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Aerial thermal documentation reveals active lava channels displaying orange-yellow incandescence against cooling basaltic surfaces. Branching network exhibits dendritic geometry characteristic of pahoehoe flows. Temperature gradients manifest as distinct chromatic stratification from bright yellow cores to dark charred periphery. Molten material demonstrates fluid dynamics principles through interconnected channel systems.
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Published 16:23
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Comments about Lava Flow Network Analysis: Incandescent Fractal Patterns on Solidifying Basalt Substrate