No, a shield volcano typically has relatively thin, low-viscosity magma, which allows it to flow easily over long distances. This type of magma, primarily basalt, leads to the broad, gently sloping shape characteristic of shield volcanoes. The fluid nature of the magma results in less explosive eruptions compared to stratovolcanoes, which have thicker, more viscous magma.
inside a shield volcano is a hot surface of mamga
TThe magma is composed of gas and is silica rich.
The amount of viscosity present in magma depends on the amount of silica it has. A composite volcano produces rhyolitic lava which is very thick. A shield volcano produces a basaltic lava with less silica and significantly less viscosity.
The magma of shield volcanoes is rich in basalt. Basalt magma is low in viscosity and gas content, allowing it to flow easily and lead to the broad, gently sloping shape characteristic of shield volcanoes.
Volcan de Fuego is related to a subduction zone. It is located along the Ring of Fire in Central America, where the Cocos Plate is subducting beneath the Caribbean Plate. This subduction process generates the magma that fuels volcanic activity at Volcan de Fuego.
the code to unlock the Nerf magma (volcan) is MAGMA3
An acid magma or a granitic magma.
A volcan form when molten magma, formed deep in the Earth, makes its way to the surface.
Basaltic, runny magma.
inside a shield volcano is a hot surface of mamga
magma
TThe magma is composed of gas and is silica rich.
False. The magma of shield volcanoes is silica-poor.
The amount of viscosity present in magma depends on the amount of silica it has. A composite volcano produces rhyolitic lava which is very thick. A shield volcano produces a basaltic lava with less silica and significantly less viscosity.
The magma of shield volcanoes is rich in basalt. Basalt magma is low in viscosity and gas content, allowing it to flow easily and lead to the broad, gently sloping shape characteristic of shield volcanoes.
Volcan de Fuego is related to a subduction zone. It is located along the Ring of Fire in Central America, where the Cocos Plate is subducting beneath the Caribbean Plate. This subduction process generates the magma that fuels volcanic activity at Volcan de Fuego.
Thick and slow-moving magma is called "silicic magma." This type of magma is typically high in silica content, making it more viscous and less able to flow easily. It often leads to explosive volcanic eruptions due to the built-up pressure.