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Here's a breakdown to make things even clearer:
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Okay, let's dive into some of the science behind Kilauea. It's not just about looking at the pretty lava; there's a ton of fascinating stuff going on beneath the surface. Kilauea is a shield volcano that's formed by the gradual accumulation of lava flows. The lava is relatively fluid and low in silica content, which allows it to flow easily over long distances, forming the gently sloping shape of the volcano. The magma that feeds Kilauea originates deep within the Earth's mantle, at a hotspot beneath the Pacific Ocean. This hotspot is a place where unusually hot mantle material rises to the surface, melting the surrounding rock and generating magma. The magma then rises through the Earth's crust, feeding the volcano's eruptions. This process is responsible for the formation of the entire Hawaiian Island chain.
