Magma in the mantle moves in a current called a convection current. A convection current is a circular flow of a substance in which a hot substance rises, cools, sinks, gets hot again, and repeats. In this way, magma in the mantle flows in currents of more hot or more cool magma.
it is normally intermediate flow because of the silica content.
When magma comes in contact with water first the water will stem because the magma is so hot the water is at or past its boiling point them the magma will harden fast because instead of its slow cooling prossess it is spead up from the waters temperature it is a big mess :) luvhh jasmine chanda
The explosive potential of a volcano is determined by two primary factors:Gas within the magmaViscosity of the magmaThe combination of the gas and the viscosity determine the explosive potential of the magma as a result of the ability for the magma to flow as well as if it can release the dissolved gasses in a passive manner.Volcanoes that have a high concentration of Silica in their magma traditionally have a tendency to erupt more explosively. In the case of basalt, although there is traditionally a high level of dissolved gasses within the magma, basalt can easily flow. The ability for basalt to easily flow allows for the passive release of the gasses that are dissolved in the magma resulting in a non-explosive eruption as the gasses are released over time as the magma reaches the surface and not catastrophically as the magma escapes.
I don't know :( this is my assignment :P
Granitic magma is highly viscous (resists flow). This high viscosity results in the entrapment and buildup of gases which create explosive eruptions.
the rock that can flow like a liquid is a mantle because the mantle has two parts. The upper part is the solid rock. The solid rock of the mantle is part is the lithosphere. Below the solid rock, the mantle rock has the ability to flow like a liquid. Most of the mantle is made up of rock that can flow. Sanjida Ahmed 752/753
Volcanoes erupt because of the flow of magma in the mantle, which reaches the surface.
The outer core of the mantle can be liquid.
It is the ability of the mantle (solid) to flow like liquid.
no part
None! Unless you mean the core. The outer core is liquid.
None! Unless you mean the core. The outer core is liquid.
None! Unless you mean the core. The outer core is liquid.
solid
My guess: its almost like boiled water. you know how the steam rises? same with the heat from the magma in the mantle. The magma itself is around 500-900 degrees celcius, so the heat is much less by the time it makes it to the surface of the earth. that is my guess
The mantle is the solid layer of earth that can flow because of great heat and pressure
Areas where continents are either moving apart or together causing magma from the mantle to flow to the surface