Parks Township comprises of three different geological formations. At the lowest points and at the Kiskiminetas River, you’ll find the Allegheny Formation. Next, the majority of township land is considered to be the Glenshaw Formation. Lastly, the highest hilltops contain the Casselman Formation.
Generalized Parks Township Formation Geology Illustration
In learning about local geology and formations, it can be confusing to visualize how the formations lie. The map above is an attempt to do just that. My original map had flat formations however an expert in state geology provided a better version for me. While sedimentary rocks typically form in water, the terrain varies. Erosion is one factor, generally being responsible for all the dips in the terrain of the map. Another is flow of water over time, where meandering rivers and streams can erode or deposit different thickness of material over millions of years.
The dips in the formations are caused by local synclines and anticlines. These are folds in the local formations that have them rising and dipping. You can not find a rock outcrop at 900 feet, and expect it to be the same a few miles down the road at the same elevation.
Another consideration is glaciation during the ice ages. While glaciers did not advance down to Parks Township, they did cause massive floods that would have drowned all but the hilltops of Parks. Lake Monongahela is one such lake. It was a proglacial lake that flooded the terrain to a height of 1,100 feet above sea level.