No human endeavour could make or inject magma into a volcano. The magma found in relation to volcanoes is a natural phenomena.
A magma is injected into a volcano's plumbing the first thing you see is inflation of the land/volcano surface, this would be accompanied by earthquakes and low frequency harmonic sounds caused by the flow of magma through the volcano's passages (like a flute). There would then be the release of gasses from the vent (a phreatic eruption) as magma heats ground or surface water. This may then be followed by eruption of magma from the volcano's vent.
Technically, it is not lava until it pours out of the volcano. While it is in the volcano it is still magma. What is not ejected in the form of lava might sink and form a plug, allowing the magma to once again build up in the volcano's magma chamber.
the magma growing in size and large cracks forming
Magma usually refers to molten rock when it is still underground, and a crater is a cup shaped depression in the surface whether in a volcano or not. If a crater were full of molten rock we'd call it lava. It might be fed by a magma pool below the surface.
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.
When a volcano is active it will erupt. These volcanoes might take many years to erupt but will still erupt.
There are divergent boundries which causes Shield Volcanoes(an ocean volcano) and there a subducting boundries which causes a composite volcano(land volcano) there is also a cinder cone but that is made from a magma chamber(a place where magma is stored beneath the volcano and in the earths crust) explodes from being overfilled and layers upon layers form.
Scientists measure the silica content, temperature, and viscosity of magma to classify it into different types, such as basaltic, andesitic, or rhyolitic. These properties help determine how explosive or effusive a volcano might be when the magma erupts.
they can hide in their houses or on top of their houses the reason why is because the magma will flow all on the ground and it might hit you
A volcano might be bubbling as a warning that the volcano will burst soon. In addition, the volcano might be bubbling after the volcano exploded lava.
Volcanic mountains can get smaller through erosion, where wind, water, and ice gradually wear down the volcano's surface over time. They can also decrease in size through volcanic collapse, where the eruption of magma causes the structure of the volcano to weaken and collapse inward.
Volcanic rocks form on or near Earth's surface from the solidification of magma (molten rock) that has erupted from a volcano. They can also form when lava cools and solidifies quickly in underwater environments, such as in ocean ridges or volcanic islands.