The magma forming stratovolcanoes rises when water trapped both in hydrated minerals and in the porous basalt<span> rock of the upper oceanic crust is released into </span>mantle<span> rock of the </span>asthenosphere<span> above the sinking oceanic slab. The release of water from hydrated minerals is termed "dewatering", and occurs at specific pressures and temperatures for each mineral, as the plate descends to greater depths. The water freed from the rock lowers the </span>melting point<span> of the overlying mantle rock, which then undergoes partial melting and rises due to its lighter density relative to the surrounding mantle rock, and pools temporarily at the base of the </span>lithosphere<span>. </span>
Answer:
He argue that they could have done better on their own.
Answer:
I believe that the answer is "The topography of mountainous region".
Explanation:
because tectonic plates is the direct cause that forms mountains and volcanos. The other options do not have anything to do with tectonic plates. The first option has to do with weather and climate and the second option has to do with physical geography. (I hope that this has helped!)
Two ways in which the proximity to water has affected Western Europe's economy:
1) Proximity of water can lead to lack of food, which affects economy of the country in various ways.
2) It has wet cool summers and wet, mild winters, so for shelters and cloths, it affects economy by transportation, extra manufacture etc.
Hope this helps!