Explore the powerful world of volcanoes and their profound impact on Earth and humanity. Each episode uncovers how these natural wonders shape our planet and influence our lives. Join us to understand the dynamic relationship between volcanoes and the ever-changing Earth.
Volcanic plumes originate deep within the Earth's mantle, often starting around 2,900 kilometers down at the core-mantle boundary. Here, heat causes molten rock to rise in columns known as mantle plumes. As these plumes ascend, they partially melt surrounding rock, creating magma that collects beneath the Earth's crust.
Magma can also form in subduction zones, where one tectonic plate sinks beneath another. This process occurs at shallower depths, typically tens of kilometers. Volcanic activity can happen in back-arc basins and submarine volcanic features, where crustal thinning allows magma to intrude at depths of a few kilometers.
Pressure builds in magma chambers beneath the crust. As more magma and dissolved gases accumulate, the pressure increases. The magma is less dense and hotter than the surrounding rock. When the pressure exceeds the strength of the rock, magma pushes through fractures, leading to an eruption.
Explosive eruptions happen when the rapid expansion of gases violently fragments the magma, ejecting ash, gas, and lava into the atmosphere.
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