Basic lava comes from shield volcanoes, Basic lava is runny and flows faster.
Acid lava comes from composite cones,is slowly moving and viscous while basic lava comes from shield volcanoes,is non viscous, runny and flows faster
B/c they are made out of lava
the lava, the mantle, the outside. so there you are you have the three basic parts to a volcano.
Examples of lava include basaltic lava, andesitic lava, and rhyolitic lava. Basaltic lava is fluid and forms flat landscapes like the Hawaiian Islands, while andesitic lava is stickier and can create steep volcanoes like those in the Andes. Rhyolitic lava is very viscous and can lead to explosive eruptions, forming features like Yellowstone's geysers.
Basic volcanic lavas are those which have a low silica (45 - 52%) and a high iron and magnesium content. The term "basic" in this context is somewhat outdated. Modern scientists generally prefer to call such lava mafic.
It's basaltic lava, not basic.
Not acid lava, basic magma.
Basic lava has low viscosity, low silica content, high temperature, and flows easily over long distances. It typically produces gentle, effusive eruptions. Acidic lava, on the other hand, has high viscosity, high silica content, lower temperature, and tends to explode violently, leading to more explosive eruptions.
a valcano
Basic lava.
Acid lava comes from composite cones,is slowly moving and viscous while basic lava comes from shield volcanoes,is non viscous, runny and flows faster
lava
Basic lava is low in viscosity.
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
B/c they are made out of lava
the lava, the mantle, the outside. so there you are you have the three basic parts to a volcano.
Activation, persistence, and intensity are the three basic characteristics associated with motivation.