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It depends on the type and size of the volcano, the viscosity, and the amount of pressure built up over time within the volcano.
In this episode charizard fights magmar over a volcano.
The melting point is not changed by pressure. It is still over 32O
It goes over many hot spots and it no longer erupts
It goes over many hot spots and it no longer erupts
There are two types of atm pressure: static and dynamic. Static atm pressure stems solely from amount of air piled above the pressure point where the pressure is measured. We typically measure that at ground level; so the pressure is based on the weight of all the air above the ground. Dynamic air pressure is based in part on the static air pressure but as modified by the flow of the air above the pressure point where it's measured. A gent named Bernoulli found that the static air pressure is reduced by a predictable amount depending on air velocity when the air flows over the pressure point. And that's the answer. The static air pressure is reduced by air flow over the pressure point. In fact the amount of reduction is proportional to the velocity of the air flow over the pressure point.
The pressure exerted outward by fluids in your body balances the pressure exerted by the atmosphere on the surface of your body. the pressure increases
The team that hit the ball over will get a point.
its your point
For incompressible fluids it is its density and the height of the fluid over the point where the pressure needs to be determined
Whether a volcano should erupt or not depends on the pressure building up in the mantle underneath. In some areas, the solid cap formed over a dormant volcano is sufficient to prevent a new eruption. In this case, the pressure could move away to find a weaker area and a new eruption and the birth of a new volcano could appear.
They eplode into supernovas.