the elements and amount of water inside the volcano. Also, the thickness of the lava.
Lava flow maybe, it is the exact opposite in my oppinion.
Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava Lava
lava
This is known as lava.
lava.
Lava is molten rock at earth's surface, whether it is in a lava flow, a lava pool, or a lava dome. A lava flow is lava that is actively flowing downhill.
No there is NOT real lava in lava lamps. If there was real lava in lava lamps, it would burn, it just oil and water.
Pahoehoe lava, Aa lava, and Blocky lava
the answer is.....lava :)
Viscous lava is very sticky and thick and is more felsic (ie it contains more silica) than non-viscous lava. This type of lava makes for a very explosive volcano, because it's so sticky that it sticks to itself and can't exit the volcano until it explodes violently. Non-viscous lava is more runny and is more mafic (has more iron, less silica). Volcanoes with non-viscous lava are less explosive because the lava just runs out slowly and no pressure builds. The Hawaiian islands are formed from volcanoes with non-viscous lava.
Both lava and pyroclastic material are classified as rocks. Lava is molten rock and pyroclastic material is various debris. There is Basaltic lava, Andesitic lava, Dacite lava, and Rhyolitic lava.