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A natural passageway in a lava flow, often referred to as a lava tube, is a tunnel-like structure formed when the surface of a lava flow cools and solidifies while the molten lava continues to flow beneath it. As the flow rate decreases or the eruption ceases, the remaining lava drains away, leaving behind a hollow tube. These formations can vary in size and can be found in various volcanic regions, providing unique ecosystems and geological features. Lava tubes can also serve as natural conduits for the movement of water and other materials.

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