Geological processes such as topography and effusion rate affect the speed of Kilauea lava flows
Geological factors such as surface topography and the rate of lava effusion are well-documented drivers that directly influence the dynamics, speed, and emplacement of lava flows at Kilauea.
The retrieved papers include specific studies on Kilauea eruptions (e.g., the 2018 lower East Rift Zone eruption and historical flows) explicitly connecting variables like effusion rates, slope angles, and pre-existing topography to lava flow velocities, dynamics, and routing behavior.
H. Dietterich, A. Diefenbach, S. Soule, M. Zoeller, M. Patrick, J. Major, P. Lundgren. Lava effusion rate evolution and erupted volume during the 2018 Kīlauea lower East Rift Zone eruption. 2021. https://doi.org/10.1007/s00445-021-01443-6
Demonstrates that variations in the rate of lava effusion significantly influence flow behavior and dynamics during Kilauea eruptions.
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Elisabeth Gallant, H. Dietterich, M. Patrick, D. Hyman, Brett B. Carr, John J. Lyons, Elinor S. Meredith. Catastrophic lava flow levee failure: precursors, processes, and implications. 2025. https://doi.org/10.30909/vol.08.01.6780
Shows that topography, slope-breaks, and surges in effusion rate directly control lava flow evolution, levee stability, and routing at Kilauea.
S. Biass, B. Houghton, E. Llewellin, K. Curran, T. Thordarson, T. Orr, C. Parcheta, P. Mouginis-Mark. Complex staged emplacement of a basaltic lava: The example of the July 1974 flow of Kīlauea. 2025. https://doi.org/10.1007/s00445-025-01817-0
Examines how terrain and variable slopes (topography) interact with complex emplacement histories to dictate the flow path and behavior of Kilauea basaltic lava.
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