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Cedar Breaks National Monument was established in 1933. A small lodge designed by Gilbert Stanley Underwood and built and operated by the Utah Parks Company once existed near the south end of the monument, but it was razed in 1972. The Cedar Breaks Lodge was the smallest of the park lodges in the Southwest.
The route turns to the east here, while continuing south leads to the rest of Cedar Breaks National Monument and State Route 148 (the Cedar Breaks Scenic Byway). [1] Cedar Breaks National Monument from the overlook on State Route 143. As the highway heads east, it descends through thick aspen forests interspersed with ancient lava fields. [4]
In 1985, the southern portion of SR-143 between SR-14 and the southern Cedar Breaks National Monument boundary was re-designated State Route 148, with no further changes to this highway. The route was designated as a Utah Scenic Byway as the Cedar Breaks Scenic Byway, with a National Forest Scenic Byway designation following on February 6, 1991 ...
The eight National Monuments in the state of Utah are: Bears Ears National Monument near San Juan County [2] Cedar Breaks National Monument near Cedar City [1] Dinosaur National Monument near Vernal [1] Grand Staircase–Escalante National Monument near Kanab [3] Hovenweep National Monument near Bluff [1] Natural Bridges National Monument near ...
Latest foliage report and map shows where to see the best. ... #58 Cedar Breaks National Monument, Utah #59 Connecticut River Valley, Connecticut #60 Door County, Wisconsin
The visitor center is located on the rim of the Cedar Breaks amphitheater, overlooking the stone rock formations. It was constructed of peeled logs with dramatically extended ends, cut to a tapered buttress shape. A large, battered stone chimney at one end echoes the log detailing. The roof is covered by cedar shakes, with extended log purlin ...
The volcanic field is on a plateau bordered to the south by the Pink Cliffs and to the west by the cliffs of Cedar Breaks National Monument, [4] and features lava flows and over 25 cinder cones [7] mostly between Panguitch Lake and Navajo Lake [8] although older volcanics occur south of Panguitch. [8]
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