The influence of effusion rate and rheology on lava flow dynamics and morphology: A case study from the 1971 and 1988-1990 eruptions at Villarrica and Lonquimay volcanoes, Southern Andes of Chile
Field analysis of two lava flows from the Southern Andes of Chile Volume- and cooling-limited lava flows show different morphologies and dimensions Volume-limited flows can be simulated as Herschel-Bulkley, Bingham or Newtonian fluids with constant temperature Cooling-limited flows are best simulated with the Yield Strength in the Crust regime