Southeast of the central area of Kodachrome Basin where most of the formations are found, several unpaved tracks
cross the mostly flat surrounding land; one goes to the large sand pipe known as Chimney Rock, while another forks
south to the trailhead for Shakespeare Arch, a concealed feature at the edge of an isolated mesa of Entrada sandstone.
http://www.americansouthwest.net/utah/kodachrome_basin/shakespeare_arch.html