly that crystals do nothave time to form at all, such as with obsidian. If mogma cools slowly. larger crystals form and can easily be seen on the surface of rock specimens. A common example of igneous rock that exhibits large erystal formation is granite. When Earth's materials are deposited in layers and pressed together over time, sedimentary rocks form. The formation of sedimentary rock begins with the deposition of sediments. As layers are added, the oldest or lower layers that were deposited first experience increased pressure. The sediments and the spaces between then are crushed together in a process cal ied conpaction. During the cementation process, the sediments are bound together when a solution fills in around the particles like glue. If the rediments deposited are sand particles, such as in a beach environment, sandstone forms. If the sediments are fine sit or clay-sited particles, commonly cal ed'mud;' such as those found in basins worldwide, shaie forms, thestone typically forms from shells and other sediments deposited in ocean environments. A quiet and undistubed ewironnent will sometimes lead to fossit formation vithin the Layers of sedimentary deposition. Metamorphic rock forms when one type of rock changes into another due to exposure to heat and pressure ofter cansed by morement of material deep beneath Carthis surface. This change to rock appearance and cemposition takes an entrenelylong tine. Metamorphle rocks are often characterized by wavy layers of mineral orytals or by the presence of unusual mincrals. Any rock can become a metamorphic rock. For example, the sedimentary rock ahule forms from layers of deposited sitt. When exposed to high pressure due to scologic processes. the metamorphic rock slate forms. The sedimentary rock sandstone changes to cuataite when exposed to extreme heat and pressure beneath Eath's surface. Another example of a metamorphic rock is mable. which forms when limestone is exposed to extreme temperatures or prescure. Igneous basalt changes to schikt in the metanorphic process. The interesting. thing about the motamorplic nrocess is that any rock-igneous, metamorphic, or seclinentary-will change and form now metamorphic rock given enough time, heat, andor pressure. The rock cycle llustrates how rocks move on and under Earth's crust and change from one typ.

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