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The cervantes lava flow geomorfology, irazú volcano (costa rica): description of the central america`s greater lava flow fieldLa geomorfología de la colada de Cervantes, volcán Irazú (Costa Rica): Descripción de uno de los campos de lava más grandes de América Central
(Universidad de Costa Rica, 2011)
Evolution of crust- and core-dominated lava flows using scaling analysis
(Springer-Verlag Berlin Heidelberg, 2013)
We present a simple tool to evaluate the dominant
dynamical regime of a lava flow and to estimate the order of
magnitude of the main rheological parameter (viscosity or
yield strength) controlling the length of the lava ...
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
(Elsevier Science, 2016-11-15)
We analyzed two historical lava flows from the Southern Andes of Chile: The lava flows from the 1971 Villarrica volcano eruption and the 1988-1990 Lonquimay volcano eruption. The 1971 lava flow has a volume of 2.3 x 10(7) ...
Evolution of crust- and core-dominated lava flows using scaling analysis
(2013)
We present a simple tool to evaluate the dominant dynamical regime of a lava flow and to estimate the order of magnitude of the main rheological parameter (viscosity or yield strength) controlling the length of the lava ...
Morphology and stratigraphy of Serra Geral silicic lava flows in the northern segment of the Torres Trough, Paraná Igneous ProvinceMorphology and stratigraphy of Serra Geral silicic lava flows in the northern segment of the Torres Trough, Paraná Igneous Province
(Sociedade Brasileira de Geologia, 2018)
Emplacement history and inflation evidence of a long basaltic lava flow located in Southern Payenia Volcanic Province, Argentina
(Elsevier Science, 2015-02)
The El Corcovo lava flow, from the Huanul shield volcano in the southern Mendoza province (central-western Argentina) traveled a distance of 70 km and covered a minimum area of ~ 415 km2. The flow emplacement was controlled ...