Silica content of lava, as well as the temperature of the lava.
runny lava
Runny lava is typically found in oceanic plates. Oceanic plates are denser than continental plates and tend to produce basaltic lava, which is more fluid and flows more easily compared to the thicker and more viscous lava produced by continental plates.
Runny lava contains low amounts of silicon, whereas sticky lava contains high amounts of silicon.
Shield volcanoes are fed by basaltic magma.
When large amounts of fluid, runny lava accumulate, they create a type of volcano known as a shield volcano. These volcanoes have broad, gentle slopes and are formed from the repeated eruption of low-viscosity lava that flows easily across the landscape. Over time, the continuous layering of this lava builds up a dome-shaped structure. Prominent examples of shield volcanoes include Mauna Loa and Mauna Kea in Hawaii.
Lava is orange and runny
Thick, highly viscous lava.
runny lava
Runny lava is typically found in oceanic plates. Oceanic plates are denser than continental plates and tend to produce basaltic lava, which is more fluid and flows more easily compared to the thicker and more viscous lava produced by continental plates.
No. The lava there would be very viscous.
2. Thick or runny lava. Thick flows slowly, runny flows faster.
Runny lava contains low amounts of silicon, whereas sticky lava contains high amounts of silicon.
runny lava
Hot and runny
Shield volcanoes are fed by basaltic magma.
When large amounts of fluid, runny lava accumulate, they create a type of volcano known as a shield volcano. These volcanoes have broad, gentle slopes and are formed from the repeated eruption of low-viscosity lava that flows easily across the landscape. Over time, the continuous layering of this lava builds up a dome-shaped structure. Prominent examples of shield volcanoes include Mauna Loa and Mauna Kea in Hawaii.
shallow-sloping sides its huge in size and is built by many layers of runny lava flows gentle sloping caused by the very fluid