Cedar Valley is northeast trending. It narrows in the southwest, between mountain ranges; in this southwest section, the
Harmony Mountains are west, and the Hurricane Cliffs are east, bordering the
Kolob Terrace. The valley is mostly about wide, between mountains, or ranges, or the Hurricane Cliffs, to the east, which is a 75-mi long landform, from
Hurricane, Utah at its southwest end. The valley's north and northwest terminus merges into the Mud Spring Wash–Rush Lake region at the southwest of the
Black Mountains (Utah), (and the southeast perimeter of the Escalante Desert); a ridgeline extending southwest from the Black Mountains parallels the Hurricane Cliffs, and its terminus is at the north end of Cedar Valley (and Rush Lake). Between the ridgeline, and Hurricane Cliffs, east, Interstate 15 traverses, (only about 1-mi wide, adjacent the site of
Summit). It is also the route of the former
Old Spanish National Historic Trail. The Historic Trail traverses the Cedar Valley from
Enoch in the northeast, across the center-north to exit through the hills northwest, and through the townsite of Iron Springs, between the hills, and on the southeast edge of the Escalante Desert.
Valley lowpoints Quichapa Lake (dry lake) is located in the center-south of the valley, northwest of
Hamilton Fort, and fed by washes and creeks, from both the northwest and southwest, and from the southeast, (Hurricane Cliffs and Cedar Mountains). At the valley's north-northwest terminus, Mud Spring Wash flows northwest into the Escalante Desert. The intermittent dry lake,
Rush Lake is at its origin; Rush Lake is adjacent the ridgeline southwest from the Black Mountains, and at the downhill region of the alluvial fan, Long Hollow. == Access ==