Field measurements of the 1983 Royal Gardens lava flows, Kilauea Volcano, and 1984 Mauna Loa lava flows, Hawaii

Mathematics – Logic

Scientific paper

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Flow Measurement, Hawaii, Rheology, Volcanoes, Chemical Composition, Comparison, Estimates, Mars Surface, Models, Rates (Per Time)

Scientific paper

Theoretical models used in the remote determination of lava flow rheology and compositions rely on estimates of such geometric and flow parameters as volume flow rates, levee heights, and channel dimensions, as well as morphologic and structural patterns on the flow surfaces. Quantitative measures of these variables are difficult to obtain, even under optimum conditions. Detailed topographic profiles across several Hawaiian lava flows that were carefully monitored by the U.S. Geological Survey during their emplacement in 1983 were surveyed in order to test various flow emplacement models. Twenty two accurate channel cross sections were constructed by combining these profiles with digitized pre-flow topographic measurements. Levee heights, shear zone widths, and flow depths could then be read directly from the cross sections and input into the models. The profiles were also compared with ones constructed for some Martian lava flows.

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