The movement of magma can vary significantly depending on factors such as its viscosity, the pressure within the Earth, and the geological conditions. In some cases, magma can flow several kilometers within a volcanic system, while in other instances, it may remain confined to a specific area. When magma erupts, it can travel even farther, depending on the eruption style and the surrounding terrain. In certain explosive eruptions, volcanic materials can be ejected high into the atmosphere and land far from the eruption site.
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