The Great Boston Mountain Delta
Long ago during the Coal Age the rugged Ozarks were the western coast of North America as rising and falling sea levels caused the scene to alternate between shallow tropical seas and coastal swampland. Continental drift had placed ancient Arkansas on the equator and the collision of land masses caused a great arc of rugged mountains to extend from eastern Canada around to become the ancestral Ouachita range. This collision had produced a single continuous land mass (Pangea) extending all the way over the south pole. That, in turn, caused great ice sheets to come and go, as driven by periodic shifts in the shape of the earth’s orbit – the same shifts that have caused ice sheets to come and go in our present Pleistocene era. With the gentle slope on the edge of our continent, river deltas extended back and forth between southern Illinois and central Arkansas as ice sheets expanded and contracted. All the while, the advancing continental collision and build-up of sediments derived from mountain ranges being created caused river deltas to extend ever farther into our area. The sandstone deposited by those deltas would become the backbone of the Boston Mountains we hike on today. [...]