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Metamorphic_Rocks
Metamorphic_Rocks

... Recrystallization: This is the growth of new mineral crystals from other rocks. ...
Physical Processes Along Internal Boundaries In An Con
Physical Processes Along Internal Boundaries In An Con

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... 4. Have fossils within them 5. Goes through the process of cooling, melting, and crystallization 6. Goes through the process of heat and pressure 7. Goes through the process of compaction and cementation 8. Consist of Intrusive and extrusive rocks 9. Can change into other rocks, can be foliated and ...
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... Pluton; Butt Buttermere ‘Granite’; CF Carrock Fell Centre; CW Crummock Water Granite; Dun Dunmail ‘Granite’; En Ennerdale Granite Intrusion; Esk Eskdale Granite Pluton; Ha Haweswater Intrusions; HG Haweswater ‘Granite’; LG Loweswater ‘Granite’; Ryd Rydal ‘Granite’; Sh Shap Granite Pluton; Sk Skiddaw ...
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Volcanoes

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Large igneous province



A large igneous province (LIP) is an extremely large accumulation of igneous rocks, including liquid rock (intrusive) or volcanic rock formations (extrusive), when hot magma extrudes from inside the Earth and flows out. The source of many or all LIPs is variously attributed to mantle plumes or to processes associated with plate tectonics. Types of LIPs can include large volcanic provinces (LVP), created through flood basalt and large plutonic provinces (LPP). Eleven distinct flood basalt episodes occurred in the past 250 million years, creating volcanic provinces, which coincided with mass extinctions in prehistoric times. Formation depends on a range of factors, such as continental configuration, latitude, volume, rate, duration of eruption, style and setting (continental vs. oceanic), the preexisting climate state, and the biota resilience to change.
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