In this analogy, the needle is as big as we can make it.
Gas-rich is where the danger is, as I understand it. Those gasses expand as they get closer to the surface, and if they're trapped in viscous magma that doesn't flow easily and puts a lot of stress on the rocks above.
The fluid basaltic lavas of Hawaii don't explode, they flow out and make shield volcanos.
For one, the scale is way, way too big. It's like stabbing an elephant with a needle and expecting it to bleed out.
Also, the dangerous type of magma is extremely viscous and gas-rich. It doesn't flow like Hawaiian lava does.