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The Tri-State tornado likely devloped like many other tornadoes did. A low poressure system was moving across the Plains, pullin warm, moist air north from the Gulf of Mexico and cooler air from Canada. As the low pressure and wedge of cool air lifted the warm air, thunderstorms developed. Strong wind shear set some of these tornadoes rotating, giving them the abuility to produce tornadoes. These thunderstorms are called supercells.

The particular supercell that spawned the Tri-state Tornado is a bit of a mystery. Back then, our ability to study storms was very limited; we did not have radar and we didn't even know what a supercell was. From what we do know, the thunderstorm seems to have formed unusually close to the center of the low pressure system. The dynamics of this area of the system may have helped to maintain the supercell in a steady state, allowing it to keep a single tornado on the ground for an extended period. This may be key, as most other historic tornadoes with extraordinarily long damage paths were likely several tornadoes that formed in succession, with poorly documented breaks in the path. Evidence suggests this was not the case with the Tri-State tornado.

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