They are both in the 1500 degree F range.
In a way. A magma is hotter then the surrounding rock, that's why the magma is molten and the rock is not. But because of this, some heat of the magma is melting the surrounding rock. You might want to classify this as erosion, but it's simply the melting of the rock surrounding the magma.
Baslatic magma is hotter.
Cooler magma flows slower than hotter magma.
when magma is melted at a higher temp. it'll be more runny so cooler magma will be slower than hotter magma
when magma is melted at a higher temp. it'll be more runny so cooler magma will be slower than hotter magma
Basaltic magma is hotter than andesitic magma. Basaltic magma typically has temperatures ranging from 1000°C to 1200°C, while andesitic magma has temperatures around 800°C to 1000°C.
Magma is generated along subduction zones primarily through the process of dehydration and melting of the subducting oceanic plate as it descends into the hotter, mantle wedge. The release of water and other volatiles from the subducting slab lowers the melting point of the overlying mantle, leading to partial melting. This molten rock then rises to form magma, which can contribute to volcanic activity and the formation of volcanic arcs associated with subduction zones.
Magma occurrs by rocks melting inside a volcano
Magma comes from the melting of material in the crust or upper mantle.
No. Water lowers the melting point of magma, both mafic and felsic.
The lower the viscosity is the hotter the magma is and faster it flows.Higher the viscosity is the cooler it is and slower it flows down.
The melting temperature of magma is primarily influenced by factors such as pressure, composition, and water content. Increased pressure raises the melting temperature, while different mineral compositions can lower it due to variations in the melting points of the constituent minerals. Additionally, the presence of water in magma decreases the melting temperature, promoting the formation of magma at lower temperatures than would be required in its absence.