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Volcanic eruptions occur when temperature rises inside the earth's crust, causing an internal explosion that violently expels materials like lava, magma, and gases from the interior to the surface. The viscosity of magma is affected by its temperature, gas content, and silica content - high viscosity magmas contain low gas, high silica, and are cooler, flowing slowly, while low viscosity magmas have more gas, less silica, and are hotter, flowing more readily. These factors influence the shape of volcanic cones and how volcanoes erupt.







