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Lava tubes provide evidence for the past flow of lava during volcanic eruptions. They form when the surface of a lava flow cools and solidifies while molten lava continues to flow beneath it, creating hollow tunnels. The presence of these tubes suggests the dynamics of lava movement, the temperature of the lava, and the characteristics of the volcanic eruption. Additionally, studying lava tubes can offer insights into the geological history and volcanic activity of a region.
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Lava can easily burn us, and if the lava stream is powerful enough, can knock us off of our feet and burn our bodies to the bone. Lava, if given enough time, can burn right to the bone, which is a huge risk to pose on human life.
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The hole in a lava field where you can see lava is often referred to as a "lava tube" or "lava vent." These openings form when the surface of a lava flow cools and solidifies while molten lava continues to flow beneath, creating a tunnel-like structure. In some cases, the roof of the lava tube can collapse, exposing the lava inside. Such features can provide spectacular views of flowing lava, especially in active volcanic regions.