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.
Lava of relatively low viscosity (relatively low silica content, so basic rock such as basalt). Associated with constructive plate margins and with intra-plate volcanoes such as Hawaii.
Silica content of lava, as well as the temperature of the lava.
no
Lava plateau
viscous
Shield volcanoes form extensive fluid lava flow that erupts numerous times.
it has aa lava, so it is not fluid like, but still basaltic.
Silica content of lava, as well as the temperature of the lava.
Lava plateaus form when fluid basaltic lava flows out of fissures.
lava
lava
no
Lava plateau
lava= material flowing from a volcano
viscous
Shield volcanoes form extensive fluid lava flow that erupts numerous times.
Lava plateaus are formed by highly fluid, basaltic lavas.
No. Basaltic lava has less silica than andesitic lava which makes it less viscous and so basaltic lava flows more easily than andesitic lava.