This was a truly unusual event and nearly impossible to forecast. There was little kinematics, 30 kts (or less) of bulk shear, veered flow, and CAPE around 100. But in this area, sometimes that's all you need with terrain and / or boundaries. Even more interesting was the "mini" supercell itself. The storm was basically 12,000 feet high (I usually skydive higher than that)! Low topped storms are typically 30,000 feet or so high. All the dynamics in this setup, albeit subtle, were confined to the lowest KM or so of atmosphere.