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Technically, it is not lava until it pours out of the volcano. While it is in the volcano it is still magma. What is not ejected in the form of lava might sink and form a plug, allowing the magma to once again build up in the volcano's magma chamber.
Lava.
magma
That is correct. When magma travels from the mantle to the crust and reaches the surface, that is a volcano.
Over time the magma chamber found inside volcanos is cut off from the mantle by tectonic plate movement. Without constant exchange of hot magma from the mantel to replace the colder magma in the volcano, (convection), the magma inside the volcano hardens into igneous rock.
The composition of the magma is a major factor in determining the form of a volcano. Magma with high viscosity tends to form steeper-sided volcanoes, while low viscosity magma results in more gently sloping volcanoes. Additionally, the frequency and type of volcanic eruptions can also influence the shape of a volcano.
basalt
The silica content and the gas content of magma are two properties that determine what kind of volcano will form. Magma with low silica content and low gas content tends to form effusive, shield volcanoes, while magma with high silica content and high gas content tends to form explosive, stratovolcanoes.
yes. magma is the lava that is in the volcano and lava is the magma that is outside a volcano
In a magma chamber
Magma inside a volcano can become a lava flow outside when pressure builds up inside the volcano, causing the magma to erupt through the volcano's vent or fissures. As the magma reaches the Earth's surface, it is then referred to as lava. Once outside the volcano, the lava can flow downhill and solidify to form igneous rock.
magma flows up to form the eruption