It is -83 with some gravity!
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.
Viscous and silica-rich magma, such as dacite or rhyolite, often erupts out of dome complexes. Due to its high viscosity, this type of magma tends to form domes and does not flow as easily as basaltic magma.
Felsic magma
Surtsey has basaltic magma, which is associated with the eruption of shield volcanoes. This type of magma is characterized by its low silica content and fluidity, allowing it to flow easily to the surface and form lava flows.
Magma with low viscosity, such as basaltic magma, typically causes quiet eruptions. This type of magma flows easily and allows gases to escape, resulting in relatively gentle eruptions with less explosive activity.
The rate of cooling of the magma determines the type of mineral formed by the magma or lava..
No, magma is not a proper noun because it is not a specific type of magma.
magma
I think it is the continental magma.
The type of rock that contains lava or magma is an igneous rock.
Mt. Cleveland has felsic lava, high in silica.
The type of rock formed by cooling of Magma or Lava is Igneous
Mount Shasta typically has andesitic magma, which is a type of intermediate magma that is common in subduction zone environments. This type of magma is rich in silica and forms from the partial melting of both oceanic and continental crust.
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.
Magma type.
This type of magma is called basaltic magma. It has a lower silica content, which gives it a darker color compared to other types of magma. Basaltic magma is commonly associated with volcanic activity at divergent plate boundaries.
Viscous and silica-rich magma, such as dacite or rhyolite, often erupts out of dome complexes. Due to its high viscosity, this type of magma tends to form domes and does not flow as easily as basaltic magma.