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Rock Cycle Diagram<a href="https://rsiasacademy.com/rock-cycle-diagram/">Rock Cycle Diagram</a> is the one that explains the processes through which the types of rocks namely – Igneous, Sedimentary and Metamorphic undergo transformation in Geologic times. Rocks of any type can be converted into any other type, or into another rock of the same type. Whenever the state of equilibrium of a particular rock type is disturbed, the rock undergoes a transformation e.g. when an Igneous rock like Basalt or Obsidian is subjected to weathering, it may break up into fragments.
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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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List each category of rock and describe how it forms.Explore Student Journal: The Rock Cycle aks on Earth can be classified into three categories based on the way they were formed. Igneous rocks are formed through volcanic action. Sedimentary ks are formed by deposition. Metamorphic rocks are formed when existing rocks undergo a change due to extreme heat and pressure. cks that have a volcanic origin are classified as igneous and form when magma or lava cools and hardens. As the magma or lava cools, crystals begin to im. The size of the crystals depends upon how fast the magma or lava cools. If magma cools quickly, small crystals form and can be observed on the rock iface, such as in basalt, for example. Lava can cool so quickly that crystals do not have time to form at all, such as with obsidian. If magma cools slowly. ger crystals form and can easily be seen on the surface of rock specimens. A commen cxample of igneous rock that exhibits large crystal formation is anite. Then Earth's materials are deposited in layers and pressed together over time, sedimentary rocks form. The formation of sedimentary rock begins with the eposition of sediments. As layers are added, the oldest or lower layers that were deposited first experience increased pressure. The sediments and the paces between them are crushed together in a process called compaction. During the cementation process, the sediments are bound together when a olution fills in around the particles like glue. If the sediments deposited are sand particles, such as in a beach environment, sandstone forms. If the ediments are fine silt or clay-sized particles, commonly called "mud." such as those found in basins worldwide, shale forms. Limestone typically forms from thells and other sediments deposited in ocean environments. A quiet and undisturbed environment will sometimes lead to fossil formation within the layers of sedimentary deposition. Metamorphic rock forms when one type of rock changes into another due to exposure to heat and pressure often coused by movement of material deep beneath Earthis surface. This change to rock appearance and composition takes an extremely long time. Metamorphic rocks are often characterized by wavy layers of mineral crystals or by the presence of unusual minerals. Any rock can become a metamorphic rock. For example, the sedimentary rock shale forms from layers of deposited silt. When exposed to high pressure due to geologic processes, the metamorphic rock slate forms. The sedimentary rock sandstone changes to quartzite when exposed to extreme heat and pressure beneath Earth's surface. Another example of a metamorahic rock is marble. which forms when limestone is exposed to extreme temperatures or pressure. Igneous basalt changes to schist in the metamorphic process. The interesting thing about the metamorphic process is that any rock-igneous, metamorphic, or sedimentary-will change and form new metamorphic rock given enough. time, heat, and/or pressure. The .
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This PowerPoint helps students to consider the concept of infinity.
This PowerPoint helps students to consider the concept of infinity.
Rock Cycle Vocabulary
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Rock Cycle Vocabulary
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Examples
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![Rock ,[object Object]](data:image/gif;base64,R0lGODlhAQABAIAAAAAAAP///yH5BAEAAAAALAAAAAABAAEAAAIBRAA7)