Bald Knoll

Bald Knoll is a cinder cone on the southwest edge of the Paunsaugunt Plateau, sitting in the gap between the south end of Bryce Canyon National Park and the western boundary of Grand Staircase-Escalante National Monument. It's the youngest of a cluster of basaltic volcanic vents in this area, with a well-preserved crater still visible at the summit and a long lava flow that traveled roughly seven miles to the southeast. Geologists date the flow to the late Pleistocene, though the cone's fresh-looking form has led to estimates ranging from a few hundred to several thousand years old.

This is a geologic feature more than a maintained hiking destination — you'll find it referenced on USGS topo maps and in volcanology surveys under several names (also called Black Knoll, Buck Knoll, or Corral Knoll locally). It sits on Dixie National Forest and BLM-adjacent land near the Alton coal mine area, with dirt-road access rather than a signed trailhead. Check current road conditions before heading out, and expect a backcountry visit rather than a developed overlook.