Lodge Center at Bryce Canyon and (Inset) Typical Guest Lodge
Lodge Center at Bryce Canyon and (Inset) Typical Guest Lodge
Interior of Guest Lodge, Zion National Park and Bryce Canyon
Interior of Guest Lodge, Zion National Park and Bryce Canyon
Rearranged and visualized principally from unpublished studies of Willis T. Lee, by courtesy of the National Parks Association.
These strata presumably were once continuous over the entire Plateau Region and the Grand Canyon. Many were much thicker than now, having been eroded during long periods when the surface was temporarily lifted above sea level. Altogether they may cover a creative period exceeding ninety million years. Strata are said to be unconformable when they do not lie in regular, parallel sequence.
Read table from bottom upward for historical sequence.
Cedar Breaks, some 2,000 feet higher than Bryce Canyon, is eroded from similar formation to that at Bryce Canyon.
Utah Parks Co. Automobile Specially Designed for Southern Utah Travel
Utah Parks Co. Automobile Specially Designed for Southern Utah Travel
[1]A table of the geological formations is on pages45and 46.[2]These accommodations are not operated by the Utah Parks Company and the information given is subject to change.
[1]A table of the geological formations is on pages45and 46.
[2]These accommodations are not operated by the Utah Parks Company and the information given is subject to change.
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This map in a higher resolution
This map in a higher resolution