Basaltic lava is a type of lava that is common in volcanic regions and is associated with shield volcanoes and oceanic hotspot volcanoes. It is characterized by its low viscosity and high temperature, which allows it to flow relatively easily across the surface.
Basaltic lava is rich in iron, magnesium, and calcium, and has a low silica content. This composition contributes to its low viscosity, making it less explosive compared to other types of lava such as andesitic or rhyolitic lava.
When basaltic lava erupts, it often flows quickly and forms extensive lava fields. The low viscosity allows it to travel long distances from the vent, creating large, gently sloping volcanic landforms.