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Fluid basaltic lavas such as rhyolite and dacite typically form thick short lavas namely lava spines, lava domes or coulees.
Fluid, basaltic lavas
Lava plateaus are formed by highly fluid, basaltic lavas.
Basic lava is the hottest lavas at about 10000 c and is highly fluid .it is dark coloured like basalt.rich in iron and mg but poor in silica
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Pahoehoe Flows.
Pahoehoe Flows.
Pahoehoe flows
Very fluid lavas have low viscosity. Lavas decrease in viscosity with lessening amounts of silicon. Mafic lavas are lower in silicon and therefore more fluid in nature.
No. Basaltic lavas are hotter and less viscous than andesitic lavas.
Basaltic lavas are hotter, but less viscous than andesitic lavas.
Hawaiian lavas are mafic.