The Morgan Station Trail

Tygarts Creek Trail To Tygarts Creek via US 23

The extent to which our trail conforms to the route used by Native Americans in 1793 varies greatly. Often there is no good road or public access to the most likely path of the original trail. In other cases, following the trail requires a four wheel drive vehicle, hiking or biking. In any case, there are many paths down a hollow or river valley, and the preferred route would have likely evolved over time depending upon changing local conditions. We may assume that Native Americans walked the literal creek beds when that was an efficient way to travel between two points along their way. The modern day hiker is drawn to creek beds because they avoid the brambles, pot holes and potentially dangerous wild things that inhabit the forests and meadows. The smaller creeks meander and it would have been natural for the ancient traveler to walk across country if the meanders added significantly to the distance. We should always remember that in farming areas, the present routing of the creeks does not necessarily reflect their natural course. The practical farmer will soon redirect a stream from the midst of his cultivated area to one side or the other. Most likely redirecting along the base of an adjoining hillside. What we see as long contiguous flat fields of cultivation would have been a web of creeks, marshes and unulating forestlands in the base of the hollows. To some extent Native Americans would have regularly set fire to these bottoms to facilitate the hunting of game, but they would have had little inclination to re-direct creeks or make level the undulations.























The bridge spans the Scioto River at the point where it flows into the Ohio River. The Scioto River was the principle route connecting the Ohio River with Chillicothe and the other Shawnee villages of central Ohio.







The lower portions of Tygarts Creek were inundated by Ohio River waters when the Ohio was dammed in the 1920's to improve navigation and reduce flooding. In 1793, the Ohio River was much narrower and shallower, and Tygarts Creek would have joined the Ohio several hundred yards north of its present outflow. The relatively deep water of Tygarts Creek in these photos is solely a result of Ohio River water backing up into the creekbed. One must follow Tygarts Creek some distance south to escape the effects of the Ohio River inundation. Tygarts Creek has probably also been artificially straightened in its course near the Ohio River.