Bryce Canyon National Park, Utah (1952)United States. National Park Service
Science
Bryce Canyon National Park, Utah (1952)
United States. National Park Service
Bryce Canyon National Park (Utah) -- Guidebooks
The area was reserved as Bryce Canyon National Monument by Presidential
proclamation, June 8, 1923. The act of June 7, 1924, authorized its
establishment as Utah National Park when certain conditions regarding
land acquisition had been met. The act of February 25, 1928, changed the
name from Utah National Park to Bryce Canyon National Park and
materially increased the size of the area. On September 15, 1928, when
all alienated lands within the proposed park area were transferred to
the United States, in accordance with the act of June 7, 1924, Bryce
Canyon National Park was established. The park now embraces more than
36,000 acres under Federal ownership.
Bryce Canyon National Park is one of the areas of the National Park
System owned by the people of the United States and administered for
them by the National Park Service, Department of the Interior. In these
areas the scenery and the objects of historic, prehistoric, and
scientific interest are carefully preserved and displayed for public
enjoyment.
Geology of Bryce Canyon National Park[1]
_Regional Features._—In Zion and Bryce Canyon National Parks the type of
scenery peculiar to the plateaus of southern Utah and northern Arizona
attains its most complete expression. Layer upon layer of shales and
sandstones have been carved into architectural forms, astonishingly
alike for size and color. The long stretches of even skyline seen on
approaching the parks from Cedar City (west), Panguitch (north), and
Grand Canyon (south) give an impression of extensive flat surfaces that
terminate in lines of cliffs, but viewpoints within the parks reveal a
ruggedness possessed by few other regions. The canyons are so narrow, so
deep, and so thickly interlaced, and the edges of the strata so
continuously exposed that the region seems made up of gorges, cliffs,
and mesas intimately associated with a marvelous variety of minor
erosion forms. The parks might be considered as mountainous regions in
which departures of many thousand feet from a general surface are
downward rather than upward.
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