Yes. That is what the asthenosphere is.
When magma reaches the top of the asthenosphere it can start to work its way through the lithosphere, potentially reaching the surface to erupt from volcanoes.
In the crust the weak spot we have is the Magma Chamber. But, deep down to the mantle such weak zone is the Asthenosphere.
At an oceanic subduction zone, the athenosphere is subducted under continental lithosphere, or under other oceanic lithosphere. Friction between these plates causes heat that creates magmas. At a divergent boundary upwelling mantle (athenosphere) decompresses due to reduced pressures, allowing magma to form. This magma is extruded onto the seafloor as pillow basalts, and beneath the seafloors as massive gabbros and sheeted (gabbro) dikes.
i dont no this question is hardActually, it's Asthenosphere. The plates are part of the lithosphere. The asthenosphere is calle dplastic rock because its solid but under so much pressure it moves.
the role of asthenosphere in magma generetion
Yes. That is what the asthenosphere is.
Yes. That is what the asthenosphere is.
Yes. That is what the asthenosphere is.
asthenosphere
Magma could be found occurring in the lithosphere or the asthenosphere, usually originating in the asthenosphere.
Magma could be found occurring in the lithosphere or the asthenosphere, usually originating in the asthenosphere.
When magma reaches the top of the asthenosphere it can start to work its way through the lithosphere, potentially reaching the surface to erupt from volcanoes.
Because of the asthenosphere.
asthenosphere
From lithospheric interactions with the asthenosphere.
The asthenosphere.