No, it is not possible for a human to escape magma as it is molten rock that can reach temperatures over 1300 degrees Fahrenheit. Any contact with magma would be fatal almost instantly.
yes
Yes, magma can escape from multiple locations in a volcano's vent system, not just one. This can result in different types of volcanic eruptions, such as both explosive and effusive eruptions, depending on the properties of the magma and the volcano's structure.
Lava.
not necessarily but there are other valves for the magma to escape.
If the gas cannot escape, such as when the magma solidifies underground, then the gasses become part of the minerals within the igneous rock. Since the main gas in most magma is water vapor, this effect will manifest mostly as hydrous minerals such as amphibole and mica.
yes
This is because silica-rich magma is thicker. The thicker the magma, the chance for the dissolved gas in there to escape is less likely. This causes an explosion. When the gases do escape, they cause an even bigger explosion
Yes, magma can escape from multiple locations in a volcano's vent system, not just one. This can result in different types of volcanic eruptions, such as both explosive and effusive eruptions, depending on the properties of the magma and the volcano's structure.
Lava.
Rhyolitic magma. This type of magma is found where the gases can't escape like in volcanic eruptions. Because the gas can not escape, the magma becomes viscous, resulting in the explosions being violent and unpredictable. The other type of magma is Basaltic magma. This can be found where continent plates are pulling away from each other and the magma is nearer the surface. This allows the gas to escape and therefore the magma is less viscous and doesn't result in explosive volcanoes, here eruptions are gentle and 'rifts' are more likely, where lava is persistent. I hope this helps! :)
not necessarily but there are other valves for the magma to escape.
basalt lava
If the gas cannot escape, such as when the magma solidifies underground, then the gasses become part of the minerals within the igneous rock. Since the main gas in most magma is water vapor, this effect will manifest mostly as hydrous minerals such as amphibole and mica.
A Magma Chamber is a space (that can change size) at a depth below a volcano in which magma can accumulate prior to an eruption. A volcanic vent is a conduit connecting the magma chamber to the surface. It is though this that the magma flows during an eruption.
Magma with low viscosity, such as basaltic magma, typically causes quiet eruptions. This type of magma flows easily and allows gases to escape, resulting in relatively gentle eruptions with less explosive activity.
a volcano will erupt forcing its magma to escape.
Vents in the volcano are passage ways for the magma, steam, and heat to escape the earth.