THE GEOLOGY OF THE TWEETSIE TRAIL: TRADITIONAL AND SMARTPHONE OPPORTUNITIES FOR PUBLIC OUTREACH
The first 4.4 miles (7 km) of the Tweetsie Trail, from the Johnson City trailhead to Elizabethton, TN, transects a major fold sequence and many geologic features. The trail cuts across three formations and exposes faults, shear zones, joints, bedding and sedimentary structures, solution features, and areas of soil creep. Lithologies along the trail include in situ carbonates, shales, and sandstones, ballast materials including limestone, granite, gneiss, and “Tweetsie” coal and magnetite. The presence of easily accessible rocks and minerals and well exposed rock outcrops affords an opportunity to introduce the public to a host of geologic concepts, a natural laboratory for student groups, and convenient locations for Scouts to earn merit badges. Five posters that explain the history and geologic context of the trail have been installed, however, more needs to be done to take advantage of the ubiquitous presence of smartphone technology on the trail. Geologic points of interest explained using ArcGIS Story Maps and QR codes, via smartphones, provides an innovative method for engaging public interest in the geosciences.