Kootenai Falls is a cascade rather than a plunge, and the reason is the rock. The Kootenai River runs across the Belt Supergroup, a 1.4 to 1.5 billion-year-old stack of metasedimentary rock that makes up most of the Cabinet Mountains and that, geologically, is roughly the same age as the oldest sedimentary rocks anywhere on the continent. In this section the river is cutting across hard quartzite interbedded with thinner, softer argillite layers, all of it tilted slightly toward the north.
That layered, tilted geometry is what produces the staircase cascade rather than a single waterfall. The river drops onto each successive quartzite bed, slides across it, and then drops again where the next softer argillite layer has worn back. The total fall is roughly 90 feet over less than a mile of river, with the main visible drop at the cascade overlook running about 30 feet. The bowl-shaped pools you can see at low summer water are spots where the river has scoured down through a soft argillite into the next quartzite shelf and stalled.
The other piece of the puzzle is glaciation. The Kootenai River trench was deepened by the Cordilleran Ice Sheet during the last glacial maximum, which scoured out the broader valley and left the river to find a new path across the resistant Belt rocks. That mismatch, an older deep valley and a younger river working across hard bedrock, is why the falls is set in a tight inner gorge rather than spread across the wider valley floor.